American Meteorological Society;Washington: American Meteorological Society
摘要:
摘要： Typhoon 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. 出版者： Washington: American Meteorological Society 出版日期： 2015-11-01 出處： Monthly weather review, 2015-11, Vol.143 (11), p.4493-4513 資源來源： EBSCOhost OmniFile Full Text Select 版權： Copyright American Meteorological Society Nov 2015 版權： Copyright American Meteorological Society 2015 識別號： ISSN: 0027-0644 識別號： EISSN: 1520-0493 識別號： DOI: 10.1175/MWR-D-15-0029.1 識別號： CODEN: MWREAB
