分裂

Jet Stream Pub Date : 2019-09-19 DOI:10.1093/oso/9780198828518.003.0012

T. Woollings

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引用次数: 0

摘要

在北大西洋上空，涡旋驱动的急流最终与副热带急流分离，形成分裂的急流结构。由于不受哈德利环流的稳定影响，北方急流的变化很大，它的移动和蜿蜒影响着北半球大部分地区的天气和气候模式。本章介绍了北大西洋涛动，这是急流变率的主要模式，概述了它的历史和影响。

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Split

Over the North Atlantic the eddy-driven jet stream finally separates from the subtropical jet, forming a split jet structure. Free from the steady influence of the Hadley cell, the northern jet is highly variable and its shifts and meanders affect weather and climate patterns around much of the hemisphere. This chapter introduces the North Atlantic Oscillation, the dominant pattern of jet variability, giving an overview of its history and impacts.

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Jet Stream

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