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英国皇家气象学会(RMetS)是天气和气候领域领先的学协会,致力于加强科学研究,提高人们对天气和气候重要性的认识,支持气象专业人员,激励气象爱好者。

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Aninvestigationintotheverticalstructuresoflow-altitudeatmosphereovertheCentralTaklimakanDesertinsummer

Authors:JinfangYin,HaodongGu,JieHuang,MinzhongWang

Journal:AtmosphericScienceLetters

Published:24June

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Inthisstudy,1-monthcontinuousradiosondeobservationaldatawereappliedtopresentthelow-altitudeverticalstructuresandtheirevolutionsovertheCentralTaklimakanDesert(CTD).Theprimaryfocusistohighlighttheverticalstructuresnearthegroundwiththehigh-resolution(10minheightand6hrintime)radiosondedata.Oneoftheuniquefeaturesevidentinourresultsisanobviousdiurnaltransitioninlowerlayersnearthegroundduetostrongsurfaceheatingorcooling.Unlikeatraditionalverticalstructureintheboundarylayerobservedoveranondesertsurface,bothsuperadiabaticandinversionlayersaredistinctduringtheday.Morespecifically,thesuperadiabaticlayerisobviousinthedaytimebecauseofstrongsolarradiationoverthedesert,andthesuperadiabaticcanreachupto0.2km.Incontrast,anapparentinversionlayerformsinthenighttimeduetothesurfacecooling.Itisfoundthatthesurfaceforcingmainlydominatesthestructuresintheboundarylayer.Atlast,theverticalstructuresfromtheobservationsare

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