Bringing My Family Tree to Australia

The details of our trip to Darwin were outlined in the first blog that I wrote and posted three days after our return (July 25th). I wrote that “the main driving force that led us to take the trip was the family trip to Melbourne.”

My Australian family started with my cousin (his father and mine were brothers), who is eight years older than me, also born in Warsaw, Poland. In that blog I also included a reference to a recent interview that he gave about his life in Warsaw during the war. In the meantime, I have found an older reference that includes a short summary of the life that he had built in Australia.

I came to Australia with the knowledge that during our stay in Melbourne, we would encounter social occasions where we’d be invited to settings that would include family members that have no idea about the relationship of my family with my cousin’s family. So, I decided to bring my family tree with me. The direct descendants of my cousin are familiar with the connection mainly because this was not our first visit to Melbourne and a few of them also visited us in the US. But family trees are open-ended documents that constantly change with time. The changes are “small” when children are born but the changes can be very large with marriages, because full new family trees are incorporated as a result of a single new marriage link. Aside from the people directly involved, chances are that members of the two families know very little about each other. Indeed, my “prediction” was confirmed at a family event that one of my cousin’s daughters arranged that included her direct family, my cousin, my wife and the mother-in-law of my cousin’s daughter. My wife and I had never met the mother-in-law, so I was glad that I had brought my family tree with me to start a lovely conversation.

I also had an ulterior motive for bringing my family tree to Australia and writing about it in this blog.

I mentioned before that my cousin’s early background has important similarities to mine. We were both in Warsaw at the start of the German invasion of Poland that started WWII and the resulting Holocaust. The difference was that at that point he was 8 years old, and I was 3 months old. This fixes my age above the life expectancy of every country in the world. (Japan holds the record – 82). I still teach, write, and travel but I am fully aware of my limited prospects. So, I am always on the lookout for younger relatives who can take over the administration of my family tree. The Holocaust made sure that, together with the more normal dynamics of family trees such as marriages and births, my tree turns out to be global. The Australian branch is an important offshoot of this tree. In addition to Australia, my tree has major branches in France, US, and Israel. I felt (and still feel) that an important part of my job is to try to ensure continuation of the data-gathering beyond my life span. I feel that with electronic communications in our possession, the dream that all humanity will be part of the same tree is not totally outlandish and that it can contribute to a feeling that all of us are parts of the same family and thus responsible for each other.

The current “record keeper” of the biggest family tree is the Oxford University Big Data Institute with 27 million people. This database is based on genomic research that promises to extend history beyond the written record to include genomic records and thus unify our academic definitions of history with archeology, anthropology and other disciplines that deal with our past. Genomic sequencing is fast becoming part of our “reading skills” and life itself is being redefined, in one sense, as a genomic writing ability. My dream is to try to redirect this to fortify our collective chance of survival. I fully realize that this is a dream that most probably will not materialize. This outlook is fed by my observation that my younger generations are fully occupied with their own dreams for their future and that “collective” dreams are not a priority for them.

A sprinkle of exception to this pessimism came from my Australian family.

The youngest son of my Australian cousin likes to travel, both professionally and as a tourist . In one of his trips that followed a trip with his father to Poland to share my cousin’s early past, he “discovered” Wysokie Mazowieckie (WM) and the efforts that some people (local and foreign) are making to resurrect the Jewish cemetery there.

A few years after that “discovery,” my wife and I took a trip to WM and met Karol Glebocki, the teacher that, with his students, became central to this effort. Figure 1 shows both of us with the tombstone of Aaron Avigdor Tomkiewicz (AAT), a man who already was the oldest ancestor in my family tree.

Figure 1 – Karol Glebocki and me near the gravestone of Aaron Avigdor Tomkiewicz in the newly restored Jewish cemetery in Wysokie Mazowieckie.

I didn’t start my family tree with the visit to WM. I started it a few years earlier, driven by a similar motive that drives me now in my search to move the effort to a younger generation. My uncle (younger brother of my mother) was with us through our Holocaust experiences but decided to settle in France and start his own “branch” there. At the time, he was the guy that was left with the most detailed memory of our past. I decided to construct the tree based on input from him. My objective was not to find my origin but just to be able to connect as many surviving members of my family as possible. For many years, to my knowledge, I was the only one in my family to administer the data. Two questions remained unanswered. AAT was listed with two wives. I was sure that he was not a bigamist, but I had no idea about the details. I knew of a French family that hosted me during the Israeli Independence war, but I knew nothing about the details of the links. Both questions got answered when I was able to link with David Askienazy from Paris. He is much younger than me and much more active and productive in assembling his family tree (listed in “My Heritage”). After our contact, my family tree grew considerably. The last major development went back to WM and a connection with Aaron Rotenberg, through the Jewish Record Indexing – Poland, with detailed data search in WM. I haven’t yet analyzed all the new data that he supplied me. My present family tree contains 352 members!

The “normal” dynamics of a family tree can be demonstrated with very recent developments that took place this year:

Over three months ago, a first granddaughter was born to my French cousin. We had the opportunity to enjoy the three generations on Zoom.

Natalie Leventhal,the grandmother of my wife’s two nieces, will celebrate her 100 birthday. I will bring the family tree with me to Connecticut, where she lives, so the younger generation will be able to take over administration of that branch.

Toward the end of this month, my wife and I will travel to Washington, DC to attend a Holocaust meeting and stay with my American cousin. We will bring the family tree with us.

The “ultimate” impact on my family tree took place few days after our return from Australia. I got an email from Matt Rozell (see below) saying that he found, in the US archive, a short movie clip taken by American soldiers that unquestionably describes our liberation by the American army on April 13, 1945 near the German town of Farsleben.

You can watch the clip-on YouTube.

After 78 years, this was a sensational find. Social networks were full of feedback and all the Israeli papers that I have access to, both in English and Hebrew, mentioned it. I got emails both from Israel and the US asking me if this was “my” train. It was. The Jerusalem Post, an Israeli, English language paper, probably had the fullest history of the event.

A short description taken from the article is below:

Never-before-seen footage of Holocaust survivors being liberated by US Army soldiers during the last stretch of World War II has been unearthed at the United States National Archives, according to a Wednesday report by the Independent.

On Friday, April 13th, 1945, soldiers from Tanks 12 and 13 from the US Army’s 743rd Tank Battalion led by a scouting jeep liberated a train transport with thousands of Holocaust victims who had left the Bergen-Belsen concentration camp one week before and were bound for Theresienstadt.

First, I started to do what many survivors of this event do – try to find myself or my family there. (My mother and her younger brother were also there.) A 78-year gap is no help. So, I tried to do better. I went through my mother’s small Bergen-Belsen book, whose title, translated into English, reads, “There was Life Even There” (it is shown in Figure 2), to look for a description of the event as written shortly after our liberation. Here’s her description of the liberation as written close to the end of the book:

On the 13th of April we stop next to a copse. The trees are humming, the birds are twittering, a light breeze wrinkles the surface of the river. Someone says we’re not far from Magdeburg. Pilsudski was imprisoned in Magdeburg, wasn’t he? They’re shooting at us from the planes. The Germans are shooting at us from the copse. I can’t see much from under my pillow. Mulek went on reconnaissance. When he came back he said they’d fished our Auslander documents out of the river. It turns out that our Palestinian certificates had arrived from Switzerland in February. That Kastner chap didn’t forget afterall! Why did the Germans throw the documents into the water? What will happen to us?

There are corpses lying on both sides of the train. The engine driver has made off on the locomotive. So we’re on a train with no locomotive and a German crew who beat us, spit at us and curse us in the intervals between shooting. They have an order to finish us off and throw our bodies into the Elbe, just like they’ve done with tens of thousands of concentration camp victims in the last few months. Is it now? Maybe they’ll wait another hour or two.

