The Influence of the Ocean on Typhoon Nuri (2008)Source: Monthly Weather Review:;2015:;volume( 143 ):;issue: 011::page 4493DOI: 10.1175/MWR-D-15-0029.1Publisher: American Meteorological Society
Abstract: yphoon Nuri (2008) was 1 of approximately 120 typhoons in the past 60 years that passed through a narrow gap, the Luzon Strait, connecting the western North Pacific and the South China Sea (SCS). In total 70% of these storms, including Nuri, reached their maximum intensities over the warm waters east of Luzon and in the Kuroshio, then rapidly weakened in the SCS. Numerical experiments were conducted to understand the intensity change of Nuri. Westward across the Kuroshio in the Luzon Strait, the 26°C isotherm shallows rapidly by half. This and stronger mixing by wind?ocean resonance preferentially cooled sea surface temperature and weakened the typhoon in SCS. A positive-feedback mechanism is then described to explain the intensification of Nuri over the western North Pacific.
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contributor author | Sun, Jingru | |
contributor author | Oey, Lie-Yauw | |
date accessioned | 2017-06-09T17:32:58Z | |
date available | 2017-06-09T17:32:58Z | |
date copyright | 2015/11/01 | |
date issued | 2015 | |
identifier issn | 0027-0644 | |
identifier other | ams-87080.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4230709 | |
description abstract | yphoon Nuri (2008) was 1 of approximately 120 typhoons in the past 60 years that passed through a narrow gap, the Luzon Strait, connecting the western North Pacific and the South China Sea (SCS). In total 70% of these storms, including Nuri, reached their maximum intensities over the warm waters east of Luzon and in the Kuroshio, then rapidly weakened in the SCS. Numerical experiments were conducted to understand the intensity change of Nuri. Westward across the Kuroshio in the Luzon Strait, the 26°C isotherm shallows rapidly by half. This and stronger mixing by wind?ocean resonance preferentially cooled sea surface temperature and weakened the typhoon in SCS. A positive-feedback mechanism is then described to explain the intensification of Nuri over the western North Pacific. | |
publisher | American Meteorological Society | |
title | The Influence of the Ocean on Typhoon Nuri (2008) | |
type | Journal Paper | |
journal volume | 143 | |
journal issue | 11 | |
journal title | Monthly Weather Review | |
identifier doi | 10.1175/MWR-D-15-0029.1 | |
journal fristpage | 4493 | |
journal lastpage | 4513 | |
tree | Monthly Weather Review:;2015:;volume( 143 ):;issue: 011 | |
contenttype | Fulltext |