Graduate School of Global Environmental Studies, Kyoto University, Yoshida-Honmachi, Sakyo-ku, Kyoto 606-8501, Japan.
Environ Monit Assess. 2013 May;185(5):4117-24. doi: 10.1007/s10661-012-2854-z. Epub 2012 Sep 13.
Drought-induced anomalies in vegetation condition over wide areas can be observed by using time-series satellite remote sensing data. Previous methods to assess the anomalies may include limitations in considering (1) the seasonality in terms of each vegetation-cover type, (2) cumulative damage during the drought event, and (3) the application to various types of land cover. This study proposed an improved methodology to assess drought impact from the annual vegetation responses, and discussed the result in terms of diverse landscape mosaics in the Mt. Kenya region (0.4° N 35.8° E ~ 1.6° S 38.4° E). From the 30-year annual rainfall records at the six meteorological stations in the study area, we identified 2000 as the drought year and 2001, 2004, and 2007 as the normal precipitation years. The time-series profiles of vegetation condition in the drought and normal precipitation years were obtained from the values of Enhanced Vegetation Index (EVI; Huete et al. 2002), which were acquired from Terra MODIS remote sensing dataset (MOD13Q1) taken every 16 days at the scale of 250-m spatial resolution. The drought impact was determined by integrating the annual differences in EVI profiles between drought and normal conditions, per pixel based on nearly same day of year. As a result, we successfully described the distribution of landscape vulnerability to drought, considering the seasonality of each vegetation-cover type at every MODIS pixel. This result will contribute to the large-scale landscape management of Mt. Kenya region. Future study should improve this method by considering land-use change occurred during the long-term monitoring period.
可以利用时间序列卫星遥感数据观测到大面积植被状况因干旱而产生的异常。以前评估这些异常的方法可能存在一些局限性,例如:(1)考虑每种植被覆盖类型的季节性;(2)干旱事件期间的累积损害;(3)应用于各种类型的土地覆盖。本研究提出了一种改进的方法来评估干旱对年度植被响应的影响,并讨论了在肯尼亚山地区(0.4°N 35.8°E~1.6°S 38.4°E)不同景观镶嵌体中的结果。从研究区域六个气象站的 30 年年度降雨记录中,我们确定 2000 年为干旱年,2001 年、2004 年和 2007 年为正常降水年。从 Terra MODIS 遥感数据集(MOD13Q1)中获取的增强植被指数(EVI;Huete 等人,2002 年)的时间序列剖面,该数据集以 250 米空间分辨率每隔 16 天获取一次。干旱影响是通过整合干旱和正常条件下 EVI 剖面的年度差异来确定的,逐像素基于几乎相同的一年中的日期。结果,我们成功地描述了景观对干旱的脆弱性分布,考虑了每个 MODIS 像素中每种植被覆盖类型的季节性。这一结果将有助于肯尼亚山地区的大规模景观管理。未来的研究应该通过考虑长期监测期间发生的土地利用变化来改进该方法。