A handful of human spectres made it from the train to a town nearby and begged some food from the Germans. “They were completely normal, like they weren’t Germans at all,” says someone with surprise. Stas and Hela went too and got a chicken and a few potatoes in return for my broken gold watch. What luck! Renia cleans the chicken and cooks it on a Primus borrowed from the Czechs. Slawcia advises us to add what’s left of the dried potatoes. There’ll be more that way. The whole compartment participates in the feast without paying any attention to the shots and ceaseless cannonade whose threatening sounds are coming from afar, from near, no matter where from. We eat. Will they make it in time? Won’t they? “How did you get hold of so many potatoes?”

Suddenly the first American soldier appears. How inconspicuous he is! Behind him there’s a group of others. One of our wheeler dealers has already recognized the friend of a friend in America. The American soldier waves his hand. His trousers are creased. We’re free.

We’re saved. Stas throws himself to the ground and cries. Others are crying, laughing, kissing. I don’t feel like crying. I feel stupid, totally empty inside. So this is the way the war has finished for us? Without pathos. Without drama. An American soldier with creased trousers and now it’s the end after so many years. So many ages.

Magdeburg is taken and the 9th American Army has taken us into its possession. Bobus proudly brings me a rucksack containing a dirty towel and a jagged comb. The children kick the Germans, take their guns away, their bikes and rucksacks.

The adults are too weak to take revenge. They don’t feel triumphant. In fact they don’t feel anything. They throw a guard to the ground. “Kneel,” they shout. They torment him, but without conviction, as if it were a duty, mildly. They’re still completely bewildered. They don’t know what to do with him, with themselves. But yesterday this selfsame guard was hitting women in the face when they begged him for a few rusks. Except what will it achieve? The Americans offer cigarettes, hand out bars of chocolate. “Aren’t you happy?” they ask. Are we happy? We don’t dare ask ourselves that question. Mother, father, Piotr, Witek, Helenka … We’ve survived and what now? “Won’t we need these potatoes anymore?” we ask the Americans uneasily.

The girls are flirting with the soldiers. Singing. Conversations. The Americans photograph the specter-train from all sides, and us, the specters from the train. We must light a fire and boil a few potatoes. I must wash Bobus and put him to sleep. Mrs M. shrieks at the top of her voice. Her husband has just died this minute. He was already a free man. She’s left with four children just when the war has finished. A huge blonde in an American uniform brings a bottle of wine to the compartment. Do I want some silk stockings? Would I go for a walk with him? He fought for me after all. He fought. I’m as light and empty as a soap bubble. My head’s spinning from the wine. From the freedom which has arrived too late for happiness. “My little one didn’t live to see the day,” says Sonia and cries. For joy?

Next day we leave the train. They take us to beautiful Hillersleben, they’ve previously thrown the Germans out. We become “Displaced Persons of the World.”

Figure 2

You have here what you need to compare my mother’s description of our liberation with that of some of the liberators. Not surprisingly, they are not the same. They are two different perspectives. To my knowledge, this is one of the few opportunities that exists to read these views. For that, I thank Matt Rozell and my mother.

The first of my blogs that describe Matt Rozell’s continuous efforts to get the liberators and survivors together was written two months after I started this blog (June 4, 2012). An important follow up came when, jointly with the people of Farlsleben, a monument was erected there that was shown in the April 12, 2022 blog. A photograph of Matt Rozell that commemorates the D-Day anniversary is shown in the June 11, 2019 blog (the guy on my left without glasses).

It is obvious (at least to me) that without this event “my” family tree wouldn’t even exist.

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Traveling to the Weather: Darwin

Figure 1
NT State Population (Source: https://images.app.goo.gl/mVia9Q8aQhxrdgsF8)

The details of our trip to Darwin were outlined in the first blog that I wrote in this series, that was posted three days after our return (July 25) and I’ll focus this blog on our Darwin trip and its environs. About 5 days were spent in an organized tour in the National Parks around Darwin, a map of which was included in that blog. They include Kakadu National Park, Litchfield National Park, and the Katherine Gorges.

Figures 1 and 2 provide a general picture. Darwin is the capital of the Northern Territory (NT). It is not a State because even the population of tiny Tasmania (that is a state) exceeds it by a factor of 2. Half of the population of NT is around Darwin; even with that, Darwin counts as a small city. Figure 2 indicates that at least in the dry season (see last week’s blog), the city and the parks around it are significant tourist draws. Indeed, walking around the city leaves the impression of a crowded place. Most of this blog will focus on a few photographs that we took during the visit.

Figure 2
Australian tourist attractions (Source: https://www.worldmap1.com/australia-tourism-map)

Before shifting to the photographs, here are a few words (and sites) about the weather and about Kakadu National Park:

The Weather (Source: https://www.australia.com/en-us/facts-and-planning/weather-in-australia/darwin-weather.html):

The wet season (November – April)
The wet season in Darwin is characterized by high humidity, monsoonal rains and storms. Average temperatures range from 24.7 – 32 °C (76.5 – 89.6°F), and humidity can push past 80 per cent. The average annual rainfall is 1727.3 mm (68 inches) and January is the wettest month. Despite this, January and February is considered by many as the most beautiful time of year in the Top End. Sunny days and afternoon storms refresh the landscape, and animals and plants flourish.

October to December is the season of spectacular lightning storms, an event eagerly awaited by locals who watch the show from beachside restaurants and bars.

The dry season (May – October)
The dry season, from May until October, is characterized by warm, dry sunny days and cool nights. Temperatures typically range from 21.6– 31.8°C (70.9 – 89.2°F), and humidity levels are much lower: around 60 – 65 per cent.

Relatively cool weather arrives in May, and until July, nights are crisp with temperatures ranging from 17 – 23 °C (62.6 – 73.4°F). It is also the perfect time to explore the more remote areas of the region that can be off-limits during the wet season.

For contrast, the average annual precipitation in NYC is 46.6 inches (1184 mm).

Kakadu National Park                                                                                                        (Source:  https://en.wikipedia.org/wiki/Kakadu_National_Park)

Kakadu National Park is located within the Alligator Rivers Region of the Northern Territory, covering an area of 19,804 km2 (7,646 sq mi), extending nearly 200 kilometers (124 mi) from north to south and over 100 kilometers (62 mi) from east to west. It is roughly the size of Wales or one-third the size of Tasmania, and is the second-largest national park in Australia, after the Munga-Thirri–Simpson Desert National Park. Most of the region is owned by the Aboriginal traditional owners, who have occupied the land for around 60,000 years and, today, manage the park jointly with Parks Australia. It is highly ecologically and biologically diverse; hosting a wide range of habitats and flora and fauna, Kakadu is fully protected by the EPBC Act. It also includes a rich heritage of Aboriginal rock art, including highly significant sites, such as Ubirr.

All our friends on the tour of the national parks were Australian. We asked the guide if this is the norm. She responded that on the previous tour, there were a few Americans and Canadians. All of us were “traveling to the weather.”  But all of us were aware that these are luxury travels that very few can afford. There is another kind of “weather traveler,” one for people that have no other option. We labeled these as “environmental refugees” and I’ve often written about this topic. (see April 3, 2018, e.g.). Most of us cannot escape the impacts of climate change. Recently, President Biden took some steps that include protections for construction workers, farmers and other laborers who are exposed to sweltering heat. All of us realize that much more needs to be done.

What follows are some pictorial highlights of the trip:

Figure 3
Louise near a Cathedral termite mound in Litchfield National Park

These mounds can last 50-60 years.

Figure 4
Kakadu National Park from above

The main conclusion that I draw from the landscape of Kakadu, is the power of water, with almost no human help or destruction, to enrich the landscape. We were given a warning about the river network: don’t swim in these rivers. The reason is shown in figure 5.

