The Arctic hasn’t been this warm for 3 million years
The Pliocene Arctic
We are part of a team of scientists who analyzed sediment cores fromLake El’gygytgynin northeast Russia in 2013 to understand the Arctic’s climate under higher atmospheric carbon dioxide levels. Fossil pollen preserved in these cores shows that the Pliocene Arctic was very different from its current state.
Today the Arctic is a treeless plain with only sparsetundra vegetation, such as grasses, sedges and a few flowering plants. In contrast, the Russian sediment cores containedpollen from trees such as larch, spruce, fir and hemlock. This shows thatboreal forests, which today end hundreds of miles farther south and west in Russia and at the Arctic Circle in Alaska, once reached all the way to the Arctic Ocean across much of Arctic Russia and North America.
Because the Arctic was much warmer in the Pliocene, the Greenland Ice Sheet did not exist. Small glaciers along Greenland’s mountainous eastern coast were among the few places with year-round ice in the Arctic. The Pliocene Earth had ice only at one end – in Antarctica – and that ice wasless extensive and more susceptible to melting.
Because the oceans were warmer and there were no large ice sheets in the Northern Hemisphere, sea levels were 30 to 50 feet (9 to 15 meters) higher around the globe than they are today. Coastlines were far inland from their current locations. The areas that are now California’s Central Valley, the Florida Peninsula and the Gulf Coast all were underwater. So was the land where major coastal cities like New York, Miami, Los Angeles, Houston and Seattle stand.
Warmer winters across what is now the western U.S. reduced snowpack, which these dayssupplies much of the region’s water. Today’s Midwest and Great Plains were so much warmer and dryer that it would have been impossible to grow corn or wheat there.
Why was there so much CO2 in the Pliocene?
How did CO2 concentrations during the Pliocene reach levels similar to today’s? Humans would not appear on Earth for at least another million years, and our use of fossil fuels is even more recent. The answer is that some natural processes that have occurred on Earth throughout its history release CO2 to the atmosphere, while others consume it. The main system that keeps these dynamics in balance and controls Earth’s climate is a natural global thermostat, regulated by rocks thatchemically react with CO2and pull it out of the atmosphere.
In soils, certain rocks continually break down into new materials in reactions that consume CO2. These reactions tend to speed up when temperatures and rainfall are higher – exactly the climate conditions that occur when atmospheric greenhouse gas concentrations rise.
But this thermostat has a built-in control. When CO2 and temperatures increase and rock weathering accelerates, it pulls more CO2 from the atmosphere. If CO2 begins to fall, temperatures cool and rock weathering slows globally, pulling out less CO2.
Rock weathering reactions also can work faster where soil contains lots of newly exposed mineral surfaces. Examples include areas with high erosion or periods when Earth’s tectonic processes pushed land upward, creating major mountain chains with steep slopes.
The rock weathering thermostat operates at a geologically slow pace. For example, at the end of the Age of Dinosaurs about 65 million years ago, scientists estimate that atmospheric CO2 levels were between 2,000 and 4,000 parts per million. It took over 50 million years to reduce them naturally to around 400 parts per million in the Pliocene.
Because natural changes in CO2 levels happened very slowly, cyclic shifts in Earth’s climate system were also very slow. Ecosystems had millions of years to adapt, adjust and slowly respond to changing climates.
A Pliocene-like future?
Today human activities are overwhelming the natural processes that pull CO2 out of the atmosphere. At the dawn of the Industrial Era in 1750, atmospheric CO2 stood at about280 parts per million. It has taken humans only 200 years to completely reverse the trajectory begun 50 million years ago and return the planet to CO2 levels not experienced for millions of years.
Most of that shift has happened since World War II. Yearly increases of 2-3 parts per million now are common. And in response, the Earth is warming at a fast pace. Since roughly 1880 the planet has warmed by1 degree Celsius (2 degrees Fahrenheit)– many times faster than any warming episode in the past 65 million years of Earth’s history.
In the Arctic, losses of reflective snow and ice cover have amplified this warming to +5 C (9 F). As a result, summertime Arctic sea ice coverage is trending lower and lower. Scientists project that the Arctic will becompletely ice-free in summerwithin the next two decades.
This isn’t the only evidence of drastic Arctic warming. Scientists have recordedextreme summer melt ratesacross the Greenland Ice Sheet. In early August, Canada’s last remaining ice shelf, in the territory of Nunavut,collapsed into the sea. Parts ofArctic SiberiaandSvalbard, a group of Norwegian islands in the Arctic Ocean, reached record-shattering high temperatures this summer.
Coastal cities, agricultural breadbasket regions and water supplies for many communities all will be radically different if this planet returns to a Pliocene CO2 world. This future is not inevitable – but avoiding it will require big steps now to decrease fossil fuel use and turn down Earth’s thermostat.
This article is republished fromThe ConversationbyJulie Brigham-Grette, Professor of Geosciences,University of Massachusetts AmherstandSteve Petsch, Associate Professor of Geosciences,University of Massachusetts Amherstunder a Creative Commons license. Read theoriginal article.
Story byThe Conversation
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