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首页> 外文期刊>Agricultural Water Management >A baseline regional evapotranspiration (ET) and change hotspots over Indian sub-tropics using satellite remote sensing data
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A baseline regional evapotranspiration (ET) and change hotspots over Indian sub-tropics using satellite remote sensing data

机译:使用卫星遥感数据,基准区域蒸散(ET)和更改印度子热带的热点

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The annual water loss through evapotranspiration (ET) is an uncertain but significant component of India's water budget. The present study generated independent estimates of baseline annual ET, calibrated with in situ micrometeorological data over Indian sub-continent, using surface energy balance framework and satellite-based long-term thermal remote sensing, visible and near-infrared observations as the primary data sources. Thirty years' (1981-2010) of satellite-based ET estimates at 0.08 degrees grid resolution were used to assess trend in regional ET, to find out change hot-spots and probable causes. Long-term collateral data, influencing ET, such as gridded (0.5 degrees x 0.5 degrees) annual rainfall (RF), annual mean surface soil moisture (SSM) at 25 km resolution from ESA scatterometers and annual mean incoming shortwave radiation from MERRA-2D reanalysis were also analyzed. Mean annual ET loss was found to be the highest for Indian cropland (890 Cubic Km) than forest (575 Cubic Km). Annual water consumption pattern over vegetation systems showed declining ET trend at the rate of -16 Cubic Km yr(-1) upto 1995 during 30 years which might be due to declining rainfall and solar dimming. This was followed by increasing ET trend (34 Cubic Km yr(-1)). During 2001-2010, irrigated cropland showed a steep increase in water consumption pattern with an average rate of 4 Cubic Km yr(-1) while grassland and forest showed declining consumption patterns since 2003 and 2007, respectively thus showing crossover points of their consumption patterns with irrigated cropland. Four agriculturally important Indian eastern, central, western and southern states showed significantly increasing ET trend with S-score of 15-25 and Z-score of 1.09-2.9 during this period. 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. Region-specific correlation of annual ET with natural forcing variables was higher for incoming shortwave radiation as compared to rainfall. The increase in ET over irrigated croplands as well as over some of the Indian states could be due to increase in anthropogenic factors which need more detailed investigations in future.
机译:通过蒸散(ET)的年度水分损失是印度的水预算不确定但重要组成部分。本研究生成了基线年度ET的独立估计,以印度分型框架和卫星基于卫星的长期热遥感,可见和近红外测量为主数据来源,校准了基准年度ET的基准年度ET。 。三十年(1981-2010)的基于卫星的ET估算值为0.08度电网分辨率,用于评估区域ET的趋势,以找出变化热点和可能的原因。长期抵押数据,影响ET,如包装(0.5°×0.5度)的年降雨(RF),每年平均地表土壤水分(SSM),从ESA散射仪和每年平均入口Merra-2D的切入短波辐射还分析了重新分析。印度农田(890立方公里)的平均年度ET损失比森林(575立方公里)最高。植被系统的年度耗水模式显示在30年内的-16立方公里(-1)的速度下降至1995年,这可能是由于降雨量下降和太阳黯聚。随后是越来越大的趋势(34立方公里(-1))。在2001 - 2010年期间,灌溉农作物急剧增加水消耗模式,平均速率为4立方体(-1),而草原和森林以来,自2003年和2007年以来,分别表现出其消费模式的交叉点有灌溉的农田。四个农业上重要的印度东部,中央,西部和南方国家表现出在此期间为15-25和Z分数为1.09-2.9的S-Score显着增加。发现ET在西部和南部国家的增加加上年降雨量和SSM的增加。但在东部和中央州,虽然ET的显着增加,但没有显着降雨趋势。与降雨相比,在传入的短波辐射相比,收集的地区ET的特定于自然迫使变量的相关性更高。灌溉农田的增加以及一些印度国家可能是由于未来需要更详细的调查的人为因素增加。

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