Figure 5
Crocodile ready for a meal in Kakadu National Park

Figure 6
Ancient (≈ 12,500 years) cave drawings by Aboriginals in Kakadu National Park

More about the cave painting can be found here.

Figure 7
Katherine Gorge

We departed from Darwin with a gorgeous sunset as shown in figure 8.

Figure 8
Sunset in Darwin

One of the best opportunities to see the sunset is to walk on one of the beaches in the late afternoon where, twice a week, during the dry season, a sunset market takes place that invites all the attendees to watch the sunset (figure 9) after buying all kinds of stuff.

Figure 9
Observers of the Sunset from Darwin’s Sunset Sunday-Thursday market.

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Traveling to the Weather

Last week’s blog outlined the reasons why my wife and I decided to take our vacation in Australia. The main reason was to see family in Melbourne and a secondary reason was to try to have a short break from the weather back home. I promise that in this and in following blogs, I will go into some details.

Traveling to visit family is a common activity that many of us do whenever we have the opportunity. I think that documenting changing extended families has the long-term outcome of developing a feeling that all of us belong to the same family and thus willing to take care of each other.

For now, however, this blog will focus on the weather.

Discussing the weather requires some background. Weather and climate are the most important topics of this collection of blogs. However, I never discussed the fundamentals of the driving forces of climate in a way that would  be understandable with no educational prerequisites. I will try to remedy that here with some quoted literature.

I think the best starting point  is the short review by Stevens in Nature Education that references figure 1 and from which I extensively cite below. This review will serve us in this and next week’s blogs. It  describes the background for choosing Darwin as an important component of our Australian vacation and it will also serve as a background for future blogs that will describe the roles that El Niño and La Niña are playing in our present climate.

 

Sunlight Intensity Is a Key Component of Climate

Directly or indirectly, the sun provides energy for living organisms, and it drives our planet’s weather and climate patterns. Because Earth is spherical, energy from the sun does not reach all areas with equal strength. Areas that are exposed more directly to the sun’s rays (i.e., those nearest to the Equator) receive greater solar input. In contrast, those in higher latitudes receive sunlight that is spread over a larger area and that has taken a longer path through the atmosphere. As a result, these higher latitudes receive less solar energy (Figure 1).

The sunlight intensity on some parts of the earth significantly varies over the course of the year as the earth changes its orientation in space. Seasonal variation in solar input occurs because the Earth is tilted on its axis by 23.5˚ (Figure 1). As Earth orbits the sun, its orientation to the sun changes. Winter in the northern hemisphere occurs as the northern tip of the planet tilts away from the sun; during this time, the southern hemisphere receives greater solar input and experiences summer. As Earth reaches the opposing point of its orbit and the northern hemisphere becomes angled toward the sun, the seasons reverse. Tropical areas experience relatively minor changes in temperature, and their seasons are characterized by the presence or absence of rain.

Sunlight Intensity Affects Global Winds, Precipitation Patterns, and Ocean Circulation Which Are All Components of Climate

At the Equator, the Earth receives greater exposure to the sun’s rays where both air and extensive bodies of water warm under the influence of the sun. Molecules are more closely packed together when cold than they are when warm, which makes warm air and water less dense than cold air and water. This difference in relative density causes heat to rise.

The warm air that rises in the tropics is wet. Sunlight causes water to evaporate from plants, soils, and bodies of water. These water molecules rise to become part of the air; because the air is warm and less dense, there is sufficient room for water molecules within the air mass. But as the air gains altitude it cools, reducing density and space for water. The water molecules condense to form clouds and eventually fall as precipitation. At the same time as sunlight is driving evaporation and precipitation patterns, it is also creating winds. As warm air moves upward, colder air from neighboring areas rush in to fill the void left behind. Tropical air moves away from the equator and toward the poles. As it travels, it cools, becomes denser, and eventually descends around 30˚ north or south latitude. This dry air mass, having lost its moisture in the tropics, absorbs moisture from the ground, creating arid conditions at these latitudes. Some of the air is drawn back toward the equator, and some is drawn toward the pole as part of a new air mass. At latitudes around 60° north and south, the air again rises, cools and releases precipitation (though less than in the tropics). Some of the cold, dry rising air then flows to the poles, where it absorbs moisture creating the cold climates of the polar regions.

Winds are also generated by the rotation of the earth. Unlike the northern and southern direction of the winds described above, there are westward and eastward winds. These winds affect ocean currents. Warm, tropical waters carry heat pole-ward along the east coast of continents; cold water from the poles is forced toward the equator along the west coast. Warm surface currents can carry heat well away from the tropics, bringing temperate climates to areas nearer the poles than the Equator. Deeper currents are driven by a combination of Earth’s rotation and temperature differences between the tropics and the poles. Cold, dense melted water from the icecaps flows underneath warmer surface waters towards the Equator. The combination of wind and ocean currents redistributes heat and moisture across Earth’s surface. Around 60% of the solar energy that reaches the earth is redistributed around the planet by atmospheric circulation and around 40% by ocean currents.

Out of this interplay between our spherical orbiting planet, sun and oceans, global regions rise that divide the year into dry and wet periods.

For so many of us in the developed world, the seasons are defined by temperature. The freshness of spring, the heat of summer, the chill of autumn and the cold of winter. But for the billions of people on our planet that live in the tropics, the seasons are marked by the presence, and absence, of rain. The annual coming of the rains after months of drought, with the renewal of life from the giving water… And then, after months of rain and clouds, the sun reborn into blue skies as the next dry season begins. This is the domain of the tropical wet and dry climates. This is the Tropical Monsoon and the Tropical Savannah.

The global extent of the tropical Monsoon-Savannah wet and dry regions are shown in figure 2 with a short description below:

Figure 2
Tropical Wet and Dry Climate (Source: climatetypesforkids.com)

Tropical Wet and Dry climate is mainly found within the tropics. The tropics are two lines of latitude about 23.5 degrees north and 23.5 degrees south of the Equator. Land in this area receives direct sunlight throughout most of the year. Tropical Wet and Dry is known for its two seasons.

This band is further explained in the NOAA entry.

The Inter-Tropical Convergence Zone (ITCZ) appears as a band of clouds consisting of showers and occasional thunderstorms that encircles the globe near the equator. The solid band of clouds may extend for many hundreds of miles and is sometimes broken into smaller line segments. Its existence is due to the convergence of the trade winds: winds in the tropics that move predominantly from the east and curve towards the Equator. When the northeast trade winds from the Northern Hemisphere and the southeast winds from the Southern Hemisphere come together, it forces the air up into the atmosphere, forming the ITCZ.

The geographic extent of the ITCZ in Australia (see the previous NOAA citation) is seen in figure 2. The timing of the dry phase (Feb-March –> August-Sep) coincided with our visit. The temperature of this climate band is approximately constant (70 – 87 F (21-30C)) and the dry weather seemed to be the ideal reprieve for tourists coming from the Northern hemisphere.

Figure 3
Mediterranean Climate (Source: http://www.grabovrat.com/mapsViews/mapsViewsMB00.html)

Mediterranean climate is very pleasant climate with warm, dry summers and cool, mild winters. It gets its name from the Mediterranean Sea. Most of the coastal land around the Mediterranean Sea experience this climate. This climate’s most important cause is the large bodies of water near the land around the Mediterranean and is only found along the coast.

I have some experience living with different kinds of wet/dry climate in different locations. It is known as the Mediterranean Climate. The geographic extent and short explanation of that band is shown in Figure 3. As was mentioned in earlier blogs, I grew up in Israel which is part of that climate band and did part of my early academic career at the University of California Berkeley, in the San Francisco Bay area. I remember fondly my Berkeley years (early 1970s.) and the climate there. Many were surprised that there were no conventional seasons there (at least as temperature was concerned). Often, they didn’t like it because they grew up with seasons. The remedy was that they could travel to “extreme” seasons – to mountains looking for “real” winter (snow) and to deserts for “real” summer (cactus trees and sand in the south).

