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Impact of climate change on disaster events in metropolitan cities -trend of disasters reported by Taiwan national medical response and preparedness system [期刊论文]
Environmental Research, 2020-01-01, 183
Lee C.-H.;  MD.;  Lin S.-H.;  MD.;  Kao C.-L.;  MD.;  Hong M.-Y.;  MD.;  Huang P.-C.;  Mr.;  Shih C.-L.;  MD./Director-General.;  Chuang C.-C.;  MD.
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Role of the meridional dipole of SSTA and associated cross-equatorial flow in the tropical eastern Pacific in terminating the 2014 El Niño development [期刊论文]
Climate Dynamics, 2018-01-01, 50 (2018-05-06
Wu Y.-K.;  Chen L.;  Hong C.-C.;  Li T.;  Chen C.-T.;  Wang L.
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Distinct influences of the ENSO-like and PMM-like SST anomalies on the mean TC genesis location in the Western North Pacific: The 2015 summer as an extreme example [期刊论文]
Journal of Climate, 2018-01-01, 31 (8
Hong C.-C.;  Lee M.-Y.;  Hsu H.-H.;  Tseng W.-L.
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Influence of climate regime shift on the interdecadal change in tropical cyclone activity over the Pacific Basin during the middle to late 1990s [期刊论文]
Climate Dynamics, 2016-01-01, 47 (2017-07-08
Hong C.-C.;  Wu Y.-K.;  Li T.
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Enhanced influences of tropical atlantic SST on WNP-NIO atmosphere-ocean coupling since the early 1980s [期刊论文]
Journal of Climate, 2016-01-01, 29 (18
Chang T.-C.;  Hsu H.-H.;  Hong C.-C.
View/Download:24/0
 
Compounding effects of warm sea surface temperature and reduced sea ice on the extreme circulation over the extratropical North Pacific and North America during the 2013-2014 boreal winter [期刊论文]
Geophysical Research Letters, 2015-01-01, 42 (5
Lee M.-Y.;  Hong C.-C.;  Hsu H.-H.
View/Download:19/0
 
Tropical SST forcing on the anomalous WNP subtropical high during July–August 2010 and the record-high SST in the tropical Atlantic [期刊论文]
Climate Dynamics, 2015-01-01, 45 (2017-03-04
Hong C.-C.;  Lee M.-Y.;  Hsu H.-H.;  Lin N.-H.;  Tsuang B.-J.
View/Download:16/0
 
The climate regime shift over the Pacific during 1996/1997 [期刊论文]
Climate Dynamics, 2014-01-01, 43 (2017-01-02
Hong C.-C.;  Wu Y.-K.;  Li T.;  Chang C.-C.
View/Download:14/0
 

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