气候变化领域集成服务门户(CCPortal): Increased shear in the North Atlantic upper-level jet stream over the past four decades

CCPortal

DOI	10.1038/s41586-019-1465-z
	Increased shear in the North Atlantic upper-level jet stream over the past four decades
	Lee, Simon H.; Williams, Paul D.; Frame, Thomas H. A.
发表日期	2019-08-29
ISSN	0028-0836
EISSN	1476-4687
卷号	572 期号:7771 页码:639-+
英文摘要	Earth's equator-to-pole temperature gradient drives westerly mid-latitude jet streams through thermal wind balance(1). In the upper atmosphere, anthropogenic climate change is strengthening this meridional temperature gradient by cooling the polar low
学科领域	Multidisciplinary Sciences
语种	英语
WOS记录号	WOS:000483405500050
来源期刊	NATURE
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/80571
作者单位	Univ Reading, Dept Meteorol, Reading, Berks, England
推荐引用方式 GB/T 7714	Lee, Simon H.,Williams, Paul D.,Frame, Thomas H. A.. Increased shear in the North Atlantic upper-level jet stream over the past four decades[J],2019,572(7771):639-+.
APA	Lee, Simon H.,Williams, Paul D.,&Frame, Thomas H. A..(2019).Increased shear in the North Atlantic upper-level jet stream over the past four decades.NATURE,572(7771),639-+.
MLA	Lee, Simon H.,et al."Increased shear in the North Atlantic upper-level jet stream over the past four decades".NATURE 572.7771(2019):639-+.