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Warming maximum in the tropical upper troposphere deduced from thermal winds

✍ Scribed by Allen, Robert J.; Sherwood, Steven C.

Book ID
109920086
Publisher
Nature Publishing Group
Year
2008
Tongue
English
Weight
346 KB
Volume
1
Category
Article
ISSN
1752-0894

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## Abstract The zonal mean state of the atmosphere in the Northern Hemisphere in winter is determined by the temperature at the Earth's surface and by two potential vorticity (PV) anomalies (defined as that part of the PV field that induces a wind field) centred over the North Pole: one in the uppe