More tropical cyclones in a cooler climate?

Recent review papers reported that many high‐resolution global climate models consistently projected a reduction of global tropical cyclone (TC) frequency in a future warmer climate, although the mechanism of the reduction is not yet fully understood. Here we present a result of 4K‐cooler climate ex...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Murakami, Hiroyuki [verfasserIn] Yoshida, Kohei Sugi, Masato

Format:	Artikel
Sprache:	Englisch

Erschienen:	2015

Rechteinformationen:	Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved.

Schlagwörter:	tropical cyclone cooler climate climate change Cyclones Global warming Ocean-atmosphere interaction Meteorology Ocean temperature Climate change

Übergeordnetes Werk:	Enthalten in: Geophysical research letters - Washington, DC : Union, 1974, 42(2015), 16, Seite 6780-6784
Übergeordnetes Werk:	volume:42 ; year:2015 ; number:16 ; pages:6780-6784

Links:	Volltext Link aufrufen Link aufrufen

DOI / URN:	10.1002/2015GL064929

Katalog-ID:	OLC1969325143

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allfields	10.1002/2015GL064929 doi PQ20160211 (DE-627)OLC1969325143 (DE-599)GBVOLC1969325143 (PRQ)p2124-9054eb66b70b31fc173e1880acf0853df67d448a622adba060a58e4ce257f49a0 (KEY)0026932820150000042001606780moretropicalcyclonesinacoolerclimate DE-627 ger DE-627 rakwb eng 550 DNB 38.70 bkl Murakami, Hiroyuki verfasserin aut More tropical cyclones in a cooler climate? 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Recent review papers reported that many high‐resolution global climate models consistently projected a reduction of global tropical cyclone (TC) frequency in a future warmer climate, although the mechanism of the reduction is not yet fully understood. Here we present a result of 4K‐cooler climate experiment. The global TC frequency significantly increases in the 4K‐cooler climate compared to the present climate. This is consistent with a significant decrease in TC frequency in the 4K‐warmer climate. For the mechanism of TC frequency reduction in a warmer climate, upward mass flux hypothesis and saturation deficit hypothesis have been proposed. The result of the 4K‐cooler climate experiment is consistent with these two hypotheses. One very interesting point is that the experiment has clearly shown that TC genesis is possible at sea surface temperature (SST) well below 26°C which has been considered as the lowest SST limit for TC genesis. The 4K‐cooler climate experiment is conducted using a high‐resolution AGCM Number of TCs is significantly increased in the 4K‐cooler climate Tropical cyclone genesis can occur at SST well below 26°C Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. tropical cyclone cooler climate climate change Cyclones Global warming Ocean-atmosphere interaction Meteorology Ocean temperature Climate change Yoshida, Kohei oth Sugi, Masato oth Enthalten in Geophysical research letters Washington, DC : Union, 1974 42(2015), 16, Seite 6780-6784 (DE-627)129095109 (DE-600)7403-2 (DE-576)01443122X 0094-8276 nnns volume:42 year:2015 number:16 pages:6780-6784 http://dx.doi.org/10.1002/2015GL064929 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015GL064929/abstract http://search.proquest.com/docview/1712403425 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_47 GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2279 38.70 AVZ AR 42 2015 16 6780-6784
spelling	10.1002/2015GL064929 doi PQ20160211 (DE-627)OLC1969325143 (DE-599)GBVOLC1969325143 (PRQ)p2124-9054eb66b70b31fc173e1880acf0853df67d448a622adba060a58e4ce257f49a0 (KEY)0026932820150000042001606780moretropicalcyclonesinacoolerclimate DE-627 ger DE-627 rakwb eng 550 DNB 38.70 bkl Murakami, Hiroyuki verfasserin aut More tropical cyclones in a cooler climate? 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Recent review papers reported that many high‐resolution global climate models consistently projected a reduction of global tropical cyclone (TC) frequency in a future warmer climate, although the mechanism of the reduction is not yet fully understood. Here we present a result of 4K‐cooler climate experiment. The global TC frequency significantly increases in the 4K‐cooler climate compared to the present climate. This is consistent with a significant decrease in TC frequency in the 4K‐warmer climate. For the mechanism of TC frequency reduction in a warmer climate, upward mass flux hypothesis and saturation deficit hypothesis have been proposed. The result of the 4K‐cooler climate experiment is consistent with these two hypotheses. One very interesting point is that the experiment has clearly