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首页> 外文期刊>Irrigation Science >Using remote sensing to evaluate the spatial variability of evapotranspiration and crop coefficient in the lower Rio Grande Valley, New Mexico
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Using remote sensing to evaluate the spatial variability of evapotranspiration and crop coefficient in the lower Rio Grande Valley, New Mexico

机译:利用遥感技术评估新墨西哥州下里奥格兰德河谷蒸散量和作物系数的空间变异性

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Pecan is a major crop in the lower Rio Grande Valley (LRGV), New Mexico. Currently, about 11,000ha of pecan orchards at various stages of growth are consuming about 40% of irrigation water in the area. Pecan evapotranspiration (ET) varies with age, canopy cover, soil type and method of water management. There is a need for better quantification of pecan ET for the purpose of water rights adjudication, watershed management and agronomical practices. This paper describes a process where remote sensing information from Landsat-5 and Landsat-7 were combined with ground level measurements to estimate pecan ET and field scale actual crop coefficient (K sub(c)) for the LRGV. The results showed that annual pecan water use for 279 fields ranged from 498 to 1,259mm with an average water use of 1,054mm. For fields with NDVI>0.6 (normalized difference vegetation index), which represented mature orchards (total of 232 fields), the annual water use ranged from 771 to 1,259mm with an average water use of 1,077mm. The results from remote sensing model compared reasonably well with ground level ET values determined by an eddy covariance system in a mature pecan orchard with an average error of 4% and the standard error of estimate (SEE) ranging from 0.91 to 1.06mm/day. A small fraction (5%) of the pecan fields were within the range of maximum ET and K sub(c).
机译:山核桃是新墨西哥州下里奥格兰德河谷(LRGV)的主要农作物。目前,该地区处于不同生长阶段的约11,000公顷山核桃果园消耗了约40%的灌溉水。山核桃的蒸散量(ET)随年龄,树冠覆盖,土壤类型和水管理方法的不同而不同。为了水权判决,流域管理和农艺实践,有必要对山核桃ET进行更好的定量。本文介绍了一个过程,其中将来自Landsat-5和Landsat-7的遥感信息与地面测量值相结合,以估计山核桃ET和LRGV的田间尺度实际作物系数(K sub(c))。结果表明,279个油田的山核桃年用水量在498至1,259mm之间,平均用水量为1,054mm。对于代表成熟果园(总计232个田地)的NDVI> 0.6(归一化差异植被指数)的田地,年用水量在771至1,259mm之间,平均用水量为1,077mm。遥感模型的结果与涡流协方差系统在成熟的山核桃果园中确定的地面水平ET值进行了合理的比较,平均误差为4%,估计的标准误差(SEE)为0.91至1.06mm /天。一小部分(5%)的山核桃田在最大ET和K sub(c)的范围内。

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