{"title":"The effect of dew on L- Band emissions from a vegetation canopy","authors":"Avinash Sharma, M. Kurum, R. Lang","doi":"10.23919/USNC-URSIRSM52661.2021.9552355","DOIUrl":null,"url":null,"abstract":"The effect of dew in a vegetation canopy on the L-Band thermal emissions is studied. An approximate electromagnetic model for dew on a leaf is used in conjunction with a Radiative Transfer to compute the thermal emissions. The dew is modeled as a thin uniform layer covering the entire surface of the leaf. From this model, the scattering amplitudes and phase functions are computed. These are then used in both the τ-ω model and a first-order Radiative Transfer model to compute the emissivity from the vegetation canopy in the presence of various amounts of dew. The τ-ω model predicts a decrease in emissivity as the dew amount increases. However, the inclusion of first-order scattering predicts the opposite relationship, where an increase in dew results in an increase in emissivity.","PeriodicalId":365284,"journal":{"name":"2021 USNC-URSI Radio Science Meeting (USCN-URSI RSM)","volume":"10 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2021-08-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"2021 USNC-URSI Radio Science Meeting (USCN-URSI RSM)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.23919/USNC-URSIRSM52661.2021.9552355","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
The effect of dew in a vegetation canopy on the L-Band thermal emissions is studied. An approximate electromagnetic model for dew on a leaf is used in conjunction with a Radiative Transfer to compute the thermal emissions. The dew is modeled as a thin uniform layer covering the entire surface of the leaf. From this model, the scattering amplitudes and phase functions are computed. These are then used in both the τ-ω model and a first-order Radiative Transfer model to compute the emissivity from the vegetation canopy in the presence of various amounts of dew. The τ-ω model predicts a decrease in emissivity as the dew amount increases. However, the inclusion of first-order scattering predicts the opposite relationship, where an increase in dew results in an increase in emissivity.