4.7 Article

Estimation of dry vegetation cover and mass from MODIS data: Verification by roughness length and sand saltation threshold

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ELSEVIER
DOI: 10.1016/j.jag.2021.102417

关键词

Dry vegetation; Soil Tillage Index; Roughness length; Threshold friction velocity; Arid region

资金

  1. Arid Land Research Center project titled Impacts of Climate Change on Drylands: Assessment and Adaptation - Japan's Ministry of Education, Culture, Sports, Science, and Technology
  2. Joint Research Program of the Arid Land Research Center, Tottori University [31C2003, 31C2012]
  3. Environment Research and Technology Development Fund of the Environmental Restoration and Conservation Agency of Japan [JPMEERF20205001]
  4. [15H05115]
  5. [17H01616]
  6. [16H02712]
  7. [25220201]

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The study found that using MODIS data and SWIR vegetation indices in the northern Gobi Desert can accurately estimate the coverage and mass of dry vegetation. The Soil Tillage Index (STI) and Normalized Difference Tillage Index (NDTI) performed well in this aspect, improving future wind erosion risk assessments in arid and semi-arid environments.
Monitoring of dry vegetation in arid and semi-arid regions is crucial in environmental investigations such as assessments of wind erosion risk, livestock forage, and fire risk. However, there has been little research into estimating the coverage and mass of dry (non-photosynthetic) vegetation. In our study area at Tsogt-Ovoo (TsO) in the northern Gobi Desert, Mongolia, we used MODIS data to compare observed dry vegetation cover (VCd obs) and mass (M-d_obs) with values estimated from the Normalized Difference Vegetation Index (NDVI) and six other potential Short Wavelength InfraRed (SWIR) dry vegetation indices. Of the seven vegetation indices, the Soil Tillage Index (STI) and Normalized Difference Tillage Index (NDTI), both of which are calculated from SWIR bands 6 and 7, provided good estimates of (VCd_obs) and (M-d_obs). Our comparisons of observed roughness length (z(0)) and threshold friction velocity (u*t) for sand saltation at stony and non-stony sites with dry vegetation cover determined from STI verified its suitability for estimating VCd(STI). At both sites, the observed z(0)and u(*t)increased with increasing estimated VCd(STI). Based on their relationships with STI, we predicted values of z(0)and u(*t)in the absence of dry vegetation that were in accordance with published data. The threshold wind speeds at 10 m height derived from u(*t)at both the stony and non-stony sites were reasonably close to the value that is commonly used in dust models. Thus, we verified that STI is a suitable index for estimating the amount of dry vegetation in the Gobi Desert and, potentially, in other arid and semi-arid regions. Although the relationships of z(0)and u(*t)with STI require further validation, it appears that the use of STI can improve future wind erosion risk assessments in arid and semi-arid environments.

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