利用Lysimeter和无人机多光谱影像可靠估算石榴树的树级蒸散量

Haoyu Niu, Tiebiao Zhao, Jiamin Wei, Dong Wang, Y. Chen
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引用次数: 4

摘要

准确估算和绘制作物蒸散量对作物水分管理具有重要意义。作物系数(Kc)是传统的蒸散发估算方法之一。许多研究表明Kc曲线与植被指数曲线之间存在线性回归关系。通常在Kc与卫星影像的归一化植被指数(NDVI)之间建立线性回归模型。卫星图像可以提供时间和空间分布的测量结果。然而,多光谱卫星图像的空间分辨率在米的范围内,这对于树木和藤蔓等具有块状冠层结构的作物来说往往是不够的。基于单树水平的蒸散发估算研究很少。因此,本研究的目的是建立一种可靠的基于无人机高分辨率多光谱图像的树级ET估算方法。与卫星图像相比,无人机图像的空间分辨率可高达厘米级。本研究在美国加州议会圣华金谷农业科学中心对石石榴树进行了实地研究。NDVI地图来源于无人机图像。Kc值是根据称重蒸渗仪的实际蒸散发和气象站的参考蒸散发计算的。建立NDVI与Kc之间的线性回归模型,对日实际ET进行估计。结果表明,该线性回归模型可以估计树水平ET, R2和平均绝对误差(MAE)分别为0.9143和0.39 mm/d。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Reliable Tree-level Evapotranspiration Estimation of Pomegranate Trees Using Lysimeter and UAV Multispectral Imagery
The accurate estimation and mapping of evapotranspiration (ET) are essential for crop water management. As one of the traditional ET estimation methods, crop coefficient (Kc) has been commonly used. Many studies indicated a linear regression relationship between the Kc curve and the vegetation index curve. The linear regression model is usually developed between the Kc and the normalized difference vegetation index (NDVI) derived from satellite imagery. The satellite images can provide temporally and spatially distributed measurements. However, multispectral satellite imagery’s spatial resolution is in the range of meters, which is often not enough for crops with clumped canopy structures, such as trees and vines. Little ET estimation has been studied based on the single-tree level. Thus, the purpose of this study was to develop a reliable tree-level ET estimation method using UAV high-resolution multispectral images. Compared with satellite imagery, the spatial resolution of UAV images can be as high as centimeter-level. A field study was conducted to investigate pomegranate trees at the USDA-ARS (US Department of Agriculture, Agricultural Research Service) San Joaquin Valley Agricultural Sciences Center in Parlier, California, USA. The NDVI map was derived from UAV imagery. The Kc values were calculated based on the actual ET from a weighing lysimeter and reference ET from the weather station. The authors then established a linear regression model between the NDVI and Kc to estimate the actual daily ET. Results showed that the linear regression model could estimate tree-level ET with an R2 and mean absolute error (MAE) of 0.9143 and 0.39 mm/day, respectively.
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