A Scatterometer is a microwave radar instrument designed specifically for ocean Applications. Although due to strong sensitivity to wetness in snow, it has been extensively used for the cryosphere applications such as extraction of snow parameters, With Scatterometers, the accuracy and complexities of snow detection algorithms are the major concerns as compared to optical data (multispectral) based algorithms since snow is more separable using visible wavelengths as compared to microwave wavelengths. But optical data are limited to cloud-free days and this is an important advantage of microwave data as compared to optical measurements where practically any cloud limits the exact characterization of the land surface state.
Sartajvir Singh Dhillon
Friday, November 27, 2020
Detection and validation of spatiotemporal snow cover variability in the Himalayas using Ku-band (13.5 GHz) SCATSAT-1 data
Tuesday, October 13, 2020
Monitoring and mapping of snow cover variability using topographically derived NDSI model over north Indian Himalayas during the period 2008–19
The Himalayas is an essential component of the cryosphere due to the large extent of snow or ice cover. The mapping and monitoring of snow cover variability over the Himalayas is the focus of many scientific studies due to the major source of water for Asian countries and equally important for climate change studies. This study describes the analysis of snow cover variability over North Indian Himalayas (NIH) covering Western Himalayas and Karakoram mountain ranges. The snow cover area (SCA) has been analyzed in three different climate zones such as the upper Himalayan zone (UHZ) (Ladakh and Karakoram range), middle Himalayan zone (MHZ) (Great Himalaya and Zanskar), and lower Himalayan zone (LHZ) (Pir Panjal and Shamshbari range) at various elevation levels as well as aspect levels during the past decade (2008–2019). The snow cover maps have been generated for NIH and its climate zones from Moderate Resolution Imaging Spectroradiometer (MODIS) data.
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.