Increased shear in the North Atlantic upper-level jet stream over the past four decades

Nature
Simon H LeeThomas H A Frame

Abstract

Earth's equator-to-pole temperature gradient drives westerly mid-latitude jet streams through thermal wind balance1. In the upper atmosphere, anthropogenic climate change is strengthening this meridional temperature gradient by cooling the polar lower stratosphere2,3 and warming the tropical upper troposphere4-6, acting to strengthen the upper-level jet stream7. In contrast, in the lower atmosphere, Arctic amplification of global warming is weakening the meridional temperature gradient8-10, acting to weaken the upper-level jet stream. Therefore, trends in the speed of the upper-level jet stream11-13 represent a closely balanced tug-of-war between two competing effects at different altitudes14. It is possible to isolate one of the competing effects by analysing the vertical shear-the change in wind speed with height-instead of the wind speed, but this approach has not previously been taken. Here we show that, although the zonal wind speed in the North Atlantic polar jet stream at 250 hectopascals has not changed since the start of the observational satellite era in 1979, the vertical shear has increased by 15 per cent (with a range of 11-17 per cent) according to three different reanalysis datasets15-17. We further show that thi...Continue Reading

Citations

Nov 13, 2020·Nature·Lin Li, Pinaki Chakraborty

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