Scientists say that the Arctic serves as a fridge since its ocean ice cools whatever is left of the world, yet late proof demonstrates that this icebox is confronting some significant issues.
Environmental change foreswearing has become progressively well known. Be that as it may, most researchers concur that enduring ice, the more established ice that can make due in summer and direct atmosphere, have seen an emotional decrease in both thickness and degree in the previous three decades.
These estimations—which are gathered with the NASA Advanced Microwave Scanning Radiometer–Earth Observing System (AMSR-E) instrument on the NASA Aqua satellite and the Special Sensor Microwave/Imager (SSM/I) instrument on the Defense Meteorological Satellite Program, the National Snow and Ice Data Center (NSIDC) reports—uncover a warming Arctic.
Why do specialists concentrate more on the Arctic than they do on Antarctica? The Arctic has more ice that endures through summer when the sea retains 90 percent of daylight, which implies it has a critical part in influencing worldwide atmosphere.
Sea ice in the Arctic are at record lows.
While natural variations have contributed to changing air temperatures, Mark Serreze of the NSIDC says “. . . it’s very convincing that we’re starting to the see the effects of human activity on Arctic ice cover.”
This figure shows sea surface temperatures (SSTs) in October 2016.
Note that temperatures in the Beaufort and Chukchi Seas were unusually high, which limited ice growth in the Arctic region.
Climate Change Institute / University of Maine
Here’s a shot of the Beaufort Sea in the Northwest.
In addition to Beaufort and Chukchi, higher sea surface temperatures and slower ice growth were found in the Barents and Kara Seas.
This figure shows a decline of 7.4 percent in ice extent per decade since 1979.
Extent and area are two different measurements. The NSIDC says, “Extent would be a measure of the edges of the slice of cheese and all of the space inside it. Area would be the measure of where there is cheese only, not including the holes.” Extent will determine whether a region is “ice-covered” or “not ice-covered” based on a threshold.
National Snow and Ice Data Center
See this image for sea ice age in 1984.
The solid white indicates older, thicker ice. This is the kind of ice that can last through summer and help offset warming.
Here’s a look at sea ice age in 2016.
The bright white has thinned out dramatically. There are still layers of ice there, but they are much younger and thinner, meaning they are less likely to last when the ocean absorbs the sunlight.
Wildlife is the first to feel its effects.
Both terrestrial and marine animals are affected—sea ice is considered a biome in itself—and many are forced to change the way they feed and migrate.
Steven Kazlowski / Barcroft Media
Arctic amplification affects land ice, and here’s why it matters.
When land ice melts, freshwater is added to the oceans. This causes sea levels to rise. Researchers say that the Greenland ice sheet has lost 140 billion tons of ice per year over the past two decades.
M. Tedesco / Columbia University on Facebook
You can ignore apocalyptic warnings but there are other reasons we should worry, including disruptions in ocean circulation and more heat absorption. For more information, visit the NSIDC website.
Sources: NASA.gov Video, NASA Goddard