H
Hiroki Tokinaga
Researcher at Kyushu University
Publications - 42
Citations - 4146
Hiroki Tokinaga is an academic researcher from Kyushu University. The author has contributed to research in topics: Sea surface temperature & Global warming. The author has an hindex of 23, co-authored 40 publications receiving 3483 citations. Previous affiliations of Hiroki Tokinaga include Hokkaido University & University of Hawaii at Manoa.
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Indian Ocean Capacitor Effect on Indo–Western Pacific Climate during the Summer following El Niño
TL;DR: In this article, the authors investigated the cause of tropical Indian Ocean (TIO) sea surface temperature (SST) warming, increased tropical tropospheric temperature, an anomalous anticyclone over the subtropical northwest Pacific, and increased mei-yu-baiu rainfall over East Asia.
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Slowdown of the Walker circulation driven by tropical Indo-Pacific warming
TL;DR: It is found that SST warming patterns are the main cause of the weakened Walker circulation over the past six decades, and model experiments show that the observed slowdown in the Walker circulation is presumably driven by oceanic rather than atmospheric processes.
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Decadal Shift in El Niño Influences on Indo–Western Pacific and East Asian Climate in the 1970s*
TL;DR: In this article, the authors investigated the influence of the El Nino-Southern Oscillation (ENSO) on the subtropical northwest (NW) Pacific climate and showed that interdecadal change in this influence is due to changes in the tropical Indian Ocean response to ENSO.
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Bathymetric effect on the winter sea surface temperature and climate of the Yellow and East China Seas
TL;DR: In this article, the authors detect clear ocean-to-atmospheric feedback in the Yellow and East China (YEC) Seas that is triggered by the submerged ocean bottom topography.
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Atmospheric Response to the Gulf Stream: Seasonal Variations*
TL;DR: In this paper, the atmospheric response to the Gulf Stream front in sea surface temperature is investigated using high-resolution data from satellite observations and operational analysis and forecast, and two types of atmospheric response are observed with different seasonality and spatial distribution.