Radiative cooling effect of Hurricane Florence in 2006 and precipitation of Typhoon Matsa in 2005

Abstract The increasing strength of tropical cyclones may be a response of the Earth's interaction between natural variability and human activities. Negative effects of the severe storms, such as flooding, landslides, damage to properties, and even a number of human casualties, have been report...

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Published in:Atmospheric Science Letters
Main Authors: Liu, Quanhua, Weng, Fuzhong
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2009
Subjects:
Online Access:http://dx.doi.org/10.1002/asl.219
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spelling crwiley:10.1002/asl.219 2024-06-02T08:14:20+00:00 Radiative cooling effect of Hurricane Florence in 2006 and precipitation of Typhoon Matsa in 2005 Liu, Quanhua Weng, Fuzhong 2009 http://dx.doi.org/10.1002/asl.219 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fasl.219 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl.219 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Atmospheric Science Letters volume 10, issue 2, page 122-126 ISSN 1530-261X 1530-261X journal-article 2009 crwiley https://doi.org/10.1002/asl.219 2024-05-03T10:44:30Z Abstract The increasing strength of tropical cyclones may be a response of the Earth's interaction between natural variability and human activities. Negative effects of the severe storms, such as flooding, landslides, damage to properties, and even a number of human casualties, have been reported many times. This study reported other aspects on Hurricanes and Typhoons, which may be beneficial to the world. We found that Hurricane Florence in 2006 decreased radiation energy by − 0.5 × 10 20 J to the Earth‐atmospheric system, about 10% of the annual global energy consumption. If the amount of energy uniformly distributes over the whole Earth surface and over 1‐year time, it corresponds to a power of − 0.003 W m −2 The total forcing power on climate change is 0.24 W m −2 , if we only take account for the stored fluxes in water, atmosphere, continents, and heat required to melt glaciers and sea ice. Thus, the shielding effect of solar radiation by tropical storms could contribute to ease global warming. In addition, hurricane and typhoon can ease drought sometimes. This study found that the total rainwater carried by Typhoon Matsa in August 2005 into China's inland amounts to about 135 billion tons. The rainfall over the northern China eased severe drought in summer 2005. Copyright © 2009 Royal Meteorological Society Article in Journal/Newspaper Sea ice Wiley Online Library Atmospheric Science Letters 10 2 122 126
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The increasing strength of tropical cyclones may be a response of the Earth's interaction between natural variability and human activities. Negative effects of the severe storms, such as flooding, landslides, damage to properties, and even a number of human casualties, have been reported many times. This study reported other aspects on Hurricanes and Typhoons, which may be beneficial to the world. We found that Hurricane Florence in 2006 decreased radiation energy by − 0.5 × 10 20 J to the Earth‐atmospheric system, about 10% of the annual global energy consumption. If the amount of energy uniformly distributes over the whole Earth surface and over 1‐year time, it corresponds to a power of − 0.003 W m −2 The total forcing power on climate change is 0.24 W m −2 , if we only take account for the stored fluxes in water, atmosphere, continents, and heat required to melt glaciers and sea ice. Thus, the shielding effect of solar radiation by tropical storms could contribute to ease global warming. In addition, hurricane and typhoon can ease drought sometimes. This study found that the total rainwater carried by Typhoon Matsa in August 2005 into China's inland amounts to about 135 billion tons. The rainfall over the northern China eased severe drought in summer 2005. Copyright © 2009 Royal Meteorological Society
format Article in Journal/Newspaper
author Liu, Quanhua
Weng, Fuzhong
spellingShingle Liu, Quanhua
Weng, Fuzhong
Radiative cooling effect of Hurricane Florence in 2006 and precipitation of Typhoon Matsa in 2005
author_facet Liu, Quanhua
Weng, Fuzhong
author_sort Liu, Quanhua
title Radiative cooling effect of Hurricane Florence in 2006 and precipitation of Typhoon Matsa in 2005
title_short Radiative cooling effect of Hurricane Florence in 2006 and precipitation of Typhoon Matsa in 2005
title_full Radiative cooling effect of Hurricane Florence in 2006 and precipitation of Typhoon Matsa in 2005
title_fullStr Radiative cooling effect of Hurricane Florence in 2006 and precipitation of Typhoon Matsa in 2005
title_full_unstemmed Radiative cooling effect of Hurricane Florence in 2006 and precipitation of Typhoon Matsa in 2005
title_sort radiative cooling effect of hurricane florence in 2006 and precipitation of typhoon matsa in 2005
publisher Wiley
publishDate 2009
url http://dx.doi.org/10.1002/asl.219
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fasl.219
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl.219
genre Sea ice
genre_facet Sea ice
op_source Atmospheric Science Letters
volume 10, issue 2, page 122-126
ISSN 1530-261X 1530-261X
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/asl.219
container_title Atmospheric Science Letters
container_volume 10
container_issue 2
container_start_page 122
op_container_end_page 126
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