Hyperspectral narrowband and multispectral broadband indices for remote sensing of crop evapotranspiration and its components (transpiration and soil evaporation)

被引:68
作者
Marshall, Michael [1 ,2 ]
Thenkabail, Prasad [2 ]
Biggs, Trent [3 ]
Post, Kirk [4 ,5 ]
机构
[1] World Agroforestry Ctr, Climate Res Unit, United Nations Ave,POB 30677-00100, Nairobi, Kenya
[2] US Geol Survey, Southwestern Geog Ctr, 2255 N Gemini Dr, Flagstaff, AZ 86001 USA
[3] San Diego State Univ, Dept Geog, Storm Hall 308C, San Diego, CA 92182 USA
[4] CSU Monterey Bay, 100 Campus Ctr, Seaside, CA 93955 USA
[5] NASA ARC Cooperat, Chapman Sci Ctr, 100 Campus Ctr, Seaside, CA 93955 USA
基金
美国国家航空航天局;
关键词
Spectroscopy; Micrometeorology; Latent heat; Energy balance; HyspIRI; PHOTOCHEMICAL REFLECTANCE INDEX; LAND-SURFACE EVAPORATION; ENERGY-BALANCE CLOSURE; VEGETATION INDEXES; WATER INDEX; GLOBAL EVAPOTRANSPIRATION; IMAGING SPECTROSCOPY; MODIS; CANOPY; CHLOROPHYLL;
D O I
10.1016/j.agrformet.2015.12.025
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Evapotranspiration (ET) is an important component of micro- and macro-scale climatic processes. In agriculture, estimates of ET are frequently used to monitor droughts, schedule irrigation, and assess crop water productivity over large areas. Currently, in situ measurements of ET are difficult to scale up for regional applications, so remote sensing technology has been increasingly used to estimate crop ET. Ratio-based vegetation indices retrieved from optical remote sensing, like the Normalized Difference Vegetation Index (NDVI), Soil Adjusted Vegetation Index, and Enhanced Vegetation Index are critical components of these models, particularly for the partitioning of ET into transpiration and soil evaporation. These indices have their limitations, however, and can induce large model bias and error. In this study, micrometeorological and spectroradiometric data collected over two growing seasons in cotton, maize, and rice fields in the Central Valley of California were used to identify spectral wavelengths from 428 to 2295 nm that produced the highest correlation to and lowest error with ET, transpiration, and soil evaporation. The analysis was performed with hyperspectral narrowbands (HNBs) at 10 nm intervals and multispectral broadbands (MSBBs) commonly retrieved by Earth observation platforms. The study revealed that (1) HNB indices consistently explained more variability in ET (Delta R-2 = 0.12), transpiration (Delta R-2 = 0.17), and soil evaporation (Delta R-2 = 0.14) than MSBB indices; (2) the relationship between transpiration using the ratio-based index most commonly used for ET modeling, NDVI, was strong (R-2 = 0.51), but the hyperspectral equivalent was superior (R-2 = 0.68); and (3) soil evaporation was not estimated well using ratio-based indices from the literature (highest R-2 = 0.37), but could be after further evaluation, using ratio-based indices centered on 743 and 953 nm (R-2 = 0.72) or 428 and 1518 nm (R-2 = 0.69). (C) 2015 The Authors. Published by Elsevier B.V.
引用
收藏
页码:122 / 134
页数:13
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