However, recent changes in parts of the region that were covered by the Mediterranean Climate that historically were considered the “Cradle of Civilization” and “Birth of the Agricultural Revolution,” are now going through desertification almost unfit for human habitation. I will follow these developments in future blogs.

The next blog will expand (with some pictures) on finding the weather (and more) in Darwin. I will show that Darwin, in terms of weather, is the “Garden of Eden” for tourists in the dry season. It is something else in its wet season.

 

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The Conflicting Reasons for my Australian Vacation

Figure 1 – Map of Australia (Source: Geology.com)

Figure 2 – The three national parks around Darwin

My wife and I are back from a three-week vacation in Australia. In this blog, I will try to explain why we went there in the first place and why my next series of blogs will be dedicated to this trip. The trip was structured so we spent half of the time with family in Melbourne and the other half of the time in Darwin and the surrounding national parks. As strange as it sounds, both halves connected to the rapid changes that now afflict our planet, and to which this blog is dedicated. However, the connection to climate change of such a trip is unquestionably problematic: the flying distance from New York City, where we live, to Melbourne is 16,763 km (10,418 miles). In addition, the distance between Melbourne and Darwin is 3,740 km. There is no question that flying such distances is not good for the planet. To add to that, both my wife and I are of an advanced age (I am of a considerably more advanced age than my wife) and our health is fragile. Flying such distances in economy class is brutal for our bodies. Fortunately, we could afford to fly business class. By doing so, however, we doubled the environmental impact of our flights.

The main driving force that led us to take the trip was the family trip to Melbourne. My family there started with my cousin (his father and mine were brothers), who is eight years older than me, also born in Warsaw, Poland. Unlike me, he encountered the Nazi invasion at the age of 8 (I was 3 months old when the Nazis invaded Poland). He survived the Holocaust and after a few years in Israel, he ended up in Melbourne with his stepfather and his mother. A few months ago, he was interviewed in Australia about his early experiences. Recently, he lost his wife, and we felt a strong urge to spend some time with him and his family. I will dedicate a future blog to making a case for constructing massive societal family trees until we demonstrate that all of us are members of the same family and thus share responsibility for each other’s well-being.

Summer break usually gives faculty time to “rearm” themselves with developments in their fields. The trip to Darwin—and to the surrounding national parks shown in Figure 2—was designed to accomplish that while also catering to our interest in exploring unfamiliar parts of the world.

July is mid-winter in Melbourne. During our stay, we had one rainy day. It was very pleasant to walk around, but less pleasant to swim. We went to Darwin to experience something different. As can be seen in the opening map, Darwin is at the northern tip of the continent. There is no winter or summer there per se, but there is a dry and a wet season. We were there at the height of the dry season, with temperatures that we might associate with a mild summer (around 25oC or 77oF). Darwin is the capital of the Northern Territory of Australia, with relatively few residents (but a lot of tourists).

The last two blogs, one by me and the other by Sonya Landau, focused on the water stress in Arizona and its conflicts with population growth. Water stress is one of the most important impacts of climate change on Arizona and many other parts of the world. Adaptation to the dry season is one of the most important tools to adapt to climate change. The visit to Darwin taught me how nature can create wonders in the wet season and how the landscape can adapt to water stress during the dry season. The next blog will try to explore these trends further.

We had some surprises in Australia that have nothing to do with environmental impact and thus will not be expanded to separate blogs. The biggest surprise (at least to me) was the news that I really didn’t need to bother exchanging my American dollars for Australian ones. We were told that—at least in the places that we planned to visit—nobody uses cash. We didn’t believe our sources and got some Australian dollars anyway. It turned out our sources were right. In Melbourne, the only place that required cash was a small Chinese restaurant where we had lunch. In Darwin, at the entrance to the Hilton hotel where we stayed, there was a sign, shown in Figure 3.

Photo of blue and white sign that says "This hotel is cashless, no money on site"Figure 3 – The “warning” on Darwin’s Hilton door

We didn’t bother to inquire what was behind the story that made management post the sign. When we went out, the soft drink machines (shown in Figure 4) made the overall shift to a “cashless” economy clear.

Photo of two soft drink vending machines. Both say "100% cashless" at the top.Figure 4 – Soft drink machines in Darwin.

Before leaving Australia, we had to change almost all our Australian money back to American dollars. I didn’t use the trip to start the conversation about the impact of such a shift on people who cannot open bank accounts and get credit cards, however, I have no doubt that such a conversation will start if the trend expands beyond the Australian borders.

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Vacation Notice

This week I am taking a break from the blog, so there will be no post. Please do come back next Tuesday, when I promise to continue our discussions.

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Sonya Landau Guest Blog: Arizona: Water Shortage vs. Population Growth

Hi, I’m Sonya Landau. I’ve been Micha’s editor for this blog since the beginning, and have contributed a couple of guest blogs over the years regarding Tucson, water, and heat (see the and June 22, 2021 posts). Given that his latest topic is Arizona and the conflict between population growth and water scarcity, I agreed to weigh in again here.

Population Growth

Last week, Micha mentioned the population of the Phoenix metro area, which is growing astronomically. According to the Arizona Commerce Authority, as of 2022, the area boasted a population of 5,040,400 and is projected to reach 8,035,300 by 2052. It is one of the fastest-growing cities in the nation. I’m a native Arizonan and I love the Sonoran Desert. I also understand the lure of relatively low real estate costs. Still, the idea of so many people moving to a place where it regularly reaches over 110oF for extended stretches during the summer and which has a history of chronic drought seems especially absurd in the face of climate change, which promises to worsen both the heat and the availability of water. In contrast, the Tucson area is (fortunately) growing slower. In 2022 it had 1,072,300 people and is expected to reach 1,436,500 by 2052. As Micha has mentioned, there is a very real chance in the not-so-distant future that many Arizona residents will become climate refugees seeking shelter in more temperate areas.

Of course, one of the key considerations in the sustainability of this growth is water. Arizona has had laws since 1980 that require developers in cities to prove a 100-year water supply for each new project that does not rely exclusively on groundwater. The goal is to avoid overtaxing and depleting the finite groundwater reserves. Last month, the state halted approval of some of the construction projects near Phoenix because of doubts about water availability. Already approved projects will continue, as will new ones that exclusively use surface or recycled water rather than groundwater.

The Colorado River and Water Rights

Arizona’s other main water source, the Colorado River, has also been in the news lately for its record low levels and the ongoing battle for usage rights between the lower Colorado Basin states: Arizona, California, and Nevada. The original allotments overestimated supply, based on projections made during a period of extremely high flow, and resulted in problems when the water level dropped. Earlier this summer, the states reached an agreement about how the water will be distributed going forward in light of the historic megadrought and expected effects of climate change. Aside from these states, however, there is also the matter of Native American tribal water rights—in this case, those of the Navajo Nation, which spans parts of Arizona, New Mexico, and Utah. There has been a long legal battle to secure water for the struggling area, based on the 1868 treaty, which created the reservation with the promise of a “permanent home.” Unfortunately, last month the Supreme Court ruled against the tribe, denying that the US has obligations to provide reliable water sources on reservations.

Agriculture and Virtual Water

The 1980 law that governs water usage in Arizona’s cities is unhelpful when it comes to the resource’s use in other situations. Arizona has an enormous agricultural industry, and there are very few regulations on water use for farming. According to CNN, “In around 80% of the state, Arizona has no laws overseeing how much water corporate megafarms are using, nor is there any way for the state to track it.” In other words, there are virtually no protocols or procedures in place for the state to establish oversight, much less control.

