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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Europe's 2003 heat wave: A satellite view of impacts and land-atmosphere feedbacks
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Europe's 2003 heat wave: A satellite view of impacts and land-atmosphere feedbacks

机译:2003年欧洲热浪:有关影响和陆地-大气反馈的卫星视图

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摘要

A combination of satellite imagery, meteorological station data, and the NCEP/NCAR reanalysis has been used to explore the spatial and temporal evolution of the 2003 heat wave in France, with focus on understanding the impacts and feedbacks at the land Surface. Vegetation was severely affected across the study area, especially ill a swath across central France that corresponds to the Western European Broadleaf (WEB) Forests ecological zone. The remotely sensed Surface temperature anomaly was also greatest in this zone, peaking at +15.4 degrees C in August. Oil a finer spatial scale, both the vegetation and surface temperature anomalies were greater for crops and pastures than for forested lands. The heat wave was also associated with all anomalous surface forcing of air temperature. Relative to other years ill record, satellite-derived estimates Of surface-sensible heat flux indicate all enhancement of 48-61% (24.0-30.5 W m(-2)) in WEB during the August heat wave maximum. Longwave radiative heating of the planetary boundary layer (PBL) was enhanced by 10.5 W m(-2) in WEB for the same period. The magnitude and spatial Structure of this local heating is consistent with models of the late twenty-first century climate in France, which predict a transitional climate zone that will become increasingly affected by Summertime drought. Models of future climate also Suggest that a soil-moisture feedback on the surface energy balance might exacerbate summertime drought, and these proposed feedback mechanisms were tested using satellite-derived heat budgets. Copyright (C) 2006 Royal Meteorological Society.
机译:结合卫星图像,气象台站数据和NCEP / NCAR再分析的方法,研究了2003年法国热浪的时空演变,重点是了解陆地表面的影响和反馈。整个研究区的植被受到严重影响,特别是在法国中部的一片沼泽中,这与西欧阔叶(WEB)森林生态区相对应。遥感的地表温度异常在该区域也最大,在八月达到+15.4摄氏度。如果空间尺度较小,则作物和牧场的植被和地表温度异常都比林地大。热波还与空气温度的所有异常表面强迫有关。相对于其他年份的病历记录,卫星得出的表面敏感热通量估计值表明,八月份热浪最大时,WEB的所有增强都达到48-61%(24.0-30.5 W m(-2))。同期,WEB中行星边界层(PBL)的长波辐射加热提高了10.5 W m(-2)。这种局部供暖的大小和空间结构与法国在二十一世纪末的气候模型相一致,该模型预测了过渡气候带将越来越受到夏季干旱的影响。未来气候模型还表明,土壤水分对表面能平衡的反馈可能会加剧夏季干旱,这些拟议的反馈机制已通过卫星衍生的热量预算进行了测试。版权所有(C)2006皇家气象学会。

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