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Long-term Change Analysis of Satellite-based Evapotranspiration over Indian Vegetated Surface

机译:印度植被表面基于卫星的蒸散量的长期变化分析

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In the present study, trend of satellite based annual evapotranspiration (ET) and natural forcing factors responsible for this were analyzed. Thirty years (1981-2010) of ET data at 0.08° grid resolution, generated over Indian region from optical-thermal observations from NOAA PAL and MODIS AQUA satellites, were used. Long-term data on gridded (0.5° × 0.5°) annual rainfall (RF), annual mean surface soil moisture (SSM) ERS scatterometer at 25 km resolution and annual mean incoming shortwave radiation from MERRA-2D reanalysis were also analyzed. Mann-Kendall tests were performed with time series data for trend analysis. Mean annual ET loss from Indian ago-ecosystem was found to be almost double (1100 Cubic Km) than Indian forest ecosystem (550 Cubic Km). Rainfed vegetation systems such as forest, rainfed cropland, grassland showed declining ET trend @ -4.8, -0.6 & -0.4 Cubic Kmyr~(-1), respectively during 30 years. Irrigated cropland initially showed ET decline upto 1995 @ -0.8 cubic Kmyr~(-1) which could possibly be due to solar dimming followed by increasing ET @ 0.9 cubic Kmyr~(-1) after 1995. A cross-over point was detected between forest ET decline and ET increase in irrigated cropland during 2008. During 2001-2010, the four agriculturally important Indian states eastern, central, western and southern showed significantly increasing ET trend with S-score of 15-25 and Z-score of 1.09-2.9. Increasing ET in western and southern states was found to be coupled with increase in annual rainfall and SSM. But in eastern and central states no significant trend in rainfall was observed though significant increase in ET was noticed. The study recommended to investigate the influence of anthropogenic factors such as increase in area under irrigation, increased use of water for irrigation through ground water pumping, change in cropping pattern and cultivars on increasing ET.
机译:在本研究中,分析了基于卫星的年度蒸散量(ET)的趋势以及造成这种情况的自然强迫因素。使用了30年(1981-2010年)的0.08°网格分辨率的ET数据,这些数据是根据NOAA PAL和MODIS AQUA卫星的光热观测结果在印度地区生成的。还分析了栅格化(0.5°×0.5°)年降雨量(RF),年平均地表土壤湿度(SSM)ERS散射仪(分辨率为25 km)和MERRA-2D再分析的年平均短波辐射的长期数据。使用时间序列数据进行了Mann-Kendall测试,以进行趋势分析。发现印度前生态系统的平均年ET损失几乎是印度森林生态系统(550立方公里)的两倍(1100立方公里)。在30年中,森林,雨养农田,草地等雨养植被系统的ET趋势分别为-4.8,-0.6和-0.4 Cubic Kmyr〜(-1)。灌溉农田最初显示ET下降到1995 @ -0.8立方Kmyr〜(-1),这可能是由于太阳变暗,然后是1995年之后ET在0.9立方Kmyr〜(-1)升高。 2008年灌溉农田的森林ET下降和ET增加。在2001-2010年期间,印度的四个农业重要州东部,中部,西部和南部的ET趋势显着增加,S值为15-25,Z值为1.09-。 2.9。西部和南部各州的ET增加与年降雨量和SSM的增加有关。但是,在东部和中部各州,尽管ET显着增加,但未观察到明显的降雨趋势。该研究建议调查人为因素的影响,例如灌溉面积的增加,通过地下水抽水增加灌溉用水,种植方式和品种的变化对ET增加的影响。

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