Thermal Remote Sensing in Land Surface Processing 2004
DOI: 10.1201/9780203502174-c3
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Land surface temperature retrieval techniques and applications

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Cited by 51 publications
(46 citation statements)
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“…지표면온도의 큰 시·공간적 변동성 을 고려할 때 정지궤도 기상위성으로부터 현업 차원 에서의 지표면온도의 산출이 가능해짐에 따라 지표면 온도의 활용에 새로운 전기가 다가오고 있다 (Prata and Cechet 1999;Sun and Pinker, 2003;Han et al, 2004;Sobrino and Romaguera 2004;Inamdar and French 2009;Pinker et al, 2009;Suh 2013b, Gottsche et al, 2016). 정확한 이해 및 고려가 필요하다 (Wan and Dozier, 1996;Goita et al, 1997;Kerr et al, 2004;Dash, 2005 (Gallo et al, 1996;Dai et al, 1999;Suh et al, 2009). 2) 연구방법 Cho et al(2015)가 개선한 기존의 알고리즘(CSW_v2.0)은 다양한 대기 조건에 대하여 휘도온도차, 지표면 방출율, Frey et al, 2012, Cho andSuh, 2013b;Li et al, 2013).…”
Section: 서 론unclassified
“…지표면온도의 큰 시·공간적 변동성 을 고려할 때 정지궤도 기상위성으로부터 현업 차원 에서의 지표면온도의 산출이 가능해짐에 따라 지표면 온도의 활용에 새로운 전기가 다가오고 있다 (Prata and Cechet 1999;Sun and Pinker, 2003;Han et al, 2004;Sobrino and Romaguera 2004;Inamdar and French 2009;Pinker et al, 2009;Suh 2013b, Gottsche et al, 2016). 정확한 이해 및 고려가 필요하다 (Wan and Dozier, 1996;Goita et al, 1997;Kerr et al, 2004;Dash, 2005 (Gallo et al, 1996;Dai et al, 1999;Suh et al, 2009). 2) 연구방법 Cho et al(2015)가 개선한 기존의 알고리즘(CSW_v2.0)은 다양한 대기 조건에 대하여 휘도온도차, 지표면 방출율, Frey et al, 2012, Cho andSuh, 2013b;Li et al, 2013).…”
Section: 서 론unclassified
“…This Split Window method is mainly used for sea surface temperature (SST), but in LST retrieval it has more conflicts (Kerr, et al, 2005). The main reason that causes less accuracy in estimating LST is the variability of land surface emissivity.…”
Section: Avhrr Algorithmmentioning
confidence: 99%
“…The first one is based on a relationship between emissivity and shortwave bands (0.5~1.1 µm). This method is almost empirical and the coefficients are surface dependent (Kerr, et al, 2005). The second method calculates emissivity by solving the radiometric equation at the surface in the thermal infrared.…”
Section: Avhrr Algorithmmentioning
confidence: 99%
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“…Methods to retrieve the LST that compensate for the emissivity effects can be classified into the following three categories: Single-channel methods, two-channel or split-window methods, and two-angle methods [44][45][46]. The single-channel methods rely on accurate atmospheric profiles [47], which are unavailable for our study site and image acquisition dates.…”
Section: Land Surface Temperature and Land Surface Emissivity Retrievalmentioning
confidence: 99%