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基于被动微波遥感的积雪深度和雪水当量反演研究进展 Title:ResearchProgressonPassiveMicrowaveRemoteSensingforSnowDepthandLiquidWaterContentRetrieval 1.Introduction SnowplaysacrucialroleintheEarth'sclimatesystem,affectingvariouscomponentsofthehydrologicalcycle,energybalance,andecosystemprocesses.Accuratemeasurementsofsnowdepthandliquidwatercontentarevitalforunderstandingtheseprocessesandmanagingwaterresourcesinsnow-dominatedregions.Passivemicrowaveremotesensinghasemergedasapowerfultoolformonitoringsnowcharacteristicsoverlargeareaswithhightemporalresolution.Thispaperreviewstherecentresearchprogressinthefieldofpassivemicrowaveremotesensingforsnowdepthandliquidwatercontentretrieval. 2.PrinciplesofPassiveMicrowaveRemoteSensingforSnowParameters Passivemicrowaveremotesensingutilizesthenaturalmicrowaveemissionsfromthesnowpacktoretrieveinformationaboutitsphysicalproperties.Themicrowaveradiationinteractswithsnowparticles,resultingincharacteristicmicrowavesignaturesthatcanberelatedtosnowdepthandliquidwatercontent.Snowdepthretrievalalgorithmsoftenexploittheinverserelationshipbetweenthemicrowaveemissionbrightnesstemperatureandsnowdepth.Liquidwatercontentretrievalalgorithmsanalyzethechangesintheemissionpropertiesatdifferentfrequenciesandpolarization. 3.SnowDepthRetrieval Variousalgorithmshavebeendevelopedforsnowdepthretrievalusingpassivemicrowaveremotesensing.Thesealgorithmsdifferintheirassumptionsregardingsnowpackproperties,suchassnowdensity,grainsize,andstratigraphy.Forinstance,thetemperature-gradientalgorithmutilizestheverticaltemperaturegradientobservedinthesnowpacktoestimatesnowdepth.TheSnowWaterEquivalentandSnowDepthRetrieval(SNODAS)modelcombinessatellitemeasurementswithgroundobservationstoprovideaccuratesnowdepthestimatesathighspatialresolutions.Otheralgorithmsemploymachinelearningtechniques,suchasartificialneuralnetworks,toimprovetheaccuracyofsnowdepthretrieval. 4.LiquidWaterContentRetrieval Liquidwatercontentinthesnowpackisanimportantparameterforevaluatingthesnowmeltprocesses,runoffgeneration,andav