Oddly, many of the crops grown in Arizona are especially thirsty and ill-fitting for a drought-ridden area. Micha has mentioned the concept of virtual water—the amount of water needed to grow a specific thing. That thing could be a single strawberry or almond, whose water intake is easy to track, or it could be something more complicated, like beef. In this instance, you must first calculate not only how much the cow drinks but also aspects such as how much water goes into growing its food (which is often grown elsewhere). The argument is that exporting produce that was grown with a lot of water in a water-insecure area amounts to the theft of critical natural resources. One of the most prominent crops grown in Arizona (and other places like California) is alfalfa, a type of hay that is used precisely for feeding cows and other livestock. It is a lucrative crop but it also requires an immense amount of water.  This is an especially sensitive subject because much of the crop is grown by foreign companies who export it to feed livestock in other countries. Ironically, one of the biggest farm corporations is from Saudi Arabia; it moved to the US because its own country outlawed the growth of such crops in its arid lands. This summer, Arizona officials have started to crack down on these foreign companies by restricting well permits. Additionally, towns and regions across Arizona are debating new regulations on agricultural water practices, including among people who have traditionally balked at governmental oversight.

Arizona’s governor, Katie Hobbs, also introduced a 100-year study of Phoenix’s groundwater. Additionally:

Governor Hobbs announced a $40 million investment of American Rescue Plan Act funds to spur increased water conservation, fund critical water infrastructure, and promote sustainable groundwater management throughout the State. The Arizona Water Resiliency Fund will be administered by the Arizona Department of Water Resources to facilitate sustainable groundwater management through grants and financial support for pressing water resiliency efforts.

This is a continuing conversation that involves both government officials and community leaders/activists. On the latter side, there is a podcast called Thirst Gap, which addresses how people in the Southwest are coping with a decreasing water supply.

Resilience

Clearly, the high-paced growth of Arizona cities—while alarming—does not show the full picture of Arizona’s water woes. Nor does the number of people moving here (especially to Phoenix) seem to be slowing. There are, however, a few steps that can be taken to make growth more sustainable in the desert. Part of that comes back to neighborhood planning and communication of services. Last week, Micha pointed out the precariousness of heat safety here, and what would happen in the event of a power outage. Several organizations—both governmental and nonprofit—have produced guides with strategies for creating resilient cities and neighborhoods. One such guide describes the issue at hand:

Resiliency is a critical characteristic that allows healthy communities to respond to unknown future changes. Social, economic, political, and environmental changes occur frequently in communities and an ability to adapt to these changes is essential to maintain community health.

The guides pay special attention to the dangers of the deadly Arizona heat and how to mitigate and adapt to potential disasters. These measures include public cooling centers, resilience hubs, identification of especially vulnerable groups, community outreach, and the creation of urban forests/green spaces.

I do not know to what extent these measures will have an immediate or lasting effect on water usage/conservation in the state. I’m not convinced that those who are part of the massive population influx are aware of or willing to help confront the problems but there are plenty of groups of local Arizonans that are making a demonstrable difference. I will list several of these below in case you want to know more.

Resources

Awareness Ranch

Dunbar/Spring Neighborhood Foresters

The Guardian: Dunbar/Spring urban food forest

Live Well Arizona: Resiliency

Oatman Flats Ranch

Phoenix regenerative agriculture

Physicians for Social Responsibility Arizona: Building Resilient Neighborhoods (BRN) Citizens’ Guide

Planning.org: Urban Heat Resilience

Rainwater Harvesting for Drylands and Beyond by Brad Lancaster

The Urban Farm in Phoenix

US Department of Agriculture: Southwest Watershed Research Center in Tucson

Watershed Management Group

Posted in Climate Change | Leave a comment

Arizona: Remedies for Water Shortage

By the time that you read this blog (and the next two), I will be in Australia. I will return toward the end of the month, and I will write about some of my experiences. In this blog and with the one that will follow, I will abandon my dark glasses from the last blog and focus on places that are trying to make our life brighter. I am starting with Arizona.

Arizona has been in the news often recently, and not always for the better. Its place in the news is often dominated by two issues: politics and the impact of climate change. The latter focuses especially on rising temperatures and water stress. I am following the daily temperature in the two biggest cities: Phoenix and Tucson. Starting in mid-May, when almost everywhere else in the US was still experiencing spring, the temperature there already hovered around 100oF. It is predicted to go considerably higher this summer, in part due to El Niño’s impact. Toward the end of May, a research article came out in the Journal of Environmental Science and Technology titled, “How Blackouts during Heat Waves Amplify Mortality and Morbidity Risk,” written by 14 coauthors, with Brian Stone Jr. as the corresponding author. The abstract is cited below:

The recent concurrence of electrical grid failure events in time with extreme temperatures is compounding the population health risks of extreme weather episodes. Here, we combine simulated heat exposure data during historical heat wave events in three large U.S. cities to assess the degree to which heat-related mortality and morbidity change in response to a concurrent electrical grid failure event. We develop a novel approach to estimating individually experienced temperature to approximate how personal-level heat exposure changes on an hourly basis, accounting for both outdoor and building-interior exposures. We find the concurrence of a multiday blackout event with heat wave conditions to more than double the estimated rate of heat-related mortality across all three cities, and to require medical attention for between 3% (Atlanta) and more than 50% (Phoenix) of the total urban population in present and future time periods. Our results highlight the need for enhanced electrical grid resilience and support a more spatially expansive use of tree canopy and high albedo roofing materials to lessen heat exposures during compound climate and infrastructure failure events.

Phoenix’s population is now estimated to be 1.6 million and it is the fastest-growing city in the US. Counting the entire Phoenix-Mesa-Scottsdale metropolitan area, that number is almost 5 million. One of the conclusions of this article is that in case of a heat wave with power failure, 50% of the population would require medical care – that’s 800,000 people (or 2.5 million in the Phoenix metro area)! This is serious. As we can see below, the water availability cannot keep up with the growth:

Underground storage may be a key for Western states navigating water shortages and extreme weather.  Aquifers under the ground have served as a reliable source of water for years. During rainy years, the aquifers would fill up naturally, helping areas get by in the dry years. But growing demand for water coupled with climate change has resulted in shortages as states pump out water from aquifers faster than they can be replenished. The fallout can also lead to damaged vegetation and wildlife as streams run dry and damage to aqueducts and flood control structures from sinking land. Municipalities and researchers across the country are working on ways to more efficiently replenish emptied-out aquifers.  By over pumping aquifers “you’ve created space. There’s space under the ground that used to be filled with water,” explained Michael Kiparsky, water program director at the Center for Law, Energy & the Environment at the University of California, Berkeley School of Law.   “And what we can do with these groundwater recharge projects is take advantage of that space, which is vastly greater than the sum of all of the surface storage reservoirs that exist now or could be built,” he said. Several communities across California, Arizona and other states have been using managed aquifer recharge for years to better regulate local water supplies.  If implemented on a wide enough scale, recharge projects hold the potential to bolster water security in drought-stricken regions while improving the health of the environment.  Kiparsky said if it can be pulled off, “it holds the promise of being able to generate a whole new water supply we really didn’t even know that we had.”

Water stress is a serious issue. I wrote about it in previous blogs (See “Human Reaction to Climate Shift” from November 1, 2022, and “Adaptation and Affordability” from December 6, 2022). As I said then:

In rich countries, such as the United States …in many cases, people are counterintuitively flocking to the most vulnerable places. Most of the fastest-growing states in the United States are in the West and South. In terms of the climate change impacts, the South is known for its floods and the West for its fires and droughts

Now, Arizona seems to  have done a U-turn and is trying to limit construction in certain areas to try to match growth with available water supply:

As the mayor of an old farming town bursting with new homes, factories and warehouses, Eric Orsborn spends his days thinking about water. The lifeblood for this growth is billions of gallons of water pumped from the ground, and his city, Buckeye, Ariz., is thirsty for more as builders push deeper into the desert fringes of Phoenix.

