Abstract

Geospatial crop water use mapping is critical for field-scale site-specific irrigation management. Landsat 7/8 satellite imagery with a widely adopted METRIC (Mapping Evapotranspiration at high Resolution with Internalized Calibration) energy balance model (LM approach) estimates accurate evapotranspiration (ET) but limits field-scale spatiotemporal (30 m pixel−1, ~16 days) mapping. A study was therefore conducted to map actual ET of commercially grown irrigated-field crops (spearmint, potato, and alfalfa) at very high-resolution (7 cm pixel−1). Six small unmanned aerial system (UAS)-based multispectral and thermal infrared imagery campaigns were conducted (two for each crop) at the same time as the Landsat 7/8 overpass. Three variants of METRIC model were used to process the UAS imagery; UAS-METRIC-1, -2, and -3 (UASM-1, -2, and -3) and outputs were compared with the standard LM approach. ET root mean square differences (RMSD) between LM-UASM-1, LM-UASM-2, and LM-UASM-3 were in the ranges of 0.2–2.9, 0.5–0.9, and 0.5–2.7 mm day−1, respectively. Internal calibrations and sensible heat fluxes majorly resulted in such differences. UASM-2 had the highest similarity with the LM approach (RMSD: 0.5–0.9, ETdep,abs (daily ET departures): 2–14%, r (Pearson correlation coefficient) = 0.91). Strong ET correlations between UASM and LM approaches (0.7–0.8, 0.7–0.8, and 0.8–0.9 for spearmint, potato, and alfalfa crops) suggest equal suitability of UASM approaches as LM to map ET for a range of similar crops. UASM approaches (Coefficient of variation, CV: 6.7–24.3%) however outperformed the LM approach (CV: 2.1–11.2%) in mapping spatial ET variations due to large number of pixels. On-demand UAS imagery may thus help in deriving high resolution site-specific ET maps, for growers to aid in timely crop water management.

Highlights

  • Satellite-based remote sensing (RS) has been extensively used with energy balance models for regional scale evapotranspiration (ET) mapping [1,2,3,4,5,6,7,8]

  • ET root mean square differences (RMSD) between LM-UASM-1, LM-UASM-2, and LM-UASM-3 were in the ranges of 0.2–2.9, 0.5–0.9, and 0.5–2.7 mm day−1, respectively

  • UASM-2 had the highest similarity with the LM approach (RMSD: 0.5–0.9, ETdep,abs: 2–14%, r (Pearson correlation coefficient) = 0.91)

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Summary

Introduction

Satellite-based remote sensing (RS) has been extensively used with energy balance models for regional scale evapotranspiration (ET) mapping [1,2,3,4,5,6,7,8]. One such widely adopted model is Mapping. Drones 2020, 4, 52 conditions, stabilized sensible heat flux (H) estimations, and internal calibration using hot and cold anchor pixels. The METRIC model has been evaluated for a wide range of irrigated field and orchard/tree crops under different agroclimatic zones, with studies reporting ET estimation errors in the ranges of 1 to 11% [11,12,13,14,15,16,17,18,19,20,21,22]

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