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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Recent trends of the tropical hydrological cycle inferred from Global Precipitation Climatology Project and International Satellite Cloud Climatology Project data
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Recent trends of the tropical hydrological cycle inferred from Global Precipitation Climatology Project and International Satellite Cloud Climatology Project data

机译:从全球降水气候学项目和国际卫星云气候学项目数据推断出的热带水文循环的最新趋势

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Sslcpaohrrgeeerse, oaimnf dmp atohcdut esth ltiehn egg l sositbmuadul ilheaysted hdrao tvlroeegn sidchs oc owyfcn lse ut;hc hahot iwimnecpvraeecrat, ssd,i inesgva gegnrre efeeomnr ehrneotgusi sooenn gs raeasgse ilosa nringale t shacesa laes the tropics, remain uncertain. The present investigation attempts to examine such trends in the observations using satellite data products comprising Global Precipitation Climatology radioajteicotn p. rSepceipciiftaictiaollny a, nedv oIlnvtienrgn atrtieonndasl oSfa tthelel ittreo Cpilcoauld h Cydlirmolaotgoilcoagly c Pycroleje ocvt ecrl othued laansdt 30 years were identified and analyzed. The results show (1) intensification of tropical precipitation in the rising regions of the Walker and Hadley circulations and weakening over the sinking regions of the associated overturning circulation; (2) poleward shift of the subtropical dry zones (up to 2° decade~(-1) in June-July-August (JJA) in the Octtoohrbeteh Hre-raNndo lHveyeem mcbiirsecpru hilnea rttieho ean n;S dao nu0dt.h 3(e-3r0n). 7sHi°ge dnmeiifcsipacadhneert-I e pi)no c lJoeunwnsaiesr-tdJe unmlty iwg-Aritahut igaounns ot( v0ae.n9rda-1l lS. 7be°rpo tdaeedmceabndeinerg-~(-1))of cloud boundaries of Hadley cell and plausible narrowing of the high cloudiness in the e Intertropical Convergence Zone region in some seasons. These results support findings of some of the previous studies that showed strengthening of the tropical hydrological cycle and expansion of the Hadley cell that are potentially related to the ent global warming trends.
机译:Sslcpaohrrgeeerse,oaimnf dmp atohcdut esth ltiehn egg l sositbmuadul ilheaysted hdrao tvlroeegn sidchs oc owyfcn lse ut; hc hahot iwimnecpvraeesses eaeasinge eeasinge eesgne geesefneesne本研究试图使用包括全球降水气候学radioajteicotn p。在内的卫星数据产品来检查观测中的此类趋势。鉴定并分析了30年以来的Cydlirmolaotgoilcoagly c Pycroleje occt ecrl cevt echeltitel Ctrcoeluld C.结果表明:(1)沃克和哈德利环流上升区的热带降水加剧,而相关的俯冲环流下沉区的热带降水减弱; (2)6月至7月至8月(JJA)的亚热带干旱区的极地偏移(直到6月至7月至8月(JJA)); s dao nu0dt.h 3( e-3r0n .. 7sHigege dnmeiifcsipacadhneert-I e pi)no c lJoeunwnsaiesr-tdJe unmlty iwg-Aritahut igaounns ot(v0ae.n9rda-1l lS。7be°rpo tdaeedmceabndeinerley-〜(-1)在某些季节,热带气旋辐合带地区的高云度似乎有所缩小。这些结果支持了以前的一些研究结果,这些研究表明热带水文循环的加强和Hadley细胞的扩张可能与全球变暖趋势有关。

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