Wednesday, August 26, 2020

Evaluation of SCATSAT-1 data for snow cover area mapping over a part of Western Himalayas

Regular monitoring and mapping of the Snow Cover Area (SCA) is important to manage the natural resources and to assess the impact of climate change on SCA. But, over inaccessible Western Himalayas, the estimation of the SCA is one of the challenging tasks due to its complex and rugged topography. SCA was mapped so far with optical sensors. Generally, the optical sensor data is affected by the presence of the cloud cover and is more sensitive towards interference from environmental effects. Alternatively, several developments were made by various authors to map the SCA using active or passive microwave data all over the globe.  It is proven that scatterometer data has the potential to retrieve the snow cover information. But the mapping of SCA using active microwave satellite data is still in its initial phase due to lower accuracy as compared to optical sensors data. 

Due to the recent advancements in classification algorithms such as Sub-Pixel Classification (SPC) and Super-Resolution Mapping (SRM), there is a clear requirement of extensive exploration of different classification algorithms for SCA estimation especially over complex undulating Western Himalayas using SCATSAT‒1 data. The integration and evaluation of advanced classification algorithms with scatterometer data are some of the primary issues in the remote sensing field. Therefore, with an investigation on such critical issues, it may be possible to extend the applicability of SCATSAT‒1 data in different applications. It is also expected that such the analysis will improve the performance of a scatterometer in the precise mapping of SCA over rugged terrain surface.

Methodology to generate Snow Cover Maps 

This study is capable to evaluate the Indian Satellite SCATSAT-1 data for snow cover mapping. Three classifiers KMC, SVM, and LSM were used for the generation of binary snow cover maps from SCATSAT-1 backscattered values. For better accuracy of the maps super-resolution mapping technique in conjunction with NDSI data has also been used. The results of classifiers and SRM have been compared with NDSI images generated from Landsat‒8 and MODIS data on clear sky days, respectively.  This means that LSM-SRM on SCATSAT-1 is a good candidate for classifying the SCMs at Ku-band but it requires an additional dataset. Further, such outcomes will be beneficial in the study of the cryosphere, especially on cloudy days. LSM-SRM results show that regular snow cover mapping for the generation of a time series maps in high‒altitude Himalayas and other regions of extreme climate sensitivity, where cloud cover plays an important role during the winter season, maybe possible by fusion of scatterometer data with optical sensor data. Currently, the application range of SCATSAT-1 may be limited due to some difficulties such as a) incidence angle variations affect the backscatter values, and b) difficult to identify pure endmember properties due to low spatial resolution. Further studies to overcome the limitations in examining SCA from scatterometer data may be useful for trend analysis of early snowmelts and seasonal snow cover variations.

Sood et al. (2020) address the potential of SCATSAT‒1 data for snow cover mapping over a part of Western Indian Himalayas. Three classifiers KMC, SVM, and LSM were used for the generation of binary snow cover maps from SCATSAT-1 backscattered values. For better accuracy of the maps super-resolution mapping technique in conjunction with NDSI data has also been used.
  
ReferenceSood V., Gusain H.S., Gupta S., Singh S., Kaur S. 2020. Evaluation of SCATSAT-1 data for snow cover area mapping over a part of Western Himalayas, Advances in Space Research, Elsevier.
Link for full study: https://doi.org/10.1016/j.asr.2020.08.017