Meltwater in Antarctica via Joseph Levy Two recent studies suggest that the climate warming occurring on Earth today is happening at a dramatically fast rate. It’s this rate of change, scientists say – the speed with which average global temperatures are expected to climb over the coming decades – that will make the ongoing climate warming troublesome for living things on Earth. Both groups of scientists used the phrase “10 times faster” to describe climate changes. One study, from Stanford University, suggests that climate change is happening 10 times faster than it has at any time in the past 65 million years. The other study, from the University of Texas, suggests that Antarctic permafrost is now melting 10 times faster than in 11,000 years, adding further evidence that Earth’s Antarctic is, in fact, warming just as Earth’s Arctic is. Click the links below to learn more about these studies. Climate warming 10 times faster than in 65 million years Antarctic permafrost melting 10 times faster than in 11 thousand years The top map shows global temperatures in the late 21st century, based on current warming trends. The bottom map illustrates the velocity of climate change, or how far species in any given area will need to migrate by the end of the 21st century to experience climate similar to present. Images via Stanford University. Climate warming 10 times faster than in 65 million years. In a study announced August 1, 2013, Stanford University climate scientists say that Earth is undergoing one of the largest climate changes in the past 65 million years. They say, moreover, that the change is currently on pace to occur at a rate 10 times faster than any change in 65 million years. Without intervention, these scientists say that this extreme pace could lead to a 5-6 degree Celsius spike in annual temperatures by the end of this century. Noah Diffenbaugh and Chris Field, both senior fellows at the Stanford Woods Institute for the Environment, published these results as part of a special report on climate change in the August 2013 issue of Science. They conducted a “targeted but broad” review of scientific literature on aspects of climate change that can affect ecosystems, and they investigated how recent observations and projections for climate change in the coming century compare to past events in Earth’s history. For instance, they compare the current warming to the 5-degree-Celsius temperature hike that occurred 20,000 years ago, as Earth emerged from the last ice age. They say that change was: … comparable to the high-end of the projections for warming over the 20th and 21st centuries. The difference is that, at the end of the last ice age, the warming took place over thousands of years. The same warming now is expected to occur over decades. Diffenbaugh and Field note that, as the climate warmed at the end of the last ice age, plants and animals moved northward to cooler climates. Similar (but possibly less successful?) migrations are expected in the coming years. Diffenbaugh and Field also say in their press release that: … some of the strongest evidence for how the global climate system responds to high levels of carbon dioxide comes from paleoclimate studies. Fifty-five million years ago, carbon dioxide in the atmosphere was elevated to a level comparable to today. The Arctic Ocean did not have ice in the summer, and nearby land was warm enough to support alligators and palm trees. But they say there are two key differences for ecosystems in the coming decades compared with the geologic past. The rapid pace of modern climate change is one. The other is that: … today there are multiple human stressors that were not present 55 million years ago, such as urbanization and air and water pollution.

Climate warming happening 10 times faster than in the past 65 million years. Antarctic permafrost melting 10 times faster than in 11,000 years,

The big tell here is that the ice is vanishing — it’s melting faster each time we measure. This is a dramatic shift from recent history.

As opposed to the potentially catastrophic bump in greenhouse gas emissions that could result if Arctic permafrost quickly melts, scientists here are presenting their findings as more of an interesting geologic curiosity. As the ground continues to thaw, researcher believe the landscape will sink and buckle, creating retrogressive thaw slumps.

Furthermore, unlike other ice melting in Antarctica which can contribute significantly to sea-level rise depending upon whether its already floating on the water or resting on solid ground, the ground ice melting here isn’t really a major component of the frozen water on the continent.