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首页> 外文期刊>Agricultural and Forest Meteorology >Latent heat flux estimation in clear sky days over Indian agroecosystems using noontime satellite remote sensing data
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Latent heat flux estimation in clear sky days over Indian agroecosystems using noontime satellite remote sensing data

机译:利用午时卫星遥感数据估算印度农业生态系统晴空天的潜热通量

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摘要

A simplified evaporative fraction ( Lambda ) based single-source energy balance scheme was tested with moderate resolution ( arrow right km) noontime satellite observations to evaluate clear sky latent heat flux ( lambda E) estimates over diverse agricultural landscapes. This approach uses two-dimensional (2D) scatter between land surface temperature (LST) and albedo to determine Lambda . The operational utility of this scheme was demonstrated for estimating regional evapotranspiration and consumptive water use during rabi (November to April) crop growing season to predict pre-harvest wheat yield (error within 15.9% of reported mean) using time series data. The existence of triangular relations between Lambda and LAI (leaf area index) or NDVI (normalized difference vegetation index) was found with basal line (hypotenuse) linearly coupled with LAI or NDVI at low level of surface soil wetness. The analysis of diurnal course of in situ Lambda proved the validity of constant- Lambda hypothesis over pure, uniform, homogeneous crop canopies but showed irregular and wave-like patterns over heterogeneous, mixed crop canopies. The root mean square error (RMSE) of noontime and daytime average lambda E estimates with respect to in situ lambda E measurements were also smaller over homogeneous agricultural canopies (41 and 23Wm super(-) super(2)) with correlation coefficients (r) 0.94 and 0.96, respectively, from 135 clear sky datasets as compared to RMSE over heterogeneous ones (59 and 28Wm super(-) super(2) with r=0.66 and 0.82, respectively from 22 datasets). The intercomparison with another Lambda based approach (LST-NDVI 2D scatter) showed the supremacy of Lambda determined from LST-albedo 2D scatter. The efficiency of LST-NDVI scatter was better during the dry down or water limited phases of crop growth only. The uncertainties of lambda E estimates were attributed to errors in core radiation budget inputs, relative loss of conservativeness of Lambda due to canopy heterogeneity, and the inherent limitations of the single-source approach. There is further scope to reduce present lambda E uncertainties by combining the new findings on Lambda (LST-albedo scatter)-NDVI triangular relations, diurnal Lambda and two-source radiation budget.
机译:使用中分辨率(箭头右千米)中午卫星观测值测试了基于简化蒸发分数(Lambda)的单源能量平衡方案,以评估各种农业景观上晴空的潜热通量(E)。该方法使用地表温度(LST)和反照率之间的二维(2D)散射来确定Lambda。该计划的运行效用已被证明可用于估计狂犬病(11月至4月)作物生长期的区域蒸散量和耗水量,从而使用时间序列数据预测收割前的小麦产量(误差在报告平均值的15.9%之内)。发现在低表层土壤湿度下,基线(斜边)与LAI或NDVI线性耦合时,λ与LAI(叶面积指数)或NDVI(归一化植被指数)之间存在三角关系。对原位Lambda日变化过程的分析证明了恒定Lambda假设在纯,均匀,均质农作物冠层上的有效性,但在非均质,混合农作物冠层上显示出不规则和波状模式。在具有相关系数(r)的同质农业冠层(41和23Wm super(-)super(2))上,中午和白天平均Lambda E估计值的午间和白天平均Lambda E估计值的均方根误差(RMSE)也较小。 135个晴朗天空数据集的数据分别为0.94和0.96,而异类数据集的RMSE分别为22个数据集的59和28Wm super(-)super(2),r = 0.66和0.82。与另一种基于Lambda的方法(LST-NDVI 2D散点图)的比较表明,从LST-反照率2D散点图确定的Lambda至高无上。仅在作物生长的干旱或水分受限阶段,LST-NDVI散射的效率更高。 Lambda E估计值的不确定性归因于核心辐射预算输入中的误差,由于冠层异质性导致的Lambda保守性相对损失以及单一来源方法的固有局限性。通过结合关于Lambda(LST-反照率散射)-NDVI三角关系,日间Lambda和两源辐射预算的新发现,还有进一步的空间来减少当前的Lambda E不确定性。

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