4.7 Article

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

Journal

AGRICULTURAL AND FOREST METEOROLOGY
Volume 218, Issue -, Pages 122-134

Publisher

ELSEVIER
DOI: 10.1016/j.agrformet.2015.12.025

Keywords

Spectroscopy; Micrometeorology; Latent heat; Energy balance; HyspIRI

Funding

  1. United States Geological Survey (USGS) Mendenhall Research Fellowship Program
  2. USGS
  3. National Association of Geoscience Teachers cooperative agreement
  4. California Energy Commission
  5. USGS Federal Matching Funds program
  6. U.S. Department of Energy's Office of Science Ameriflux program
  7. California Department of Water Resources (CADWR)
  8. National Aeronautics and Space Administration (NASA)
  9. University of California (UC) at Berkeley and Davis

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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.

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