Log in to save to my catalogue

What Controls the Mean East–West Sea Surface Temperature Gradient in the Equatorial Pacific: The Rol...

What Controls the Mean East–West Sea Surface Temperature Gradient in the Equatorial Pacific: The Rol...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1516742889

What Controls the Mean East–West Sea Surface Temperature Gradient in the Equatorial Pacific: The Role of Cloud Albedo

About this item

Full title

What Controls the Mean East–West Sea Surface Temperature Gradient in the Equatorial Pacific: The Role of Cloud Albedo

Author / Creator

Publisher

Boston, MA: American Meteorological Society

Journal title

Journal of climate, 2014-04, Vol.27 (7), p.2757-2778

Language

English

Formats

Publication information

Publisher

Boston, MA: American Meteorological Society

More information

Scope and Contents

Contents

The mean east–west sea surface temperature gradient along the equator is a key feature of tropical climate. Tightly coupled to the atmospheric Walker circulation and the oceanic east–west thermocline tilt, it effectively defines tropical climate conditions. In the Pacific, its presence permits the El Niño–Southern Oscillation phenomenon. What deter...

Alternative Titles

Full title

What Controls the Mean East–West Sea Surface Temperature Gradient in the Equatorial Pacific: The Role of Cloud Albedo

Authors, Artists and Contributors

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_miscellaneous_1516742889

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1516742889

Other Identifiers

ISSN

0894-8755

E-ISSN

1520-0442

DOI

10.1175/JCLI-D-13-00255.1

How to access this item