4.7 Article

Diurnal and Seasonal Mapping of Water Deficit Index and Evapotranspiration by an Unmanned Aerial System: A Case Study for Winter Wheat in Denmark

Journal

REMOTE SENSING
Volume 13, Issue 15, Pages -

Publisher

MDPI
DOI: 10.3390/rs13152998

Keywords

drought stress; energy balance; fraction of transpirable soil water; temperature trapezoid; thermal imagery; vegetation index

Funding

  1. Innovation Fund Denmark [7049-00004B]

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Precision irrigation is a promising method to mitigate drought impacts on crop production by optimizing water resources. This study utilized unmanned aerial systems equipped with sensors to detect and quantify drought stress in winter wheat. The Water Deficit Index showed a strong correlation with plant water status. Future research should focus on temporal upscaling of evapotranspiration for developing site-specific irrigation recommendations.
Precision irrigation is a promising method to mitigate the impacts of drought stress on crop production with the optimal use of water resources. However, the reliable assessment of plant water status has not been adequately demonstrated, and unmanned aerial systems (UAS) offer great potential for spatiotemporal improvements. This study utilized UAS equipped with multispectral and thermal sensors to detect and quantify drought stress in winter wheat (Triticum aestivum L.) using the Water Deficit Index (WDI). Biennial field experiments were conducted on coarse sand soil in Denmark and analyses were performed at both diurnal and seasonal timescales. The WDI was significantly correlated with leaf stomatal conductance (R-2 = 0.61-0.73), and the correlation was weaker with leaf water potential (R-2 = 0.39-0.56) and topsoil water status (the highest R-2 of 0.68). A semi-physical model depicting the relationship between WDI and fraction of transpirable soil water (FTSW) in the root zone was derived with R-2 = 0.74. Moreover, WDI estimates were improved using an energy balance model with an iterative scheme to estimate the net radiation and land surface temperature, as well as the dual crop coefficient. The diurnal variation in WDI revealed a pattern of the ratio of actual to potential evapotranspiration, being higher in the morning, decreasing at noon hours and 'recovering' in the afternoon. Future work should investigate the temporal upscaling of evapotranspiration, which may be used to develop methods for site-specific irrigation recommendations.

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