4.7 Article

Modeling Vegetation Water Stress over the Forest from Space: Temperature Vegetation Water Stress Index (TVWSI)

Journal

REMOTE SENSING
Volume 13, Issue 22, Pages -

Publisher

MDPI
DOI: 10.3390/rs13224635

Keywords

Moderate Resolution Imaging Spectroradiometer (MODIS); soil moisture; vegetation water stress; LST-NDVI trapezoid; AWRA-L; Temperature Vegetation Water Stress Index (TVWSI)

Funding

  1. Integrated Forest Ecosystem Research program - Victorian Department of Environment, Land, Water and Planning (DELWP) [094687]
  2. University of Melbourne Research Scholarship (MRS) [268129]

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A new Temperature Vegetation Water Stress Index (TVWSI) was proposed in this study, which combines canopy temperature, water content, and fractional cover to predict soil moisture more accurately. TVWSI showed high correlation with observed data and outperformed other widely used water stress indices in soil moisture prediction accuracy.
The conventional Land Surface Temperature (LST)-Normalized Difference Vegetation Index (NDVI) trapezoid model has been widely used to retrieve vegetation water stress. However, it has two inherent limitations: (1) its complex and computationally intensive parameterization for multi-temporal observations and (2) deficiency in canopy water content information. We tested the hypothesis that an improved water stress index could be constructed by the representation of canopy water content information to the LST-NDVI trapezoid model. Therefore, this study proposes a new index that combines three indicators associated with vegetation water stress: canopy temperature through LST, canopy water content through Surface Water Content Index (SWCI), and canopy fractional cover through NDVI in one temporally transferrable index. Firstly, a new optical space of SWCI-NDVI was conceptualized based on the linear physical relationship between shortwave infrared (SWIR) and soil moisture. Secondly, the SWCI-NDVI feature space was parameterized, and an index d(SWCI, NDVI) was computed based on the distribution of the observations in the SWCI-NDVI spectral space. Finally, standardized LST (LST/long term mean of LST) was combined to d(SWCI, NDVI) to give a new water stress index, Temperature Vegetation Water Stress Index (TVWSI). The modeled soil moisture from the Australian Water Resource Assessment-Landscape (AWRA-L) and Soil Water Fraction (SWF) from four FLUXNET sites across Victoria and New South Wales were used to evaluate TVWSI. The index TVWSI exhibited a high correlation with AWRA-L soil moisture (R-2 of 0.71 with p < 0.001) and the ground-based SWF (R-2 of 0.25-0.51 with p < 0.001). TVWSI predicted soil moisture more accurately with RMSE of 21.82 mm (AWRA-L) and 0.02-0.04 (SWF) compared to the RMSE ranging 28.98-36.68 mm (AWRA-L) and 0.03-0.05 (SWF) were obtained for some widely used water stress indices. The TVWSI could also be a useful input parameter for other environmental models.

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