But last week, Arizona announced it would limit some future home construction in Buckeye and other places because of a shortfall in groundwater. The worried calls started pouring in to Mr. Orsborn.

“I have neighbors who come up to me and say, ‘What are you doing? Are we running out of water?’” Mr. Orsborn said. “It put our community on edge, thinking, ‘What is going on here and do I need to move?’”

No, he tells them. Breathe.

The upheaval was caused by a new state study that found groundwater supplies in the Phoenix area were about 4 percent short of what is needed for planned growth over the next 100 years. That may feel like a far-off horizon, but it is enough of a change to force the state to rethink its future in the near and long terms.

Arizona has some of the strictest groundwater laws in the country in more regulated areas like Phoenix. For decades, the state has required new developments to show they have a 100-year supply of water before they can sell lots or break ground.

Arizona is also trying to increase its water supply by using desalination. However, a quick look at the map below shows that Arizona doesn’t have access to the ocean. What it has is a border with California, which has a long ocean shore. However, California, for a variety of reasons, also has massive water stress. For a long time, the state has been considering constructing water desalination systems. I wrote about it 10 years ago (See the November 12, November 19, and December 3, 2013 blogs). The feedback on my writing by a Californian expert on the water issue (Peter Gleick) can be found in the November 19, 2013 blog.

(Source: Wikimedia SVG map of the United States, Created by Wapcaplet)

I tried to get more recent information on desalination efforts in California and ended up with one company:

Environmentalists say desalination decimates ocean life, costs too much money and energy, and soon will be made obsolete by water recycling. But as Western states face an epic drought, regulators appear ready to approve a desalination plant in Huntington Beach, California.

After spending 22 years and $100 million navigating a thicket of state regulations and environmentalists’ challenges, Poseidon Water is down to one major regulatory hurdle – the California Coastal Commission. The company feels confident enough to talk of breaking ground by the end of next year on the $1.4 billion plant that would produce some 50 million gallons of drinking water daily.

Arizona was apparently familiar with desalination efforts in California and decided to try to build its own facility in Mexico:

Fifty miles south of the U.S. border, at the edge of a city on the Gulf of California, a few acres of dusty shrubs could determine the future of Arizona.

As the state’s two major sources of water, groundwater and the Colorado River, dwindle from drought, climate change and overuse, officials are considering a hydrological Hail Mary: the construction of a plant in Mexico to suck salt out of seawater, then pipe that water hundreds of miles, much of it uphill, to Phoenix.

The idea of building a desalination plant in Mexico has been discussed in Arizona for years. But now, a $5 billion project proposed by an Israeli company is under serious consideration, an indication of how worries about water shortages are rattling policymakers in Arizona and across the American West.

The pipeline is proposed to move desalinated water from Mexico to Phoenix. There is a strong likelihood of it passing close to Tucson. Tucson is the second largest city in Arizona; its present rate of growth is considerably slower than that of Phoenix. However, most of the water-related policies are decided at the state level. We are fortunate to have a friend in Tucson: Sonya Landau, the editor of this blog (see her guest blogs from June 22, 2021 and October 9, 2018). It will be fascinating to see her take on Arizona’s fight between water and growth in next week’s guest blog.

Posted in Climate Change, US, Water | 1 Comment

Phase Transition in People’s Movements

(Source: Mitratech)

As I mentioned in earlier blogs, my spring semester is over, and the summer break has started. My wife and I have been dealing with some health issues and we were thinking seriously about staying home, recuperating, and doing some home-bound research (AI??) to get us ready for the Fall semester that starts at the end of August. Then, the sky turned orange on us, Manhattan became invisible, and there were predictions that the situation will worsen when El Niño comes to visit later in the summer. The issue isn’t confined to where I live, either. Local scenes all over are predicted to expand and worsen:

As climate change drives an increase in wildfires, we’re seeing more smoke lofted into the upper atmosphere each fire season. Depending on wind and weather, this smoke can spread hundreds or thousands of miles from its source—as we saw in early June on the U.S. East Coast.

And we’re likely to continue seeing it increase in severity, frequency, and longevity as the planet warms.

In addition to these prospects, the head of our family in Australia (my cousin – older than me!!) is not in great shape. We decided it’s time to forget all our problems here and visit him in Australia (it’s the start of winter there). We leave soon.

Meanwhile, the climate crisis is also starting to take shape as a financial crisis:

This month, the largest homeowner insurance company in California, State Farm, announced that it would stop selling coverage to homeowners. That’s not just in wildfire zones, but everywhere in the state. Insurance companies, tired of losing money, are raising rates, restricting coverage or pulling out of some areas altogether — making it more expensive for people to live in their homes. “Risk has a price,” said Roy Wright, the former official in charge of insurance at the Federal Emergency Management Agency, and now head of the Insurance Institute for Business and Home Safety, a research group. “We’re just now seeing it.”

It’s not just the insurance companies that are calculating the livability of different places. According to ProPublica:

Climate change is remapping where humans can exist on the planet. As optimum conditions shift away from the equator and toward the poles, more than 600 million people have already been stranded outside of a crucial environmental niche that scientists say best supports life. By late this century, according to a study published last month in the journal Nature Sustainability, 3 to 6 billion people, or between a third and a half of humanity, could be trapped outside of that zone, facing extreme heat, food scarcity and higher death rates, unless emissions are sharply curtailed or mass migration is accommodated.

In an earlier blog (September 17, 2019), I tried to explain how a mama polar bear teaches her cubs the nature of phase transition by noting the sizes of icebergs floating in the surrounding water and pointing out how they constantly change. That blog was focused on energy transition. This blog is focused on people’s attempts to move when they face changes that they don’t like. I started it with my simple vacation announcement (getting out of NYC). There’s been another major movement: as a result of COVID-19, it was a necessity, for a time, to do much of our work from home. Technology developed that enabled many of us to do so much more conveniently. This technology stays with us, even as the pandemic is abating, triggering major societal changes.

Dictionary.com distinguishes between the movements of people, starting with the following introduction:

There are a lot of words to refer to people who move from one place to another. Some are used in overlapping ways, but there are key differences between many of them, including whether the person is coming or going, and for what reasons.

The dictionary chooses to concentrate on differentiating between the following classes of movement:

⚡ Quick summary

  • emigrant vs. immigrant: An emigrant is someone who emigrates—moves away from a country. An immigrant is someone who immigrates—moves to a different country. Both words can apply to the same person—a person must first emigrate to immigrate. However, these terms are often used to distinguish different groups, such as when tracking how many people are moving to a country and how many are moving away.
  • immigrant vs. migrant: Migrant can generally refer to a person who moves from one place to another (or back and forth). It’s often used more specifically to refer to a migrant worker (who moves from place to place for work) or as another way of referring to an immigrant (which implies permanent relocation), especially one who may be subject to removal from the country they are trying to relocate to.
  • migrant vs. refugee: Refugee specifically implies that a person is fleeing their country for their safety, often due to war or political persecution. This may be the case for many migrants, but the word itself does not imply this, and the term is used more broadly.
  • refugee vs. asylum seeker: Asylum seeker specifically refers to a person who applies for refuge or asylum in a foreign country or its embassy, especially for political reasons. Some refugees may be asylum seekers, but not all asylum seekers necessarily consider themselves refugees.

The smaller movements, such as travel and workplace choices, are not mentioned; these include the “movements” that I am currently engaged in. These small movements are mostly voluntary and taken by people that can afford them, as opposed to the mostly forced movements described by the dictionary. In a sense, I started my life among those labels listed above—the Holocaust forced me to migrate—and I am closing my life as a voluntary traveler.