shown that TC genesis is possible at sea surface temperature (SST) well below 26°C which has been considered as the lowest SST limit for TC genesis. The 4K‐cooler climate experiment is conducted using a high‐resolution AGCM Number of TCs is significantly increased in the 4K‐cooler climate Tropical cyclone genesis can occur at SST well below 26°C Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. tropical cyclone cooler climate climate change Cyclones Global warming Ocean-atmosphere interaction Meteorology Ocean temperature Climate change Yoshida, Kohei oth Sugi, Masato oth Enthalten in Geophysical research letters Washington, DC : Union, 1974 42(2015), 16, Seite 6780-6784 (DE-627)129095109 (DE-600)7403-2 (DE-576)01443122X 0094-8276 nnns volume:42 year:2015 number:16 pages:6780-6784 http://dx.doi.org/10.1002/2015GL064929 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015GL064929/abstract http://search.proquest.com/docview/1712403425 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_47 GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2279 38.70 AVZ AR 42 2015 16 6780-6784
allfields_unstemmed	10.1002/2015GL064929 doi PQ20160211 (DE-627)OLC1969325143 (DE-599)GBVOLC1969325143 (PRQ)p2124-9054eb66b70b31fc173e1880acf0853df67d448a622adba060a58e4ce257f49a0 (KEY)0026932820150000042001606780moretropicalcyclonesinacoolerclimate DE-627 ger DE-627 rakwb eng 550 DNB 38.70 bkl Murakami, Hiroyuki verfasserin aut More tropical cyclones in a cooler climate? 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Recent review papers reported that many high‐resolution global climate models consistently projected a reduction of global tropical cyclone (TC) frequency in a future warmer climate, although the mechanism of the reduction is not yet fully understood. Here we present a result of 4K‐cooler climate experiment. The global TC frequency significantly increases in the 4K‐cooler climate compared to the present climate. This is consistent with a significant decrease in TC frequency in the 4K‐warmer climate. For the mechanism of TC frequency reduction in a warmer climate, upward mass flux hypothesis and saturation deficit hypothesis have been proposed. The result of the 4K‐cooler climate experiment is consistent with these two hypotheses. One very interesting point is that the experiment has clearly shown that TC genesis is possible at sea surface temperature (SST) well below 26°C which has been considered as the lowest SST limit for TC genesis. The 4K‐cooler climate experiment is conducted using a high‐resolution AGCM Number of TCs is significantly increased in the 4K‐cooler climate Tropical cyclone genesis can occur at SST well below 26°C Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. tropical cyclone cooler climate climate change Cyclones Global warming Ocean-atmosphere interaction Meteorology Ocean temperature Climate change Yoshida, Kohei oth Sugi, Masato oth Enthalten in Geophysical research letters Washington, DC : Union, 1974 42(2015), 16, Seite 6780-6784 (DE-627)129095109 (DE-600)7403-2 (DE-576)01443122X 0094-8276 nnns volume:42 year:2015 number:16 pages:6780-6784 http://dx.doi.org/10.1002/2015GL064929 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015GL064929/abstract http://search.proquest.com/docview/1712403425 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_47 GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2279 38.70 AVZ AR 42 2015 16 6780-6784
allfieldsGer	10.1002/2015GL064929 doi PQ20160211 (DE-627)OLC1969325143 (DE-599)GBVOLC1969325143 (PRQ)p2124-9054eb66b70b31fc173e1880acf0853df67d448a622adba060a58e4ce257f49a0 (KEY)0026932820150000042001606780moretropicalcyclonesinacoolerclimate DE-627 ger DE-627 rakwb eng 550 DNB 38.70 bkl Murakami, Hiroyuki verfasserin aut More tropical cyclones in a cooler climate? 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Recent review papers reported that many high‐resolution global climate models consistently projected a reduction of global tropical cyclone (TC) frequency in a future warmer climate, although the mechanism of the reduction is not yet fully understood. Here we present a result of 4K‐cooler climate experiment. The global TC frequency significantly increases in the 4K‐cooler climate compared to the present climate. This is consistent with a significant decrease in TC frequency in the 4K‐warmer climate. For the mechanism of TC frequency reduction in a warmer climate, upward mass flux hypothesis and saturation deficit hypothesis have been proposed. The result of the 4K‐cooler climate experiment is consistent with these two hypotheses. One very interesting point is that the experiment has clearly