On tropical cyclone frequency and the warm pool area

The proposition that the rate of tropical cyclogenesis increases with the size of the "warm pool" is tested by comparing the seasonal variation of the warm pool area with the seasonality of the number of tropical cyclones. An analysis based on empirical data from the Northern Hemisphere is...

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Main Author: R. E. Benestad
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2009
Subjects:
Online Access:https://doaj.org/article/6ba5c53296794e1d9f370d722d9dbe34
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author R. E. Benestad
author_facet R. E. Benestad
author_sort R. E. Benestad
collection Directory of Open Access Journals: DOAJ Articles
description The proposition that the rate of tropical cyclogenesis increases with the size of the "warm pool" is tested by comparing the seasonal variation of the warm pool area with the seasonality of the number of tropical cyclones. An analysis based on empirical data from the Northern Hemisphere is presented, where the warm pool associated with tropical cyclone activity is defined as the area, A , enclosed by the 26.5°C SST isotherm. Similar analysis was applied to the temperature weighted area A T with similar results. An intriguing non-linear relationship of high statistical significance was found between the temperature weighted area in the North Atlantic and the North-West Pacific on the one hand and the number of cyclones, N , in the same ocean basin on the other, but this pattern was not found over the North Indian Ocean. A simple statistical model was developed, based on the historical relationship between N and A . The simple model was then validated against independent inter-annual variations in the seasonal cyclone counts in the North Atlantic, but the correlation was not statistically significant in the North-West Pacific. No correlation, however, was found between N and A in the North Indian Ocean. A non-linear relationship between the cyclone number and temperature weighted area may in some ocean basins explain both why there has not been any linear trend in the number of cyclones over time as well as the recent upturn in the number of Atlantic hurricanes. The results also suggest that the notion of the number of tropical cyclones being insensitive to the area A is a misconception.
format Article in Journal/Newspaper
genre North Atlantic
genre_facet North Atlantic
geographic Indian
Pacific
geographic_facet Indian
Pacific
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op_relation http://www.nat-hazards-earth-syst-sci.net/9/635/2009/nhess-9-635-2009.pdf
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https://doaj.org/toc/1684-9981
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https://doaj.org/article/6ba5c53296794e1d9f370d722d9dbe34
op_source Natural Hazards and Earth System Sciences, Vol 9, Iss 2, Pp 635-645 (2009)
publishDate 2009
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spelling ftdoajarticles:oai:doaj.org/article:6ba5c53296794e1d9f370d722d9dbe34 2025-01-16T23:37:48+00:00 On tropical cyclone frequency and the warm pool area R. E. Benestad 2009-04-01T00:00:00Z https://doaj.org/article/6ba5c53296794e1d9f370d722d9dbe34 EN eng Copernicus Publications http://www.nat-hazards-earth-syst-sci.net/9/635/2009/nhess-9-635-2009.pdf https://doaj.org/toc/1561-8633 https://doaj.org/toc/1684-9981 1561-8633 1684-9981 https://doaj.org/article/6ba5c53296794e1d9f370d722d9dbe34 Natural Hazards and Earth System Sciences, Vol 9, Iss 2, Pp 635-645 (2009) Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 Geology QE1-996.5 article 2009 ftdoajarticles 2023-01-08T01:34:44Z The proposition that the rate of tropical cyclogenesis increases with the size of the "warm pool" is tested by comparing the seasonal variation of the warm pool area with the seasonality of the number of tropical cyclones. An analysis based on empirical data from the Northern Hemisphere is presented, where the warm pool associated with tropical cyclone activity is defined as the area, A , enclosed by the 26.5°C SST isotherm. Similar analysis was applied to the temperature weighted area A T with similar results. An intriguing non-linear relationship of high statistical significance was found between the temperature weighted area in the North Atlantic and the North-West Pacific on the one hand and the number of cyclones, N , in the same ocean basin on the other, but this pattern was not found over the North Indian Ocean. A simple statistical model was developed, based on the historical relationship between N and A . The simple model was then validated against independent inter-annual variations in the seasonal cyclone counts in the North Atlantic, but the correlation was not statistically significant in the North-West Pacific. No correlation, however, was found between N and A in the North Indian Ocean. A non-linear relationship between the cyclone number and temperature weighted area may in some ocean basins explain both why there has not been any linear trend in the number of cyclones over time as well as the recent upturn in the number of Atlantic hurricanes. The results also suggest that the notion of the number of tropical cyclones being insensitive to the area A is a misconception. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Indian Pacific
spellingShingle Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
Geology
QE1-996.5
R. E. Benestad
On tropical cyclone frequency and the warm pool area
title On tropical cyclone frequency and the warm pool area
title_full On tropical cyclone frequency and the warm pool area
title_fullStr On tropical cyclone frequency and the warm pool area
title_full_unstemmed On tropical cyclone frequency and the warm pool area
title_short On tropical cyclone frequency and the warm pool area
title_sort on tropical cyclone frequency and the warm pool area
topic Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
Geology
QE1-996.5
topic_facet Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
Geology
QE1-996.5
url https://doaj.org/article/6ba5c53296794e1d9f370d722d9dbe34