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Landsat Identification of Tornado Damage by Land Cover and an Evaluation of Damage Recovery in Forests

机译:土地覆盖龙卷风损伤的土地识别及森林损伤恢复评价

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Multispectral satellite imagery provides a spaceborne perspective on tornado damage identification; however, few studies have explored how tornadoes alter the spectral signature of different land-cover types. In part 1 of this study, Landsat surface reflectance is used to explore how 17 tornadoes modify the spectral signature, NDVI, and "Tassled Cap'' parameters inside forest (N = 16), grassland (N = 10), and urban (N 5 17) land cover. Land cover influences the magnitude of change observed, particularly in spring/summer imagery, with most tornado-damaged surfaces exhibiting a higher median reflectance in the visible and shortwave infrared, and a lower median reflectance in the near-infrared spectral ranges. These changes result in a higher median Tasseled Cap brightness, lower Tasseled Cap greenness and wetness, and lower NDVI relative to unaffected areas. Other factors affecting the magnitude of change in reflectance include season, vegetation condition, land-cover heterogeneity, and tornado strength. While vegetation indices like NDVI provide a quick way to identify damage, they have limited utility when monitoring recovery because of the cyclical seasonal vegetation cycle. Since tornado damage provides an analogous spectral signal to that of forest clearing, NDVI is compared with a forest disturbance index (DI) across a 5-yr Landsat climatology surrounding the 27 April 2011 tornado outbreak in part 2 of this study. Preoutbreak DI values remain relatively stable across seasons. In the five tornado-damaged areas evaluated, DI values peak within 6 months followed by a decline coincident with ongoing recovery. DI-like metrics provide a seasonally independent mechanism to fill the gap in identifying damage and monitoring recovery.
机译:多光谱卫星图像在龙卷风损伤识别方面提供了星载的透视;然而,很少有研究探索了龙卷风如何改变不同陆地覆盖类型的光谱特征。在本研究的第1部分中,Landsat表面反射率用于探索17次龙卷风修改森林内(n = 16),草原(n = 10)和城市(n = 10)和城市(n 5 17)陆地覆盖。陆地覆盖影响所观察到的变化的程度,特别是在春季/夏季图像中,大多数龙卷风损坏的表面,在可见和短波红外线上表现出更高的中位数反射,以及近红外线中的较低的中位反射率光谱范围。这些变化导致更高的中值流苏帽亮度,降低流苏帽绿色和湿度,以及相对于未受影响的区域的较低的NDVI。影响反射率变化的大小的其他因素包括季节,植被状况,陆地覆盖异质性,以及龙卷风强度。虽然NDVI等植被指数提供了一种快速识别损坏的方式,但由于周期性季节性植被周期监测恢复时,它们具有有限的效用。自龙卷风以来损坏为森林清算提供了类似的光谱信号,将NDVI与跨越5年4月27日的森林障碍指数(DI)进行比较,周围2011年4月27日Tornado爆发在本研究第2部分。在季节的季节仍然相对稳定前爆发。在五个龙卷风损坏的区域,在6个月内达到6个月内的DI值达到峰值,随后与正在进行的恢复一致的衰退。 Di-libic指标提供了季节性独立的机制,以填补识别损坏和监测恢复的差距。

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