shown that TC genesis is possible at sea surface temperature (SST) well below 26°C which has been considered as the lowest SST limit for TC genesis. The 4K‐cooler climate experiment is conducted using a high‐resolution AGCM Number of TCs is significantly increased in the 4K‐cooler climate Tropical cyclone genesis can occur at SST well below 26°C Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. tropical cyclone cooler climate climate change Cyclones Global warming Ocean-atmosphere interaction Meteorology Ocean temperature Climate change Yoshida, Kohei oth Sugi, Masato oth Enthalten in Geophysical research letters Washington, DC : Union, 1974 42(2015), 16, Seite 6780-6784 (DE-627)129095109 (DE-600)7403-2 (DE-576)01443122X 0094-8276 nnns volume:42 year:2015 number:16 pages:6780-6784 http://dx.doi.org/10.1002/2015GL064929 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015GL064929/abstract http://search.proquest.com/docview/1712403425 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_47 GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2279 38.70 AVZ AR 42 2015 16 6780-6784
allfieldsSound	10.1002/2015GL064929 doi PQ20160211 (DE-627)OLC1969325143 (DE-599)GBVOLC1969325143 (PRQ)p2124-9054eb66b70b31fc173e1880acf0853df67d448a622adba060a58e4ce257f49a0 (KEY)0026932820150000042001606780moretropicalcyclonesinacoolerclimate DE-627 ger DE-627 rakwb eng 550 DNB 38.70 bkl Murakami, Hiroyuki verfasserin aut More tropical cyclones in a cooler climate? 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Recent review papers reported that many high‐resolution global climate models consistently projected a reduction of global tropical cyclone (TC) frequency in a future warmer climate, although the mechanism of the reduction is not yet fully understood. Here we present a result of 4K‐cooler climate experiment. The global TC frequency significantly increases in the 4K‐cooler climate compared to the present climate. This is consistent with a significant decrease in TC frequency in the 4K‐warmer climate. For the mechanism of TC frequency reduction in a warmer climate, upward mass flux hypothesis and saturation deficit hypothesis have been proposed. The result of the 4K‐cooler climate experiment is consistent with these two hypotheses. One very interesting point is that the experiment has clearly shown that TC genesis is possible at sea surface temperature (SST) well below 26°C which has been considered as the lowest SST limit for TC genesis. The 4K‐cooler climate experiment is conducted using a high‐resolution AGCM Number of TCs is significantly increased in the 4K‐cooler climate Tropical cyclone genesis can occur at SST well below 26°C Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. tropical cyclone cooler climate climate change Cyclones Global warming Ocean-atmosphere interaction Meteorology Ocean temperature Climate change Yoshida, Kohei oth Sugi, Masato oth Enthalten in Geophysical research letters Washington, DC : Union, 1974 42(2015), 16, Seite 6780-6784 (DE-627)129095109 (DE-600)7403-2 (DE-576)01443122X 0094-8276 nnns volume:42 year:2015 number:16 pages:6780-6784 http://dx.doi.org/10.1002/2015GL064929 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015GL064929/abstract http://search.proquest.com/docview/1712403425 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_47 GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2279 38.70 AVZ AR 42 2015 16 6780-6784
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source	Enthalten in Geophysical research letters 42(2015), 16, Seite 6780-6784 volume:42 year:2015 number:16 pages:6780-6784
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author	Murakami, Hiroyuki
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topic_title	550 DNB 38.70 bkl More tropical cyclones in a cooler climate? tropical cyclone cooler climate climate change Cyclones Global warming Ocean-atmosphere interaction Meteorology Ocean temperature Climate change
topic	ddc 550 bkl 38.70 misc tropical cyclone misc cooler climate misc climate change misc Cyclones misc Global warming misc Ocean-atmosphere interaction misc Meteorology misc Ocean temperature misc Climate change
topic_unstemmed	ddc 550 bkl 38.70 misc tropical cyclone misc cooler climate misc climate change misc Cyclones misc Global warming misc Ocean-atmosphere interaction misc Meteorology misc Ocean temperature misc Climate change
topic_browse	ddc 550 bkl 38.70 misc tropical cyclone misc cooler climate misc climate change misc Cyclones misc Global warming misc Ocean-atmosphere interaction misc Meteorology misc Ocean temperature misc Climate change
