相关实验视频
Updated: Jul 1, 2025

07:28
Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
6.5K
概括
增加的融水正在北大西洋形成"冷泡", 显著改变全球天气模式. 这种现象会影响大气循环和降雨,
科学领域:
- 海洋学
- 气候学
- 天气学
背景情况:
- 北大西洋流是南大西洋逆流的重要组成部分,正在减弱.
- 冰川和冰盖,特别是格陵兰的融水流量增加,
- 这种冷却效应正在形成一个不同的区域,
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