Response of the atmospheric circulation in non-tropical regions of the Northern Hemisphere to processes taking place in the tropical region

Response of the atmospheric circulation in non-tropical regions of the Northern Hemisphere to... The paper concentrates on the response of the atmospheric circulation non-tropical regions of the Northern Hemisphere to considerable sea surface temperature anomalies regularly occurring in the equatorial Pacific Ocean, related to the El Niño event. It has been established that during El Niño, zonal western circulation and meridional southern circulation tend to decay (being −2.6% and −5.4% respectively), while meridional northern circulation intensifies (+8.0%). The paper examines regional peculiarities of the non-tropical atmospheric response to the processes taking in the tropics. It is shown that atmospheric circulation reconstruction is most essential in the Siberian (10.4%) and Pacific (10.2%) sections and is minimal (4.3%) in the Atlantic region. These peculiarities of the regional atmospheric circulation reconstruction may be taken into account to predict short-term climatic variations in the Northern Hemisphere. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Physical Oceanography Springer Journals

Response of the atmospheric circulation in non-tropical regions of the Northern Hemisphere to processes taking place in the tropical region

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Publisher
Kluwer Academic Publishers
Copyright
Copyright © 1997 by VSP
Subject
Earth Sciences; Oceanography; Remote Sensing/Photogrammetry; Atmospheric Sciences; Climate Change; Environmental Physics
ISSN
0928-5105
eISSN
0928-5105
D.O.I.
10.1007/BF02523668
Publisher site
See Article on Publisher Site

Abstract

The paper concentrates on the response of the atmospheric circulation non-tropical regions of the Northern Hemisphere to considerable sea surface temperature anomalies regularly occurring in the equatorial Pacific Ocean, related to the El Niño event. It has been established that during El Niño, zonal western circulation and meridional southern circulation tend to decay (being −2.6% and −5.4% respectively), while meridional northern circulation intensifies (+8.0%). The paper examines regional peculiarities of the non-tropical atmospheric response to the processes taking in the tropics. It is shown that atmospheric circulation reconstruction is most essential in the Siberian (10.4%) and Pacific (10.2%) sections and is minimal (4.3%) in the Atlantic region. These peculiarities of the regional atmospheric circulation reconstruction may be taken into account to predict short-term climatic variations in the Northern Hemisphere.

Journal

Physical OceanographySpringer Journals

Published: Oct 22, 2006

References

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