Arctic changes into a new climate state | Polarjournal
Polar bears are not the only ones facing big changes. The decrease of sea ice in summer and the time of formation of new sea ice significantly determine air temperatures above the Arctic Ocean in autumn and winter. The higher the air temperatures, the more precipitation falls as rain instead of snow. Photo: Julia Hager

The effects are visible and tangible almost everywhere in the rapidly warming Arctic: shrinking glaciers, ice shelves and ice caps, retreating sea ice, thawing permafrost, burning tundra, changes in species composition, to name only the most obvious. A new comprehensive study, published in the journal Nature Climate Change, on the status of the Arctic climate now shows that the Arctic is apparently in the process of changing from a predominantly frozen state to a completely different climate.

Weather patterns in the upper latitudes have always varied from year to year, with more or less sea ice, colder or warmer winters, and longer or shorter seasons of rain instead of snow. But the new research by scientists at the National Center for Atmospheric Research (NCAR) finds that the Arctic has now warmed so significantly that its year-to-year variability is moving outside the bounds of any past fluctuations, signaling the transition to a “new Arctic” climate regime.

“It’s a period of such rapid change that observations of past weather patterns no longer show what you can expect next year. The Arctic is already entering a completely different climate than just a few decades ago.”

Laura Landrum, National Center for Atmospheric Research

“The rate of change is remarkable,” said NCAR scientist Laura Landrum, the lead author of the study. “It’s a period of such rapid change that observations of past weather patterns no longer show what you can expect next year. The Arctic is already entering a completely different climate than just a few decades ago.”

In the new study, Landrum and her co-author, NCAR scientist Marika Holland, find that Arctic sea ice has melted so significantly in recent decades that even an unusually cold year will no longer have the amount of summer sea ice that existed as recently as the mid-20th century. Autumn and winter air temperatures will also warm enough to enter a statistically distinct climate by the middle of this century, followed by a seasonal change in precipitation that will result in additional months in which rain will fall instead of snow.

Fires in the arctic tundra are growing in size and can hardly be controlled. The release of huge amounts of carbon dioxide is further fueling climate change. Photo: Peter Griffith, NASA

For the study, Landrum and Holland used hundreds of detailed computer simulations as well as observations of Arctic climate conditions. The vast amount of data enabled them to statistically define the climate boundaries of the “old Arctic” – or how much variability can naturally occur from year to year – and then to identify when human-caused warming will push the Arctic beyond those natural bounds and into a new climate.

The future projections used for the study are based on a high-end scenario for future emissions of greenhouse gases, a trajectory known as RCP 8.5. The paper notes, however, that reduced emissions would lessen the extent of climate change in the Arctic.

The shifting climate has wide-ranging enormous consequences for ecosystems, water resource management, flood planning, and infrastructure.

Fundamental change
The far north is warming more rapidly than lower-latitude regions, which is due to a process known as Arctic amplification. This occurs because light-colored sea ice, which reflects heat back into space, is replaced by darker ocean water, which traps heat. In addition, relatively warm ocean waters are no longer shielded in the winter as effectively by the insulating properties of thick sea ice.

The changes in Arctic climate are so profound that the average extent of sea ice in September, when it reaches its annual minimum, has dropped by 31% since the first decade of the satellite era (1979-88).
Landrum and Holland wanted to determine if this decline shows that the Arctic climate has fundamentally changed. They also wanted to study changes to two other key aspects that are indicative of the frozen state of Arctic climate: air temperatures in the fall and winter, and the seasonal transition in precipitation from mostly snow to mostly rain.

Due to rapid warming, the Arctic is changing to a completely new climate. The expansion of sea ice in late summer at the time of the minimum has already changed to a statistically different climate (above). Clear changes are also visible in the air temperatures at the earth’s surface (center) and the number of days with rain instead of snow (bottom). Graphic: Simmi Sinha, © University Corporation for Atmospheric Research

To answer these questions, they turned to multiple simulations from five of the world’s leading climate models that have been used for an international research project known as the Coupled Model Intercomparison Project 5, or CMIP5. The large number of simulations enabled them to assemble a statistically significant picture of Arctic climate, allowing them to differentiate year-to-year natural climate variability from a transition to a new Arctic climate.

The scientists compared the model output to observations, confirming that the models were accurately capturing past climate and therefore could reliably simulate future climate.

Landrum and Holland then applied statistical techniques to determine when climatic changes exceeded the bounds of natural variability. For this last question, they identified a different climate as emerging when the 10-year average was at least two standard deviations away from the average of the climate in the decade 1950-59.

In other words, if the sea ice extent changed so much that the average in, say, the 1990s was lower in 97.7% of all cases than the sea ice extent for any year in the 1950s, then the 1990s were defined as a new climate.

When they applied these techniques to sea ice extent, they found that the Arctic has already entered a new climate. Each of the five models showed sea ice retreating so dramatically that a new climate for sea ice had emerged in the late 20th and early 21st centuries.

The rapidly rising air temperatures lead to a softening of the permafrost soil, so that, as here on the coast of Alaska, large pieces break off. The bigger problem, however, is the release of carbon dioxide and methane, which is associated with the thawing process. Photo: USGS

Looking forward, they also found that the Arctic may start to experience largely ice-free conditions in the next several decades. Several of the models indicated that the Arctic could become mostly ice free for 3-10 months annually by the end of the century, based on a scenario of high greenhouse gas emissions.

In terms of air temperatures, Landrum and Holland focused on autumn and winter, which are strongly influenced by the summertime reduction of sea ice and the subsequent timing of the ice regrowth. They found that the air temperatures over the ocean will enter a new climate during the first half or middle of this century, with air temperatures over land warming substantially later in the century.

The seasonal cycle of precipitation will change dramatically by the middle of the century. If emissions persist at a high level, most continental regions will experience an increase in the rainy season of 20-60 days by mid-century and 60-90 days by the end of the century. In some Arctic regions, rain may occur any month of the year by century’s end.

“The Arctic is likely to experience extremes in sea ice, temperature, and precipitation that are far outside anything that we’ve experienced before,” Landrum said. “We need to change our definition of what Arctic climate is.”

Source: National Center for Atmospheric Research

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