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Arctic Ocean |
Credit & Copyright: Dr. Bruce G.
Marcot
Explanation: Welcome to the northernmost town of the United States, Utqiagvik, Alaska. This town is at the edge of the North American continent, here along the Arctic Ocean, where the Chukchi Sea and the Beaufort Sea meet. Although it is mid-July in these photos, there still should be sea ice piled along the shoreline here. Except ... welcome, also, to warming at the edge. In years and decades past, dense sea ice would accumulate along the shoreline here, where the shallow depth allowed thick, multi-year ice to reach to the bottom and adhere to it as "fast ice." The dense ice would, in turn, protect the coastline and inhabitants from storm surges.
This is regional climate warming in action. But not just warming. For some time, it has been known that this high arctic region has been warming at twice the rate as warming further south in temperate zones ... except more recently, that rate has accelerated to four times the rate compared to the rest of the world (Rantanen et al. 2022). Such warming is called Arctic amplification, in play for the last 43 years at least.
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