首页> 外文会议>Dragon 2 final results amp; Dragon 3 Kick-off symposium >DROUGHT MONITORING FOR THE MIDDLE REACHES OF YARLUNG ZANGBO RIVER AND ITS TWO TRIBUTARIES FROM SATELLITE IMAGES
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DROUGHT MONITORING FOR THE MIDDLE REACHES OF YARLUNG ZANGBO RIVER AND ITS TWO TRIBUTARIES FROM SATELLITE IMAGES

机译:卫星图像对雅鲁藏布江中游及其两个灾区的干旱监测

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摘要

The middle reaches of Yarlung Zangbo Riverrn(YR) and its two tributaries (Lhasa River andrnNianchu River) is a main agricultural region inrncentral Tibet Autonomous Region. Droughtrnmonitoring has significant meaning for localrncrop growth monitoring, crop yield assessmentrnand disaster monitoring. It also has greatrntheoretical importance for understanding localrnenergy and water balance status. In this paper,rnMODIS data on 14 April 2003, 16 October 2003rnunder nearly clear weather conditions arernselected as the spring and autumn cases. Thernland surface parameters, such as land surfacerntemperature (LST), albedo, NormalizedrnDifference Vegetation Index (NDVI), emissivityrnetc., have been derived from different algorithmsrnfor MODIS data. In combination withrnmeteorological data, the drought severity indexrn(DSI) is determined by applying Surface EnergyrnBalance System (SEBS). The estimations showrnthat spring drought is much more severe thanrnautumn drought. The river runoff is the dominantrnfactor for spring drought. The spatial variationsrnof drought conditions in the middle reaches ofrnYR and its two tributaries can also be clearlyrnidentified.
机译:雅鲁藏布江中游及其两个支流(拉萨河和年楚河)是西藏自治区的主要农业地区。干旱监测对当地作物生长监测,作物单产评估和灾害监测具有重要意义。它对于理解局部能源和水平衡状况也具有极大的理论重要性。本文选择2003年4月14日,2003年10月16日的MODIS数据作为春季和秋季的案例。陆地表面参数,如陆地表面温度(LST),反照率,归一化差异植被指数(NDVI),发射率等,是从MODIS数据的不同算法得出的。结合气象数据,通过应用地表能量平衡系统(SEBS)确定干旱严重程度指数(DSI)。估计结果表明,春季干旱比轮生干旱严重得多。河流径流是春季干旱的主要因素。还可以清楚地确定rnYR中游及其两个支流的干旱条件的空间变化。

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  • 会议地点 Beijing(CN)
  • 作者单位

    School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China,zhonglei@ustc.edu.cn,Faculty of Geo-information science and Earth observation (ITC), University of Twente, Enschede, The Netherlands,Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan PlateauResearch, Chinese Academy of Sciences, Beijing, China;

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan PlateauResearch, Chinese Academy of Sciences, Beijing, China;

    Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou;

    Faculty of Geo-information science and Earth observation (ITC), University of Twente, Enschede, The Netherlands;

    School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China;

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan PlateauResearch, Chinese Academy of Sciences, Beijing, China;

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan PlateauResearch, Chinese Academy of Sciences, Beijing, China;

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