Abstract

Cloud obscuration is a major problem for using Moderate Resolution Imaging Spectroradiometer (MODIS) images in different applications. This issue poses serious difficulties in monitoring the snow cover in mountainous regions due to high cloudiness in such areas. To overcome this, different cloud removal methods have been developed in the past where most of them use MODIS snow cover products and spatiotemporal dependencies of snow to estimate the undercloud coverage. In this study, a new approach is adopted that uses surface reflectance data in the cloud-free pixels and estimates the surface reflectance of a cloudy pixel as if there were no cloud. This estimation is obtained by subsequently applying the k-nearest neighbor and dynamic time compositing methods. The modified surface reflectance data are then utilized as inputs of a Normalized Difference Snow Index (NDSI)-based algorithm to map snow cover in the study area. The results indicate that the suggested approach is able to appropriately estimate undercloud surface reflectance in bands 2, 4 and 6, and can map the snow cover with 97% accuracy, which is a substantial improvement over the conventional method with an accuracy of 86%. Finally, although a clear underestimation of snow cover (about 15%) is observed by applying the proposed approach, still, it is much better than the 30% underestimation obtained by the conventional method.

Highlights

  • Snow is an important component of hydrological cycle

  • The results indicate that the suggested approach is able to appropriately estimate undercloud surface reflectance in bands

  • 2, 4 and 6, and can map the snow cover with 97% accuracy, which is a substantial improvement over the conventional method with an accuracy of 86%

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Summary

Introduction

Many efforts have been made to measure and accurately estimate it in river basins for better management of water resources. In situ measurements are the most common way to quantify snow variations. Such measurements are costly and limited to a few points that are mostly located in lower elevations of basins. Snow varies drastically in temporal and spatial extent and it is mainly concentrated at higher elevations. The development of remote sensing technology has offered an alternative for snow monitoring. This technology provides near global coverage, high temporal and spatial resolution, and is able to measure different parameters

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