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Comment on "Changes in Tropical Cyclone Number, Duration, and Intensity in a Warming Environment"

Science24 Mar 2006Vol 311, Issue 5768p. 1713DOI: 10.1126/science.1121522

Abstract

Analyses of tropical cyclone records from the western North Pacific reveal that the recent increase in occurrence of intense typhoons reported by Webster et al. (Reports, 16 Sep. 2005, p. 1844) is not a trend. Rather, it is likely a part of the large interdecadal variations in the number of intense typhoons related to similar temporal fluctuations in the atmospheric environment.
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References and Notes

1
P. J. Webster, G. J. Holland, J. C. Curry, H.-R. Chang, Science309, 1844 (2005).
2
Tropical storms have maximum wind speeds between 63 and 118 km hour–1, and typhoons have maximum wind speeds greater than 118 km hour–1.
4
Aircraft reconnaissance of typhoons in the WNP was made by the Joint Typhoon Warning Center from 1959 to 1987 for selected TCs.
5
J. C. L. Chan, K. S. Liu, J. Clim.17, 4590 (2004).
6
S. J. Camargo, A. H. Sobel, J. Clim.18, 2996 (2005).
7
K. Emanuel, Nature436, 686 (2005).
8
A description of the Saffir-Simpson scale can be found at www.aoml.noaa.gov/general/lib/laescae.html.
9
The Joint Typhoon Warning Center (4) used a statistical technique called principal component analysis (PCA) to represent the two-dimensional fields of each of these three parameters. With the PCA, the major temporal variations (called principal components) of a field can be identified. For each time period, a value (coefficient) can be assigned corresponding to the amplitude of the principal component in that period. In this particular case, a positive coefficient gives an atmospheric flow with a stronger rotational flow (VORT), a weaker vertical shear (SHEAR), and more moist static energy (MSE), all of which are favorable conditions for typhoon formation and intensification (4). The data for these fields come from the “reanalyses” of the U.S. National Centers for Environmental Prediction.
10
K. E. Trenberth, Science308, 1753 (2005).
11
Suggestions from C. Landsea of the U.S. National Hurricane Center and J. Kepert of the Australian Bureau of Meteorology are much appreciated. This work was supported by City University of Hong Kong grant 9610021.

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Published In

Science
Volume 311 | Issue 5768
24 March 2006

Submission history

Received: 18 October 2005
Accepted: 14 February 2006
Published in print: 24 March 2006

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Authors

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Johnny C. L. Chan
Laboratory for Atmospheric Research, Department of Physics and Materials Science, City University of Hong Kong, Tat Chee Avenue, Kowloon, Hong Kong, China.

Notes

To whom correspondence should be addressed. E-mail: [email protected]

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