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首页> 外文期刊>Environmental Science and Pollution Research >Studying of drought phenomena and vegetation trends over South Asia from 1990 to 2015 by using AVHRR and NASA's MERRA data
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Studying of drought phenomena and vegetation trends over South Asia from 1990 to 2015 by using AVHRR and NASA's MERRA data

机译:从1990年到2015年使用AVHRR和NASA MERRA数据研究南亚干旱现象和植被趋势

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Drought is a severe climate fact that mainly results from low rainfall leading to serious threat of water shortages an ecological system of South Asia. Due to the current drought conditions and vegetation dynamics, the situation could further be intensified over South Asia. Thus, we study the drought impacts on vegetation dynamics over South Asia, aimed to find out the spatiotemporal differences in vegetation dynamics and seasons at which vegetation is determined by drought. Our approach is based on the using of advanced very high resolution radiometer (AVHRR) normalized difference vegetation index (NDVI) data and (NASA's MERRA) air temperature and rainfall data (1990-2015). Due to the low vegetation and dryness in South Asia, the NDVI is more helpful in describing the drought condition. From April to October, there were fast improvements in NDVI, VHI, and VCI. During September, the monthly VHI and VCI were stabilized and enhanced in October once more and in December again indicated a declining trend. The PCI, TCI, VCI, and VHI monthly values confirmed that in 2001, an extreme drought year, and continuous up to 2003, which lead the maximum drought in the South Asia regions. A considerably significantly correlation value in summer (JJA) and autumn (SON) seasons are showed between precipitation and NDVI. While the relationship between NVSWI and NDVI presented considerably high relationship in DJF, JJA, and SON, which specify an excellent indication for monitoring water stress. From 1990 to 2015, the difference of vegetation trend was obvious showed among various regions. The drought frequency was reducing trends from 1990 to 2015 over South Asia.
机译:干旱是一个严重的气候事实,主要是由于低降雨导致严重水资源威胁短缺的南亚生态系统。由于目前的干旱条件和植被动态,可以进一步加剧南亚的情况。因此,我们研究对南亚的植被动态的干旱影响,旨在发现植被动态和植被确定干旱植被的季节差异。我们的方法是基于先进的非常高分辨率辐射计(AVHRR)归一化差异植被指数(NASA)空气温度和降雨数据(1990-2015)的使用。由于南亚的植被和干燥较低,NDVI更有助于描述干旱状况。从4月到10月,NDVI,VHI和VCI的快速改善。在9月期间,每月vhi和vci在10月份稳定和加强,再次12月再次表明趋势下降。 PCI,TCI,VCI和VHI月度价值证实,2001年,一个极端的干旱年份,持续到2003年,这引发了南亚地区的最大干旱。夏季(JJA)和秋季(儿子)季节在降水和NDVI之间具有相当大的相关价值。虽然NVSWI和NDVI之间的关系在DJF,JJA和SOON中呈现了很高的关系,但是为监测水分应激的良好指示。从1990年到2015年,植被趋势的差异是明显的,各个地区都有明显。干旱频率降低了1990年至2015年南亚的趋势。

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