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Updated: Jul 1, 2025

07:28
Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
6.5K
まとめ
融水が増え 北大西洋に"寒い泡"が形成され 地球全体の天気パターンが大きく変化しています この現象は 大気循環と降水に影響を与え 広範囲に及ぶ影響を及ぼします
科学分野:
- 海洋学
- 気候学
- 気象学
背景:
- 北大西洋流は,南大西洋逆流 (AMOC) の重要な構成要素で,弱くなっています.
- 特にグリーンランドでは 氷河や氷床から 溶ける水の流入が増加し 表面の新鮮化や冷却に寄与しています
- この冷却効果は"寒い塊"と呼ばれる 固有の地表水域を形成しています
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