Tag: University of Vermont

Herman Daly.

A recent article in The Conversation

I was short of time yesterday when I turned my mind to Tuesday’s post. So I hope you won’t mind if I leave you with this very interesting article.


The inconvenient truth of Herman Daly: There is no economy without environment

The economy depends on the environment. Economics can seem to forget that point. Ines Lee Photos/Moment via Getty Images

Jon D. Erickson, University of Vermont

Herman Daly had a flair for stating the obvious. When an economy creates more costs than benefits, he called it “uneconomic growth.” But you won’t find that conclusion in economics textbooks. Even suggesting that economic growth could cost more than it’s worth can be seen as economic heresy.

The renegade economist, known as the father of ecological economics and a leading architect of sustainable development, died on Oct. 28, 2022, at the age of 84. He spent his career questioning an economics disconnected from an environmental footing and moral compass.

In an age of climate chaos and economic crisis, his ideas that inspired a movement to live within our means are increasingly essential.

The seeds of an ecological economist

Herman Daly grew up in Beaumont, Texas, ground zero of the early 20th century oil boom. He witnessed the unprecedented growth and prosperity of the “gusher age” set against the poverty and deprivation that lingered after the Great Depression.

To Daly, as many young men then and since believed, economic growth was the solution to the world’s problems, especially in developing countries. To study economics in college and export the northern model to the global south was seen as a righteous path.

Headshot photo of Daly as an older man, with glasses and thinning hair,
Economist Herman Daly (1938-2022) Courtesy of Island Press

But Daly was a voracious reader, a side effect of having polio as a boy and missing out on the Texas football craze. Outside the confines of assigned textbooks, he found a history of economic thought steeped in rich philosophical debates on the function and purpose of the economy.

Unlike the precision of a market equilibrium sketched on the classroom blackboard, the real-world economy was messy and political, designed by those in power to choose winners and losers. He believed that economists should at least ask: Growth for whom, for what purpose and for how long?

Daly’s biggest realization came through reading marine biologist Rachel Carson’s 1962 book “Silent Spring,” and seeing her call to “come to terms with nature … to prove our maturity and our mastery, not of nature but of ourselves.” By then, he was working on a Ph.D. in Latin American development at Vanderbilt University and was already quite skeptical of the hyperindividualism baked into economic models. In Carson’s writing, the conflict between a growing economy and a fragile environment was blindingly clear.

After a fateful class with Nicholas Georgescu-Roegen, Daly’s conversion was complete. Georgescu-Roegen, a Romanian-born economist, dismissed the free market fairy tale of a pendulum swinging back and forth, effortlessly seeking a natural state of equilibrium. He argued that the economy was more like an hourglass, a one-way process converting valuable resources into useless waste.

Daly became convinced that economics should no longer prioritize the efficiency of this one-way process but instead focus on the “optimal” scale of an economy that the Earth can sustain. Just shy of his 30th birthday in 1968, while working as a visiting professor in the poverty-stricken Ceará region of northeastern Brazil, Daly published “On Economics as a Life Science.”

His sketches and tables of the economy as a metabolic process, entirely dependent on the biosphere as source for sustenance and sink for waste, were the road map for a revolution in economics.

Economics of a full world

Daly spent the rest of his career drawing boxes in circles. In what he called the “pre-analytical vision,” the economy – the box – was viewed as the “wholly owned subsidiary” of the environment, the circle.

When the economy is small relative to the containing environment, a focus on the efficiency of a growing system has merit. But Daly argued that in a “full world,” with an economy that outgrows its sustaining environment, the system is in danger of collapse.

Illustrations of a square (economy) inside a circle (ecosystem). Energy and matter go into and out of the economy square, and some is recycled. Meanwhile solar energy enters the ecosystem circle and some heat escapes. In one, the square is too large.
Herman Daly’s conception of the economy as a subsystem of the environment. In a ‘full world,’ more growth can become uneconomic. Adapted from ‘Beyond Growth.’ Used with permission from Beacon Press.

While a professor at Louisiana State University in the 1970s, at the height of the U.S. environmental movement, Daly brought the box-in-circle framing to its logical conclusion in “Steady-State Economics.” Daly reasoned that growth and exploitation are prioritized in the competitive, pioneer stage of a young ecosystem. But with age comes a new focus on durability and cooperation. His steady-state model shifted the goal away from blind expansion of the economy and toward purposeful improvement of the human condition.

The international development community took notice. Following the United Nations’ 1987 publication of “Our Common Future,” which framed the goals of a “sustainable” development, Daly saw a window for development policy reform. He left the safety of tenure at LSU to join a rogue group of environmental scientists at the World Bank.

For the better part of six years, they worked to upend the reigning economic logic that treated “the Earth as if it were a business in liquidation.” He often butted heads with senior leadership, most famously with Larry Summers, the bank’s chief economist at the time, who publicly waved off Daly’s question of whether the size of a growing economy relative to a fixed ecosystem was of any importance. The future U.S. treasury secretary’s reply was short and dismissive: “That’s not the right way to look at it.”

