Interactions of large-scale tropical motion systems during the 1996-1997 Australian monsoon

During the northern winter monsoon, several large-scale tropical motion systems are active in the southern tropical region of the ITCZ and SPCZ, including the maritime continent, northern Australia and the West Pacific. Superimposed on the mean state are transient large-scale systems including the M...

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Main Author: Taylor, Sylvia C.
Other Authors: Chang, Chih-Pei
Language:en_US
Published: Monterey, California. Naval Postgraduate School 2012
Online Access:http://hdl.handle.net/10945/8549
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spelling ndltd-nps.edu-oai-calhoun.nps.edu-10945-85492014-11-27T16:07:44Z Interactions of large-scale tropical motion systems during the 1996-1997 Australian monsoon Taylor, Sylvia C. Chang, Chih-Pei During the northern winter monsoon, several large-scale tropical motion systems are active in the southern tropical region of the ITCZ and SPCZ, including the maritime continent, northern Australia and the West Pacific. Superimposed on the mean state are transient large-scale systems including the Madden-Julian Oscillation (MJO) propagating from the equatorial Indian Ocean, the northeasterly cold surges from the northern hemisphere, and the easterly waves from the central or western Pacific. This work studied the possible interactions among these large-scale systems and their roles in the development of tropical cyclones. GMS water vapor data and NCEP reanalysis data during December 1996 to March 1997 were used. Examination of daily maps revealed that most of the TC development requires the interaction of two or more large-scale transient systems. The most frequent occurrences involved the interaction of the MJO and cold surges, followed by the interaction of the MJO and easterly waves 2012-08-09T19:21:29Z 2012-08-09T19:21:29Z 1998-09-01 Thesis http://hdl.handle.net/10945/8549 a207933 en_US Monterey, California. Naval Postgraduate School
collection NDLTD
language en_US
sources NDLTD
description During the northern winter monsoon, several large-scale tropical motion systems are active in the southern tropical region of the ITCZ and SPCZ, including the maritime continent, northern Australia and the West Pacific. Superimposed on the mean state are transient large-scale systems including the Madden-Julian Oscillation (MJO) propagating from the equatorial Indian Ocean, the northeasterly cold surges from the northern hemisphere, and the easterly waves from the central or western Pacific. This work studied the possible interactions among these large-scale systems and their roles in the development of tropical cyclones. GMS water vapor data and NCEP reanalysis data during December 1996 to March 1997 were used. Examination of daily maps revealed that most of the TC development requires the interaction of two or more large-scale transient systems. The most frequent occurrences involved the interaction of the MJO and cold surges, followed by the interaction of the MJO and easterly waves
author2 Chang, Chih-Pei
author_facet Chang, Chih-Pei
Taylor, Sylvia C.
author Taylor, Sylvia C.
spellingShingle Taylor, Sylvia C.
Interactions of large-scale tropical motion systems during the 1996-1997 Australian monsoon
author_sort Taylor, Sylvia C.
title Interactions of large-scale tropical motion systems during the 1996-1997 Australian monsoon
title_short Interactions of large-scale tropical motion systems during the 1996-1997 Australian monsoon
title_full Interactions of large-scale tropical motion systems during the 1996-1997 Australian monsoon
title_fullStr Interactions of large-scale tropical motion systems during the 1996-1997 Australian monsoon
title_full_unstemmed Interactions of large-scale tropical motion systems during the 1996-1997 Australian monsoon
title_sort interactions of large-scale tropical motion systems during the 1996-1997 australian monsoon
publisher Monterey, California. Naval Postgraduate School
publishDate 2012
url http://hdl.handle.net/10945/8549
work_keys_str_mv AT taylorsylviac interactionsoflargescaletropicalmotionsystemsduringthe19961997australianmonsoon
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