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title	More tropical cyclones in a cooler climate?
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title_full	More tropical cyclones in a cooler climate?
author_sort	Murakami, Hiroyuki
journal	Geophysical research letters
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container_start_page	6780
author_browse	Murakami, Hiroyuki
container_volume	42
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author-letter	Murakami, Hiroyuki
doi_str_mv	10.1002/2015GL064929
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title_sort	more tropical cyclones in a cooler climate?
title_auth	More tropical cyclones in a cooler climate?
abstract	Recent review papers reported that many high‐resolution global climate models consistently projected a reduction of global tropical cyclone (TC) frequency in a future warmer climate, although the mechanism of the reduction is not yet fully understood. Here we present a result of 4K‐cooler climate experiment. The global TC frequency significantly increases in the 4K‐cooler climate compared to the present climate. This is consistent with a significant decrease in TC frequency in the 4K‐warmer climate. For the mechanism of TC frequency reduction in a warmer climate, upward mass flux hypothesis and saturation deficit hypothesis have been proposed. The result of the 4K‐cooler climate experiment is consistent with these two hypotheses. One very interesting point is that the experiment has clearly shown that TC genesis is possible at sea surface temperature (SST) well below 26°C which has been considered as the lowest SST limit for TC genesis. The 4K‐cooler climate experiment is conducted using a high‐resolution AGCM Number of TCs is significantly increased in the 4K‐cooler climate Tropical cyclone genesis can occur at SST well below 26°C
abstractGer	Recent review papers reported that many high‐resolution global climate models consistently projected a reduction of global tropical cyclone (TC) frequency in a future warmer climate, although the mechanism of the reduction is not yet fully understood. Here we present a result of 4K‐cooler climate experiment. The global TC frequency significantly increases in the 4K‐cooler climate compared to the present climate. This is consistent with a significant decrease in TC frequency in the 4K‐warmer climate. For the mechanism of TC frequency reduction in a warmer climate, upward mass flux hypothesis and saturation deficit hypothesis have been proposed. The result of the 4K‐cooler climate experiment is consistent with these two hypotheses. One very interesting point is that the experiment has clearly shown that TC genesis is possible at sea surface temperature (SST) well below 26°C which has been considered as the lowest SST limit for TC genesis. The 4K‐cooler climate experiment is conducted using a high‐resolution AGCM Number of TCs is significantly increased in the 4K‐cooler climate Tropical cyclone genesis can occur at SST well below 26°C
abstract_unstemmed	Recent review papers reported that many high‐resolution global climate models consistently projected a reduction of global tropical cyclone (TC) frequency in a future warmer climate, although the mechanism of the reduction is not yet fully understood. Here we present a result of 4K‐cooler climate experiment. The global TC frequency significantly increases in the 4K‐cooler climate compared to the present climate. This is consistent with a significant decrease in TC frequency in the 4K‐warmer climate. For the mechanism of TC frequency reduction in a warmer climate, upward mass flux hypothesis and saturation deficit hypothesis have been proposed. The result of the 4K‐cooler climate experiment is consistent with these two hypotheses. One very interesting point is that the experiment has clearly shown that TC genesis is possible at sea surface temperature (SST) well below 26°C which has been considered as the lowest SST limit for TC genesis. The 4K‐cooler climate experiment is conducted using a high‐resolution AGCM Number of TCs is significantly increased in the 4K‐cooler climate Tropical cyclone genesis can occur at SST well below 26°C
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container_issue	16
title_short	More tropical cyclones in a cooler climate?
url	http://dx.doi.org/10.1002/2015GL064929 http://onlinelibrary.wiley.com/doi/10.1002/2015GL064929/abstract http://search.proquest.com/docview/1712403425
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author2	Yoshida, Kohei Sugi, Masato
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up_date	2024-07-04T05:14:10.720Z
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