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ANALYSIS OF DYNAMIC CHANGEOF HONG JIANNAO LAKE BASED ON SCALED SOIL MOISTURE MONITORING INDEX

机译:基于尺度土壤水分监测指标的洪建脑湖动态变化分析

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to climate change and human activities, Hong Jiannao Lake located in the arid and semi-arid area of China, it played a very important role in the regulation of the local climate, the balance of water resources and the maintenance of biological diversity. Hongjiannao Lake area in recent years continues to shrink, it was urgent to get the Hongjiannao Lake area change trend. This article take Hongjiannao Lake as study object using MODIS image of NIR and Red wavelength reflectivity data, selected April to October of 2000-2014,consturcted scale of SMMI (S-SMMI) based on soil moisture monitoring index (SMMI). The result indicated that lake area reduced from 46.9?kmsup2/sup in 2000 to 27.8?kmsup2/sup in 2014, average decay rate is 1.3?kmsup2/sup/a. The lake’s annual change showed a trend of periodic change. In general, the lake area began to increase slowly each year in April, and the area of the lake area reached the maximum, and then decreased gradually in June to July. Finally, we analysed the main driving factors included natural, man-made, and underground mining which lead to the lake area shrink.
机译:对于气候变化和人类活动,洪建na湖位于中国的干旱和半干旱地区,它在调节当地气候,水资源平衡和维持生物多样性方面发挥着非常重要的作用。近年来红碱na湖面积持续缩小,迫切需要得到红碱na湖面积的变化趋势。本文以红建na湖为研究对象,利用NIR的MODIS图像和红色波长反射率数据,选取2000- 2014年4月至10月,根据土壤水分监测指标(SMMI)构造SMMI(S-SMMI)规模。结果表明,湖泊面积从2000年的46.9?km 2 减少到2014年的27.8?km 2 ,平均衰减率为1.3?km 2 /一个。湖泊的年度变化显示出周期性变化的趋势。总的来说,湖泊面积每年4月开始缓慢增加,湖泊面积达到最大,然后在6月至7月逐渐减少。最后,我们分析了导致湖泊面积缩小的主要驱动因素,包括自然,人为和地下采矿。

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