Summer heat waves over Eastern China: dynamical processes and trend attribution
Recent trends in summer heat waves (HW) over Central-Eastern China and their atmospheric drivers are investigated using the ERA Interim re-analysis. A composite analysis shows that these events are preceded by an increase in 500 hPa geopotential height. Consequently, a subsidence anomaly develops ov...
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Veröffentlicht in: | Environmental research letters 2017-02, Vol.12 (2), p.24015 |
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description | Recent trends in summer heat waves (HW) over Central-Eastern China and their atmospheric drivers are investigated using the ERA Interim re-analysis. A composite analysis shows that these events are preceded by an increase in 500 hPa geopotential height. Consequently, a subsidence anomaly develops over the region and surface solar radiation increases. An increase in the northward moisture transport from the tropical region is also found to increase specific humidity, leading to warmer night-time temperatures. Feedback effects are also important: decrease of precipitation and enhanced evaporation also increases the specific humidity and North-Westerlies due to the low pressure lead to more heat convergence. HW occurrence increases, especially during the last decade, and is largely due to an increase in the mean temperature rather than to a change in dynamics, suggesting a human influence. |
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Res. Lett</addtitle><description>Recent trends in summer heat waves (HW) over Central-Eastern China and their atmospheric drivers are investigated using the ERA Interim re-analysis. A composite analysis shows that these events are preceded by an increase in 500 hPa geopotential height. Consequently, a subsidence anomaly develops over the region and surface solar radiation increases. An increase in the northward moisture transport from the tropical region is also found to increase specific humidity, leading to warmer night-time temperatures. Feedback effects are also important: decrease of precipitation and enhanced evaporation also increases the specific humidity and North-Westerlies due to the low pressure lead to more heat convergence. HW occurrence increases, especially during the last decade, and is largely due to an increase in the mean temperature rather than to a change in dynamics, suggesting a human influence.</description><subject>attribution</subject><subject>China</subject><subject>Evaporation</subject><subject>extreme weather events</subject><subject>Geopotential</subject><subject>Geopotential height</subject><subject>Heat</subject><subject>Heat waves</subject><subject>Human influences</subject><subject>Humidity</subject><subject>Low pressure</subject><subject>Solar radiation</subject><subject>Specific humidity</subject><subject>Summer</subject><subject>Tropical environment</subject><subject>Tropical environments</subject><issn>1748-9326</issn><issn>1748-9326</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>O3W</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>DOA</sourceid><recordid>eNp1kU1v2zAMho2hA9Zmu-9oYIdellaUJVvqbQj6BQTood1ZoCV6cZBYmaRkyL-fUhdpD-1FFIn3fSSSRfEd2AUwpS6hEWqqK15fIsoWq0_F6bF08ub-pTiLccmYFLJRp8XD43a9plAuCFP5D3cUS7_L-TXGRGEoZ4t-wKvS7Qdc9xZX5SZ4SzFmHQ6uTIHyiSmFvt2m3g9fi88driJ9e4mT4vfN9dPsbjp_uL2f_ZpPrQSRpmQ5tq2qm67WHHiVE9eBriutudJcAghqOiYAGyFq1rTKVryqrZZIDrJhUtyPXOdxaTahX2PYG4-9eS748MdgSL1dkbHUVFA53XHeCcoE5tpWKGTKEYKGzPoxsnJvf7cUk1n6bRjy9w2XQoPkULOsYqPKBh9joO74KjBzWIE5zNgcZmzGFWTL-Wjp_eaVSWFlgBtuGBcMpNm4Lit_vqP8EPwfyU-UPw</recordid><startdate>20170201</startdate><enddate>20170201</enddate><creator>Freychet, Nicolas</creator><creator>Tett, Simon</creator><creator>Wang, Jun</creator><creator>Hegerl, Gabriele</creator><general>IOP Publishing</general><scope>O3W</scope><scope>TSCCA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FE</scope><scope>8FG</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>L6V</scope><scope>M7S</scope><scope>PATMY</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>DOA</scope></search><sort><creationdate>20170201</creationdate><title>Summer heat waves over Eastern China: dynamical processes and trend attribution</title><author>Freychet, Nicolas ; 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subjects | attribution China Evaporation extreme weather events Geopotential Geopotential height Heat Heat waves Human influences Humidity Low pressure Solar radiation Specific humidity Summer Tropical environment Tropical environments |
title | Summer heat waves over Eastern China: dynamical processes and trend attribution |
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