Potential of multispectral reflectance for assessment of snow geophysical parameters in Solang valley in the lower Indian Himalayas. Issue 1 (2nd January 2020)

• Record Type: Journal Article
• Authors: Varade, Divyesh; Dikshit, Onkar
• Is Part Of: GIScience & remote sensing. Volume 57:Issue 1(2020)
• Page Start: 107
• Page End: 126
• Publication Date: 2020-01-02
• Subjects: Snow wetness -- snow density -- snow permittivity -- near-infrared reflectance -- triangle method; Geodesy -- Periodicals; Cartography -- Periodicals; Aerial photogrammetry -- Periodicals; Remote sensing -- Periodicals; 526.05
• DOI: 10.1080/15481603.2019.1672365
• Languages: English
• ISSNs: 1548-1603

Abstract

ABSTRACT: Snow geophysical parameters such as wetness, density and permittivity are a significant input in hydrological models and water resource management. In this paper, we utilize the triangle method based on a feature space developed with the near-infrared (NIR) reflectance and the Normalized Differenced Snow Index (NDSI) for the estimation of surface snow wetness, permittivity and density. The triangular feature space based on NIR reflectance and NDSI is parameterized to yield a linear relationship between the snow wetness and the NIR reflectance. Snow density and permittivity are derived based on the least squares solution of empirical relations based on the observations of surface snow wetness. The proposed methodology was evaluated using Sentinel-2 data, and the modeled snow geophysical parameters were validated with respect to field measurements. Based on the results, it was inferred that the NIR reflectance varies linearly with the liquid water content in the snow. A good agreement was determined between the modeled and measured parameters for wet snow conditions as observed by the coefficient of determination of 0.968, 0.521 and 0.969 for the snow wetness, density and permittivity (real part), respectively. The proposed approach can be significantly utilized with unmanned aerial sensors for monitoring of physical properties of fresh or wet snow and is thus expected to contribute considerably in hydrological applications and avalanche studies.