But by the end of his tenure there, Daly and colleagues had successfully incorporated new environmental impact standards into all development loans and projects. And the international sustainability agenda they helped shape is now baked into the U.N. Sustainable Development Goals of 193 countries, “a plan of action for people, planet and prosperity.” In 1994, Daly returned to academia at the University of Maryland, and his life’s work was recognized the world over in the years to follow, including by Sweden’s Right Livelihood Award, the Netherlands’ Heineken Prize for Environmental Science, Norway’s Sophie Prize, Italy’s Medal of the Presidency, Japan’s Blue Planet Prize and even Adbuster’s person of the year.

Today, the imprint of his career can be found far and wide, including measures of the Genuine Progress Indicator of an economy, new Doughnut Economics framing of social floors within environmental ceilings, worldwide degree programs in ecological economics and a vibrant degrowth movement focused on a just transition to a right-sized economy.

I knew Herman Daly for two decades as a co-author, mentor and teacher. He always made time for me and my students, most recently writing the foreword to my upcoming book, “The Progress Illusion: Reclaiming Our Future from the Fairytale of Economics.” I will be forever grateful for his inspiration and courage to, as he put it, “ask the naive, honest questions” and then not be “satisfied until I get the answers.”

Jon D. Erickson, Professor of Sustainability Science and Policy, University of Vermont

This article is republished from The Conversation under a Creative Commons license. Read the original article.


I found this to be absolutely fascinating and I am sure many besides me agree.


Nothing to do with dogs but everything to do with the future!

An item in The Conversation recently was not only interesting from a scientific point-of-view but also it had real lessons for the way that we humans are interfering with the planet.

As The Conversation introduced the article:

A mile below the surface of the Greenland ice sheet, an ancient Arctic ecosystem is preserved in the frozen soil. How scientists discovered its leaves, twigs and mosses is a story in itself. It starts with a secret military base built into the northern Greenland ice.

Scientists Andrew Christ and Paul Bierman describe the discovery as something of a Rosetta stone for understanding how well the ice sheet stood up to global warming in the past – and how it might respond in the future.

So, for a change, read something that has nothing to do with our furry friends.


Ancient leaves preserved under a mile of Greenland’s ice – and lost in a freezer for years – hold lessons about climate change

Remnants of ancient Greenland tundra were preserved in soil beneath the ice sheet. Andrew Christ and Dorothy Peteet, CC BY-ND

Andrew Christ, University of Vermont and Paul Bierman, University of Vermont

In 1963, inside a covert U.S. military base in northern Greenland, a team of scientists began drilling down through the Greenland ice sheet. Piece by piece, they extracted an ice core 4 inches across and nearly a mile long. At the very end, they pulled up something else – 12 feet of frozen soil.

The ice told a story of Earth’s climate history. The frozen soil was examined, set aside and then forgotten.

Half a century later, scientists rediscovered that soil in a Danish freezer. It is now revealing its secrets.

Using lab techniques unimaginable in the 1960s when the core was drilled, we and an international team of fellow scientists were able to show that Greenland’s massive ice sheet had melted to the ground there within the past million years. Radiocarbon dating shows that it would have happened more than 50,000 years ago. It most likely happened during times when the climate was warm and sea level was high, possibly 400,000 years ago.

And there was more. As we explored the soil under a microscope, we were stunned to discover the remnants of a tundra ecosystem – twigs, leaves and moss. We were looking at northern Greenland as it existed the last time the region was ice-free. Our peer-reviewed study was published on March 15 in Proceedings of the National Academy of Sciences.

Two men with the ice core
Engineers pull up a section of the 4,560-foot-long ice core at Camp Century in the 1960s. U.S. Army Corps of Engineers

Paul Bierman, a geomorphologist and geochemist, describes what he and his colleagues found in the soil.

With no ice sheet, sunlight would have warmed the soil enough for tundra vegetation to cover the landscape. The oceans around the globe would have been more than 10 feet higher, and maybe even 20 feet. The land on which Boston, London and Shanghai sit today would have been under the ocean waves.

All of this happened before humans began warming the Earth’s climate. The atmosphere at that time contained far less carbon dioxide than it does today, and it wasn’t rising as quickly. The ice core and the soil below are something of a Rosetta Stone for understanding how durable the Greenland ice sheet has been during past warm periods – and how quickly it might melt again as the climate heats up.

Secret military bases and Danish freezers

The story of the ice core begins during the Cold War with a military mission dubbed Project Iceworm. Starting around 1959, the U.S. Army hauled hundreds of soldiers, heavy equipment and even a nuclear reactor across the ice sheet in northwest Greenland and dug a base of tunnels inside the ice. They called it Camp Century.

It was part of a secret plan to hide nuclear weapons from the Soviets. The public knew it as an Arctic research laboratory. Walter Cronkite even paid a visit and filed a report.

Workers cover a trench to build the under-ice military base
Workers build the snow tunnels at the Camp Century research base in 1960. U.S. Army Corps of Engineers

Camp Century didn’t last long. The snow and ice began slowly crushing the buildings inside the tunnels below, forcing the military to abandon it in 1966. During its short life, however, scientists were able to extract the ice core and begin analyzing Greenland’s climate history. As ice builds up year by year, it captures layers of volcanic ash and changes in precipitation over time, and it traps air bubbles that reveal the past composition of the atmosphere.