The constant movement of people throughout the world is not new; nor is such movement unique to humans. Everything that can move does so to better their survival prospects. Our current situation is introducing natural limits to both human population and livable places. Now climate change, driven by anthropogenic changes in livable places, is accelerating those limits and converting the situation to a phase transition. There are two main phases as I see them: either the availability of living places decreases to a degree that might drive the human race to extinction, or we adapt and mitigate the changes, allowing humanity to flourish in the future. The latter option would depend on transitioning our energy use to fusion and thus converting Earth to a “star” that will circle the sun as a binary system with robotic, artificial intelligence to guide humanity’s long-term existence. Based on our current global governing system, if I were a betting man, I would bet on the dark side (extinction), and do what I could to shift the prospects.

Let us examine a bit more closely the prospective limits to living space:

Globally the exponential population increase over the last century has driven various movements based on the final sizes of the habitable land. One of my favorite science blogs gives an overview:

Landcover is one key way that we can measure how much of the terrestrial environment has been covered by humans. Earth’s surface is about 500 million km2, but most of that (70.8%) is water, which we’re not really very good at. So ignoring oil rigs and the occasional cruise liner, we’re only talking about a total possible land surface to cover of roughly 149 million km2.

The thing is, landcover is something that is changing (and our technology to estimate it is improving) constantly, so even fairly recent estimates may already be out of date. A meta-analysis in 2011, which included 326 studies of urban landcover using remote sensing technology such as satellite images, found that urban landcover increased by nearly 60,000 km2 between 1970 and 2000.

In the year 2000, estimates suggest that globally, urban land covered somewhere between 700,000 and 3.5 million km2 – but that’s a pretty big margin of error. The meta-analysis found that the largest rates of increase in urban landcover were seen in India, China and Africa, while North America experienced the largest total change since 1970. In all regions, urban land expanded either faster or equivalent to population growth rates, suggesting our societies are also becoming more expansive.

Using data from 1970 to 2000, the researchers then tried to project future urban land cover change – their results predict that global urban landcover will increase by a further 1.5 million km2 by 2030. Over half-way to this prediction, where are we now?

Trying to explain the consequences of humanity’s movements to her cubs is a big job for a mama polar bear, and I am afraid that it will not get easier—either for her or the rest of us.

Posted in Climate Change, immigration | Leave a comment

Prerequisites Part 2: Continuing Education

(Source: Education Corner)

Last week’s blog ended with the following two short paragraphs:

Mid-career or career-shift education seems to be the right remedy for acquiring job-relevant knowledge of the fast-changing reality. Adult education is being offered now in many colleges. I will expand on this issue in my next blog.

I’m not sure that everyone needs to go back to school but we do need to take care of dangerous gaps in our knowledge as they affect our decisions, especially when those decisions can have such an enormous impact. I will discuss this more in next week’s blog.

This blog will try to put some content behind these statements.

A broader introduction to continuing education is cited below:

Continuing Education is a form of education that most professionals need to pursue after their formal education to have the most updated knowledge in their field of expertise. There are many mediums and methods for such programs; they would vary from one-time classes, conferences, online courses, and post-degree programs.

Although not all professions require this continuous learning, most specialized careers do. For example, in the medical field, doctors need to continually study and learn new and advanced methods for treating their patients. Health care specialists need to stay current in improving the welfare of everyone. The same thing applies to lawyers, politicians, scientists, professors, and many more experts.

This will prepare you to handle new responsibilities and create better opportunities too. With the continually changing of the globalized society, continuing education will be more commonplace shortly. Even notable people and people in business around the world are advocates of it.

Learning is a lifetime process, so make the most of it by taking advantage of the different sources and platforms for continuing education.

The key relevant sentence in that quote is the last one, particularly in an environment in which reality changes are accelerating at the rate that we are observing.

An earlier blog that was focused on the forecasted population decline (March 7, 2023) showed a global map comparing changes in the 65+ age group, between 2015 and 2050. It indicated a major increase in elderly people. I focused specifically on the developed world, where this shift is accompanied by major increases in social spending on this segment of the population. A more recent accounting goes even further, predicting a decline toward 6 billion by the end of the century (from about 10 billion at the peak around the mid-20th century) with a commensurate accelerated increase in the proportion of the elderly. These newer data indicate that the largest 15 countries by GDP all have fertility rates below replacement (this includes India and China) and that globally we are quickly approaching replacement.

I am 84 years old. My wife is younger but not by much. We both have tenure at the same school, and have decided not to retire as long as we can be effective, both in our teaching and service to our institution. Throughout our long academic careers, we have also had the opportunity to take sabbatical breaks, during which we were able to observe the accelerated changes in the reality that surrounds both our professional and private lives. This practice is not unique to our institution; it runs across much of the academic world.

I have mentioned earlier that I have family in France, with whom we are trying to maintain as much contact as we possibly can (see the December 18, 2018 blog, in the context of the Yellow Vests demonstrations). One of the family members, a physician by profession, visited us a few months ago, with her immediate family. She stayed for a week and enjoyed the experience. I asked why she couldn’t stay longer, and she answered that she had to return to work to take over a temporary managerial position. I asked her to consider taking a sabbatical in NYC so we could spend more time together. She didn’t know what I was talking about, and I realized immediately how unique academic situations are. I tried to Google to find out which companies offer a paid sabbatical to their employees and I got a list that looked more like opportunities for extended vacations. They are nice but they are not academic sabbaticals.

I am fully aware that most people go through life without the benefits of higher education. This is particularly true in developing countries, but it is also true in rich countries. The numbers are shown in Figure 1. The bigger issue is primary education and not higher or continuing education (for many, it comes down to gender equity more than the availability of educational institutions).

However, the issues of equity in educational availability and the availability of continuing education are different. In today’s environment, attaining higher education in some form is not a prerequisite for understanding changing environments. It is, however, a tool required to successfully adapt to the changing environment and be able to make a living. There is a difference.

Figure 1 (Source: UNESCO Institute of Statistics via World Resources Simulation Center)

At least in developed countries, and many developing countries, the infrastructure for higher education exists. The infrastructure for continuing education also exists but is a bit chaotic. Higher education is focused on degree programs: you register for a degree, the school states the requirements for the degree, and you follow them. Usually, the degree programs are divided into departments, each of which administers the degree in its particular areas. In principle, most of the courses that are available for degree programs are also available for general education. However, many of the courses (especially in the sciences) are vertical, meaning there are prerequisites for taking them. For a degree program, the responsible departments will set out a degree map, which ensures that you will meet the prerequisites. If you just enroll in a course, paying no attention to the prerequisites, chances are that you will be completely unprepared and will drop out of the course, wasting your time and money.

Back to the first of the two sentences I quoted at the beginning, from last week’s blog:

One of the best ways that is presently being employed to ascertain that job holders follow the changing realities and the progress in their specific areas is to require a license for practitioners. We are used to licenses that give us permission to do stuff, such as drivers’ licenses, passports, and identity cards. Many of the licenses come with expiration dates that require passing some tests before renewals. In the US, most of the licenses are issued by states. From personal experience, growing up and being educated in Israel, many of my friends who attended medical schools took the American exams to practice medicine in some US states as a matter of routine. The rationale was that the demanding tests should not be a problem immediately after finishing medical school but might present a bigger challenge after a year or two out of school.

Business News Daily has a list of professions that require a license:

You already know you need a license to become a truck driver, but did you know that nearly 1 in 4 occupations in the U.S. now require a license? According to data from the U.S. Bureau of Labor Statistics, about 23% of full-time workers have a license or certification.

