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在该项目中,根据单日小型无人机系统(sUAS)和涡度相关法(EC)信息评估日蒸散量方法。

Assessing Daily Evapotranspiration Methodologies from One-Time-of-Day sUAS and EC Information in the Project.

作者信息

Nassar Ayman, Torres-Rua Alfonso, Kustas William, Alfieri Joseph, Hipps Lawrence, Prueger John, Nieto Héctor, Alsina Maria Mar, White William, McKee Lynn, Coopmans Calvin, Sanchez Luis, Dokoozlian Nick

机构信息

Department of Civil and Environmental Engineering, Utah State University, Logan, UT 84322, USA.

Utah Water Research Laboratory, Utah State University, Logan, UT 84322, USA.

出版信息

Remote Sens (Basel). 2021 Aug 1;13(15):2887. doi: 10.3390/rs13152887. Epub 2021 Jul 23.

DOI:10.3390/rs13152887
PMID:35003785
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8739081/
Abstract

Daily evapotranspiration ( ) plays a key role in irrigation water management and is particularly important in drought-stricken areas, such as California and high-value crops. Remote sensing allows for the cost-effective estimation of spatial evapotranspiration (), and the advent of small unmanned aerial systems () technology has made it possible to estimate instantaneous high-resolution at the plant, row, and subfield scales. estimates using "instantaneous" remote sensing measurements with half-hourly/hourly forcing micrometeorological data, yielding hourly fluxes in W/m that are then translated to a daily scale (mm/day) under two assumptions: (a) relative rates, such as the ratios of -to-net radiation ( ) or -to-solar radiation ( ), are assumed to be constant rather than absolute, and (b) nighttime evaporation () and transpiration () contributions are negligible. While assumption (a) may be reasonable for unstressed, full cover crops (no exposed soil), the and rates may significantly vary over the course of the day for partially vegetated cover conditions due to diurnal variations of soil and crop temperatures and interactions between soil and vegetation elements in agricultural environments, such as vineyards and orchards. In this study, five existing extrapolation approaches that compute the daily from the "instantaneous" remotely sensed estimates and the eddy covariance () flux tower measurements were evaluated under different weather, grapevine variety, and trellis designs. Per assumption (b), the nighttime contribution was ignored. Each extrapolation technique (evaporative fraction (), solar radiation ( ), net radiation-to-solar radiation ( ) ratio, Gaussian (), and Sine) makes use of clear skies and quasi-sinusoidal diurnal variations of hourly and other meteorological parameters. The estimates and measurements were collected over multiple years and times from different vineyard sites in California as part of the USDA Agricultural Research Service Grape Remote Sensing Atmospheric Profile and Evapotranspiration eXperiment (). Optical and thermal imagery data at 10 cm and 60 cm, respectively, were collected by the Utah State University Program and used in the Two-Source Energy Balance () model to estimate the instantaneous or hourly at overpass time. The hourly from the measurements was also used to validate the extrapolation techniques. Overall, the analysis using measurements indicates that the , , and approaches presented the best goodness-of-fit statistics for a window of time between 1030 and 1330 PST (Pacific Standard Time), with the approach yielding better agreement with the measurements. Similar results were found using and data. The 1030-1330 time window also provided the greatest agreement between the actual daily and the extrapolated daily , with the approach again yielding better agreement with the ground measurements. The expected accuracy of the upscaled daily estimates across all vineyard sites in California is below 0.5 mm/day, ( extrapolation accuracy was found to be 0.34 mm/day), making the daily scale results from reliable and suitable for day-to-day water management applications.

摘要

日蒸散量( )在灌溉用水管理中起着关键作用,在干旱地区(如加利福尼亚州)以及高价值作物种植区尤为重要。遥感技术能够经济高效地估算空间蒸散量( ),小型无人机系统( )技术的出现使得在植株、行和子田尺度上估算瞬时高分辨率的蒸散量成为可能。 通过利用半小时/小时强迫微气象数据的“瞬时”遥感测量来估算蒸散量,得出以W/m为单位的每小时通量,然后在两个假设下转换为日尺度(mm/天):(a)假设诸如蒸散量与净辐射( )之比或蒸散量与太阳辐射( )之比等相对比率是恒定的,而非绝对的;(b)夜间蒸发( )和蒸腾( )的贡献可忽略不计。虽然假设(a)对于未受胁迫的全覆盖作物(无裸露土壤)可能是合理的,但由于农业环境(如葡萄园和果园)中土壤和作物温度的日变化以及土壤与植被要素之间的相互作用,对于部分植被覆盖条件,蒸散量和蒸腾速率在一天中可能会有显著变化。在本研究中,评估了五种现有的外推方法,这些方法根据“瞬时”遥感蒸散量估算值和涡度相关( )通量塔测量值来计算日蒸散量,评估是在不同天气、葡萄品种和棚架设计条件下进行的。根据假设(b),忽略了夜间蒸散量的贡献。每种外推技术(蒸发分数( )、太阳辐射( )、净辐射与太阳辐射( )之比、高斯( )和正弦)都利用了晴空条件以及每小时蒸散量和其他气象参数的准正弦日变化。作为美国农业部农业研究服务局葡萄遥感大气剖面与蒸散实验( )的一部分,多年来在不同时间从加利福尼亚州的不同葡萄园地点收集了蒸散量估算值和涡度相关测量值。犹他州立大学 项目分别收集了10厘米和60厘米的光学和热红外影像数据,并用于双源能量平衡( )模型,以估算过境时刻的瞬时或每小时蒸散量。来自涡度相关测量的每小时蒸散量也用于验证外推技术。总体而言,使用涡度相关测量的分析表明,在太平洋标准时间1030至1330的时间段内, 、 和 方法呈现出最佳的拟合优度统计结果,其中 方法与涡度相关测量结果的一致性更好。使用光学和热红外数据也发现了类似结果。1030 - 1330这个时间段还使得实际日蒸散量与外推的日蒸散量之间的一致性最高, 方法再次与地面测量结果的一致性更好。加利福尼亚州所有葡萄园地点的日蒸散量估算值向上扩展后的预期精度低于0.5毫米/天( 外推精度为0.34毫米/天),这使得来自 的日尺度结果可靠且适用于日常用水管理应用。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e6f7/8739081/1bbc386ecedc/nihms-1766090-f0021.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e6f7/8739081/c16a63e84a50/nihms-1766090-f0009.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e6f7/8739081/738ef5f3eb40/nihms-1766090-f0019.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e6f7/8739081/1bbc386ecedc/nihms-1766090-f0021.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e6f7/8739081/c16a63e84a50/nihms-1766090-f0009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e6f7/8739081/5e104d72ba64/nihms-1766090-f0011.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e6f7/8739081/b7ee47b93b95/nihms-1766090-f0013.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e6f7/8739081/3c47cf6a7a02/nihms-1766090-f0017.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e6f7/8739081/738ef5f3eb40/nihms-1766090-f0019.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e6f7/8739081/1bbc386ecedc/nihms-1766090-f0021.jpg

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