Arctic transitioning to a new climate state
Projections call for less ice, more rain, warmer air

Date:
September 14, 2020
Source:
National Center for Atmospheric Research/University Corporation
for Atmospheric Research
Summary:
The fast-warming Arctic has started to transition from a
predominantly frozen state into an entirely different climate with
significantly less sea ice, warmer temperatures, and more rain,
according to a comprehensive new study of Arctic conditions.



FULL STORY ==========================================================================
The fast-warming Arctic has started to transition from a predominantly
frozen state into an entirely different climate, according to a
comprehensive new study of Arctic conditions.


========================================================================== 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.

"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.

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.

The research was funded by the National Science Foundation, which is
NCAR's sponsor, and the National Oceanic and Atmospheric Administration.

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.

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.

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."

========================================================================== Story Source: Materials provided by National_Center_for_Atmospheric_Research/University Corporation_for_Atmospheric_Research. Original written by David
Hosansky. Note: Content may be edited for style and length.


========================================================================== Journal Reference:
1. Laura Landrum and Marika M. Holland. Extremes become routine in an
emerging New Arctic. Nature Climate Change, 2020 DOI:
10.1038/s41558-020- 0892-z ==========================================================================

Link to news story: https://www.sciencedaily.com/releases/2020/09/200914112232.htm

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