Requirements for renewals can be demonstrated by the following regulation in Texas:

Continuing professional education (CPE) is required to renew a standard certificate. Your certificate will be set to inactive status if you do not renew by the expiration date. CPE hours are required, even if your certificate has already been set to inactive status. Certificates cannot be renewed by completing examinations. 

  • Classroom teachers must complete 150 CPE hours.
    • No more than 150 CPE hours are required, even if you hold multiple classroom certificate areas.
  • If you hold an administrative and/or student services certificate you must complete 200 CPE hours.sw
  • No more than 200 CPE hours are required, even if you hold multiple certificates, such as: classroom, administrative and student services certificates.

General CPE information is located on the Continuing Professional Education Information page, along with renewal FAQs.

I added the emphasis on the non-exam requirements to show that there are other ways to measure continued learning within a field.

License requirements are not based on the “noble” wish that we stay up-to-date in our professions. In many cases, the practice is also strongly motivated by the not-so-noble desire to limit competition in the profession. I reserve this issue for a separate discussion.

Should we require a license before approving a US supreme court judge or mandate renewal requirements? I don’t think so! There are effective alternatives. In the case of the US Supreme Court, the chief justice could try to periodically (once every five years?) sort the cases in front of the court into a semi-disciplinary data collection and (politely) ask  every judge to be the point man/woman in that area. It would be at the judge’s discretion to determine if he/she needed additional education in his/her area. That judge would not have different voting powers in his/her areas of specialty, but he/she would be asked to update fellow judges on the latest developments in that particular field.

For higher education institutions, it would be both convenient and doable to expand existing educational structures to include certification demands. In today’s environment, this is already done in schools of education in universities.

Posted in Education | Leave a comment

Prerequisites for Supreme Court Judges


(Source: MarcusObal on Wikimedia)

“Playing with fire” is an idiom that has become popular on more than one level. Cambridge Dictionary describes it as “to act in a way that is very dangerous and to take risks.” I am writing this blog in NYC, which is currently (hopefully for only a short time), the most polluted big city in the world, due to a weather system driving the smog from major wildfires in Eastern Canada in our direction. One can combine this idiom with reality in many major environmental indicators. To demonstrate the issue and offer a possible solution, I will start with the US Supreme Court. About two weeks ago, the Supreme Court announced an important, unanimous environmental decision, the essence of which is summarized in the New York Times article below:

After half a century of painstaking restoration under the Clean Water Act, streams and wetlands nationwide are once again at risk of contamination by pollution and outright destruction as a result of a ruling on Thursday by the Supreme Court.

The Environmental Protection Agency has long interpreted the Clean Water Act as protecting most of the nation’s wetlands from pollution. But now the court has significantly limited the reach of the law, concluding that it precludes the agency from regulating discharges of pollution into wetlands unless they have “a continuous surface connection” to bodies of water that, using “ordinary parlance,” the court described as streams, oceans, rivers and lakes.

At least half of the nation’s wetlands could lose protection under this ruling, which provides an even narrower definition of “protected waters” than the Trump administration had sought.

The full ruling is posted on the court’s webpage.

I want to emphasize that although the ruling was unanimous, it came with four separate justifications, each of which will probably have a strong impact in terms of the future authority of the EPA or, more broadly will put such authority to the test again in a not-so-distant future. Below is the essence of Justice Kavanaugh’s separate reasoning (to which the three liberal justices joined). He agreed with the ruling but was troubled about the potential ramifications:

I write separately because I respectfully disagree with the Court’s new test for assessing when wetlands are covered by the Clean Water Act. The Court concludes that wetlands are covered by the Act only when the wetlands have a “continuous surface connection” to waters of the United States—that is, when the wetlands are “adjoining” covered waters. Ante, at 20, 22 (internal quotation marks omitted). In my view, the Court’s “continuous surface connection” test departs from the statutory text, from 45 years of consistent agency practice, and from this Court’s precedents. The Court’s test narrows the Clean Water Act’s coverage of “adjacent” wetlands to mean only “adjoining” wetlands. But “adjacent” and “adjoining” have distinct meanings: Adjoining wetlands are contiguous to or bordering a covered water, whereas adjacent wetlands include both (i) those wetlands contiguous to or bordering a covered water, and (ii) wetlands separated from a covered water only by a man-made dike or barrier, natural river berm, beach dune, or the like. By narrowing the Act’s coverage of wetlands to only adjoining wetlands, the Court’s new test will leave some long-regulated adjacent wetlands no longer covered by the Clean Water Act, with significant repercussions for water quality and flood control throughout the United States. Therefore, I respectfully concur only in the Court’s judgment.

In different words, Justice Kavanaugh is accusing some of his colleagues of being ignorant about basic environmental workings, like the interconnections of the global water cycle. To put it more broadly, he accuses other justices of playing with fire when it comes to our environmental well-being.

The last few blogs (starting on April 25th, with the Earth Day blog) focused on colleges’ attempts to include the accelerating global realities that will affect students throughout their lifetimes into the official strategic plans. I indicated that faculty can be prepared for such instruction only through conducting and/or following timely research. Most of these reality changes are anthropogenic. They break the traditional separations of physical and social sciences. It is not surprising that the impact of these changing realities doesn’t stop at the gates of universities but has spread to affect all of us and everything we do, including the role of supreme court judges.

This is starting to come to life in another decision, still pending before the Supreme Court, regarding the admission criteria that colleges and universities are allowed to use. David Brooks makes an interesting point in his op-ed, suggesting that race-based affirmative action be replaced by a class-based equivalent:

We now have whole industries that take attendance at an elite school as a marker of whether they should hire you or not. So the hierarchies built by the admissions committees get replicated across society. America has become a nation in which the elite educated few marry each other, send their kids to the same exclusive schools, move to the same wealthy neighborhoods and pass down disproportionate economic and cultural power from generation to generation — the meritocratic Brahmin class.

And, as Michael Sandel of Harvard has argued, the meritocratic culture gives the “winners” the illusion that this sorting mechanism is righteous and inevitable and that they’ve earned everything they’ve got.

And then we sit around wondering why Trumpian populists revolt.

Worse, this system is built on a definition of “merit” that is utterly bonkers. In what sane world do we sort people — often for life — based on their ability to be teacher-pleasers from age 15 to 18?

The last sentence in the citation can be rewritten: In what sane world do we ask people to perform any job — often for life — based on their ability to be teacher-pleasers from age 15 to 18?

There should be prerequisites for judging environmental issues. We need to redirect, to fill skill deficiencies regardless of age. This is obviously not limited to environmental issues, nor to issues that require a solid science education (STEM). Recently, such a need emerged in another majority decision accusing Andy Warhol of stepping on copyright requirements. Again, it looks like only one minority opinion (Justice Elena Kagan) knew what she was talking about.

Mid-career or career-shift education seems to be the right remedy for acquiring job-relevant knowledge of the fast-changing reality. Adult education is being offered now in many colleges. I will expand on this issue in my next blog.

One good example of how this works is the accelerating emergence of Artificial Intelligence (see ChatGPT) in our everyday life and the emerging realization of the need for government regulations to limit misuse and prevent disasters. A few months ago, one member of Congress recognized the need for more information and took the appropriate step to increase his knowledge of the issue:

For Northern Virginia Congressman Don Beyer, it’s never too late to go back to school. At 72 years old, Beyer — who represents Arlington, Alexandria City, Falls Church and parts of Fairfax County — is a part-time student at George Mason University.

“I’m pursuing a graduate degree in computer science with emphasis on machine learning, and according to George Mason University, that’s the closest to quote unquote artificial intelligence,” said Beyer, a 1972 graduate of Williams College in Massachusetts.

I’m not sure that everyone needs to go back to school but we do need to take care of dangerous gaps in our knowledge as they affect our decisions, especially when those decisions can have such an enormous impact. I will discuss this more in next week’s blog.

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