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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Detecting intercepted snow on mountain needleleaf forest canopies using satellite remote sensing
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Detecting intercepted snow on mountain needleleaf forest canopies using satellite remote sensing

机译:使用卫星遥感检测在山上针心森林檐篷上的截止

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摘要

Snow interception in cold regions needleleaf forest canopies is a crucial process that controls local snow accumulation and redistribution over > 20% of the Earth's land surface. Various ground-based methods exist to measure intercepted snow load, however all are based on single-tree measurements and are difficult to implement. No research has focussed on detecting large areal intercepted snow loads and no studies have assessed the use of satellite observations. In this study, four remote sensing indices (NDSI, NDVI, albedo, and land surface temperature (LST)) were retrieved from Landsat images to study their sensitivity to canopy intercepted snow and the possibility of using them to detect the presence of intercepted snow. The results indicate that presence of intercepted snow on canopy increased NDSI and albedo, but decreased NDVI. Intercepted snow presence also decreased the areal variability of NDSI and NDVI while increasing that of albedo. For these three indices, the differences between snow-free and snowcovered canopies were correlated to topography and forest canopy cover. Of these indices, NDSI changed the greatest. Intercepted snow noticeably decreased the LST difference between forest and open areas in springtime while the influence in wintertime was relatively smaller. An intercepted snow detection approach that uses both NDSI and NDVI to classify pixels into either snowcovered canopy or other (snow-free canopy and non-forest areas) is proposed here. A case study applying this approach compared remote sensing detection to simulations by the snow interception and sublimation model implemented in the Cold Regions Hydrological Modelling platform (CRHM). This used local meteorological observations from the pine, spruce and fir forest covered Marmot Creek Research Basin in the Canadian Rockies. The remote sensing detection of intercepted snow agreed well with CRHM simulations for continuous forests (83%) and less well for sparse forests (72%) and clearings wi
机译:寒冷地区的雪拦截Contleaf Forest Canopies是一个关键的过程,控制当地积雪并再分配到地球陆地的20%。存在以测量截取的雪载的各种基于地基的方法,但是所有基于单树测量,难以实现。没有研究侧重于检测大量的截障雪载,没有研究评估使用卫星观察。在本研究中,从Landsat图像中检索了四个遥感指数(NDSI,NDVI,Albedo和陆表面温度(LST),以研究它们对冠层的敏感性截取的雪以及使用它们来检测截止雪的存在的可能性。结果表明,在冠层上存在截止的雪,增加了NDSI和Albedo,但下降了NDVI。截止的雪花儿也会降低NDSI和NDVI的由于Albedo的抗变异性。对于这三个指数,无雪和雪覆盖的檐篷之间的差异与地形和森林冠层覆盖相关。在这些指数中,NDSI更加伟大。截止的雪显着降低了森林与开放区域之间的LST差异,而冬季的影响相对较小。在此提出了一种截获的雪地检测方法,它使用NDSI和NDVI将像素分类为雪砖层或其他(无雪树冠和非林区)。应用这种方法的案例研究将遥感检测与冷区水文模拟平台(CRHM)中实施的雪截取和升华模型进行了次遥感检测。这侧使用了松树,云杉和冷杉森林的局部气象观测在加拿大落基罗基中覆盖了Marmot Cree Care Carchsoin盆地。截至截止雪的遥感检测与CRHM模拟相同,用于连续森林(83%),稀疏森林(72%)和清除Wi

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