Improving CLM4.5 Simulations of Land-Atmosphere Exchange during Freeze-Thaw Processes on the Tibetan Plateau

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摘要 Soilisheterogeneousandhasdifferentthermalandhydraulicproperties,causingvariedbehaviorinheatandmoisturetransport.Therefore,soilhasanimportanteffectonland–atmosphereinteractions.Inthisstudy,animprovedsoilparameterizationschemethatconsidersgravelandorganicmatterinthesoilwasintroducedintoCLM4.5(CommunityLandModel).ByusingdatafromtheZoigeandMadoisitesontheTibetanPlateau,theabilityofthemodeltosimultaneouslysimulatethedurationoffreeze–thawperiods,soiltemperature,soilmoisture,andsurfaceenergyduringfreeze–thawprocesses,wasvalidated.Theresultsindicatedthat:(1)thenewparameterizationperformedbetterinsimulatingthedurationofthefrozen,thawing,unfrozen,andfreezingperiods;(2)withthenewscheme,thesoilthermalconductivityvaluesweredecreased;(3)thenewparameterizationimprovedsoiltemperaturesimulationandeffectivelydecreasedcoldbiases;(4)thenewparameterizationschemeeffectivelydecreasedthedrybiasesofsoilliquidwatercontentduringthefreezing,completelyfrozen,andthawingperiods,butincreasedthewetbiasesduringthecompletelythawedperiod;and(5)thenetradiation,latentheatflux,andsoilsurfaceheatfluxoftheZoigeandMadoisitesweremuchimprovedbytheneworganicmatterandthermalconductivityparameterization.
机构地区 不详
出处 《气象学报:英文版》 2017年5期
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出版日期 2017年05月15日(中国期刊网平台首次上网日期,不代表论文的发表时间)
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