Intraseasonal relationships between tropical heating and extratropical jets

Intraseasonal variations of the northern midlatitude circulation and their relationships with the global tropical heating field are investigated using climate model fields. The greatest intraseasonal variance in the midlatitude flow is found in the vicinity of the time mean jets, and in the areas im...

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Main Author: Neith, Michael T.
Other Authors: Murphree, James Thomas, Naval Postgraduate School (U.S.), Meteorology, Chang, Chih-Pei
Format: Thesis
Language:English
Published: Monterey, California. Naval Postgraduate School 1992
Subjects:
Online Access:https://hdl.handle.net/10945/23931
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spelling ftnavalpschool:oai:calhoun.nps.edu:10945/23931 2024-06-09T07:48:14+00:00 Intraseasonal relationships between tropical heating and extratropical jets Neith, Michael T. Murphree, James Thomas Naval Postgraduate School (U.S.) Meteorology Chang, Chih-Pei 1992-12 98 p. application/pdf https://hdl.handle.net/10945/23931 en_US eng Monterey, California. Naval Postgraduate School https://hdl.handle.net/10945/23931 This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States. Teleconnections Intraseasonal oscillations Tropical heating Extratropical jets Thesis 1992 ftnavalpschool 2024-05-15T00:32:04Z Intraseasonal variations of the northern midlatitude circulation and their relationships with the global tropical heating field are investigated using climate model fields. The greatest intraseasonal variance in the midlatitude flow is found in the vicinity of the time mean jets, and in the areas immediately downstream of these jet exits. The model kinetic energy field associated with these jets shows a clear 30-60 day variation and eastward propagation within and between the different jet regions. This intraseasonal behavior is found to be well correlated with heating anomalies in specific parts of the global tropics. For each of the jet regions, we use a simple composite analysis to identify the global heating patterns associated with periods of strong and weak flow. For the North Pacific jet, strong flow occurs during and after periods of positive heating anomalies in the tropical western and central Pacific, and negative heating anomalies in the Indian Ocean. Conversely, the North Pacific flow is weak when these heating anomalies are reversed. The North Atlantic jet shows comparable relationships, with positive heating anomalies in the tropical western and eastern Pacific, and negative heating anomalies in the tropical Indian and Atlantic Oceans, before and during periods of strong flow. Approved for public release; distribution is unlimited. Lieutenant, United States Navy http://archive.org/details/intraseasonalrel1094523931 Thesis North Atlantic Naval Postgraduate School: Calhoun Indian Pacific
institution Open Polar
collection Naval Postgraduate School: Calhoun
op_collection_id ftnavalpschool
language English
topic Teleconnections
Intraseasonal oscillations
Tropical heating
Extratropical jets
spellingShingle Teleconnections
Intraseasonal oscillations
Tropical heating
Extratropical jets
Neith, Michael T.
Intraseasonal relationships between tropical heating and extratropical jets
topic_facet Teleconnections
Intraseasonal oscillations
Tropical heating
Extratropical jets
description Intraseasonal variations of the northern midlatitude circulation and their relationships with the global tropical heating field are investigated using climate model fields. The greatest intraseasonal variance in the midlatitude flow is found in the vicinity of the time mean jets, and in the areas immediately downstream of these jet exits. The model kinetic energy field associated with these jets shows a clear 30-60 day variation and eastward propagation within and between the different jet regions. This intraseasonal behavior is found to be well correlated with heating anomalies in specific parts of the global tropics. For each of the jet regions, we use a simple composite analysis to identify the global heating patterns associated with periods of strong and weak flow. For the North Pacific jet, strong flow occurs during and after periods of positive heating anomalies in the tropical western and central Pacific, and negative heating anomalies in the Indian Ocean. Conversely, the North Pacific flow is weak when these heating anomalies are reversed. The North Atlantic jet shows comparable relationships, with positive heating anomalies in the tropical western and eastern Pacific, and negative heating anomalies in the tropical Indian and Atlantic Oceans, before and during periods of strong flow. Approved for public release; distribution is unlimited. Lieutenant, United States Navy http://archive.org/details/intraseasonalrel1094523931
author2 Murphree, James Thomas
Naval Postgraduate School (U.S.)
Meteorology
Chang, Chih-Pei
format Thesis
author Neith, Michael T.
author_facet Neith, Michael T.
author_sort Neith, Michael T.
title Intraseasonal relationships between tropical heating and extratropical jets
title_short Intraseasonal relationships between tropical heating and extratropical jets
title_full Intraseasonal relationships between tropical heating and extratropical jets
title_fullStr Intraseasonal relationships between tropical heating and extratropical jets
title_full_unstemmed Intraseasonal relationships between tropical heating and extratropical jets
title_sort intraseasonal relationships between tropical heating and extratropical jets
publisher Monterey, California. Naval Postgraduate School
publishDate 1992
url https://hdl.handle.net/10945/23931
geographic Indian
Pacific
geographic_facet Indian
Pacific
genre North Atlantic
genre_facet North Atlantic
op_relation https://hdl.handle.net/10945/23931
op_rights This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.
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