One of the original scientists, glaciologist Chester Langway, kept the core and soil samples frozen at the University at Buffalo for years, then he shipped them to a Danish archive in the 1990s, where the soil was soon forgotten.

A few years ago, our Danish colleagues found the soil samples in a box of glass cookie jars with faded labels: “Camp Century Sub-Ice.”

Scientists look at the sediment in jars
Geomorphologist Paul Bierman (right) and geochemist Joerg Schaefer of Columbia University examine the jars holding Camp Century sediment for the first time. They were in a Danish freezer set at -17 F. Paul Bierman, CC BY-ND

A surprise under the microscope

On a hot July day in 2019, two samples of soil arrived at our lab at the University of Vermont frozen solid. We began the painstaking process of splitting the precious few ounces of frozen mud and sand for different analyses.

First, we photographed the layering in the soil before it was lost forever. Then we chiseled off small bits to examine under the microscope. We melted the rest and saved the ancient water.

Then came the biggest surprise. While we were washing the soil, we spotted something floating in the rinse water. Paul grabbed a pipette and some filter paper, Drew grabbed tweezers and turned on the microscope. We were absolutely stunned as we looked down the eyepiece.

Staring back at us were leaves, twigs and mosses. This wasn’t just soil. This was an ancient ecosystem perfectly preserved in Greenland’s natural deep freeze.

One of the authors looking excited
Glacial geomorphologist Andrew Christ (right), with geology student Landon Williamson, holds up the first twig spotted as they washed a sediment sample from Camp Century. Paul Bierman, CC BY-ND

Dating million-year-old moss

How old were these plants?

Over the last million years, Earth’s climate was punctuated by relatively short warm periods, typically lasting about 10,000 years, called interglacials, when there was less ice at the poles and sea level was higher. The Greenland ice sheet survived through all of human history during the Holocene, the present interglacial period of the last 12,000 years, and most of the interglacials in the last million years.

But our research shows that at least one of these interglacial periods was warm enough for a long enough period of time to melt large portions of the Greenland ice sheet, allowing a tundra ecosystem to emerge in northwestern Greenland.

We used two techniques to determine the age of the soil and the plants. First, we used clean room chemistry and a particle accelerator to count atoms that form in rocks and sediment when exposed to natural radiation that bombards Earth. Then, a colleague used an ultra-sensitive method for measuring light emitted from grains of sand to determine the last time they were exposed to sunlight.

Maps of Greenland Ice Sheet speed and bedrock elevation
Maps of Greenland show the speed of the ice sheet as it flows (left) and the landscape hidden beneath it (right). BedMachine v3; Copernicus Climate Change Service (C3S), CC BY-ND

Chart of CO2 concentrations over time
The concentration of carbon dioxide in the atmosphere today is well beyond past levels determined from ice cores. On March 14, 2021, the CO2 level was about 417 ppm. NASA Jet Propulsion Laboratory, CC BY-ND

The million-year time frame is important. Previous work on another ice core, GISP2, extracted from central Greenland in the 1990s, showed that the ice had also been absent there within the last million years, perhaps about 400,000 years ago.

Lessons for a world facing rapid climate change

Losing the Greenland ice sheet would be catastrophic to humanity today. The melted ice would raise sea level by more than 20 feet. That would redraw coastlines worldwide.

About 40% of the global population lives within 60 miles of a coast, and 600 million people live within 30 feet of sea level. If warming continues, ice melt from Greenland and Antarctica will pour more water into the oceans. Communities will be forced to relocate, climate refugees will become more common, and costly infrastructure will be abandoned. Already, sea level rise has amplified flooding from coastal storms, causing hundreds of billions of dollars of damage every year.

A rock and tundra with a glacier in the background
Tundra near the Greenland ice sheet today. Is this what Camp Century looked like before the ice came back sometime in the last million years? Paul Bierman, CC BY-ND

The story of Camp Century spans two critical moments in modern history. An Arctic military base built in response to the existential threat of nuclear war inadvertently led us to discover another threat from ice cores – the threat of sea level rise from human-caused climate change. Now, its legacy is helping scientists understand how the Earth responds to a changing climate.

Andrew Christ, Postdoctoral Fellow and Lecturer in Geology, University of Vermont and Paul Bierman, Fellow of the Gund Institute for Environment, Professor of Geology and Natural Resources, University of Vermont

This article is republished from The Conversation under a Creative Commons license. Read the original article.


The article is republished with the full permission of The Conversation.

I hope you read it because the way the climate is changing is affecting all of us now and sooner rather than later we have all got to amend our ways. Indeed, when I look at anyone who has potentially thirty or more years of life in them I ponder what their future is going to be like. And, of course, it won’t be a drastic change in thirty years it is already happening now albeit at times difficult to see.

But there is not one scintilla of doubt that we humans are the cause and we humans have to be the solution!