학술논문

Super-resolution Snow-cover Mapping of Ku-Band based ISRO’s SCATSAT-1 Data using Spectral Mixture Analysis
Document Type
Conference
Source
IGARSS 2023 - 2023 IEEE International Geoscience and Remote Sensing Symposium Geoscience and Remote Sensing Symposium, IGARSS 2023 - 2023 IEEE International. :129-132 Jul, 2023
Subject
Aerospace
Components, Circuits, Devices and Systems
Fields, Waves and Electromagnetics
Geoscience
Signal Processing and Analysis
Satellites
Graphical models
Radar measurements
Snow
Superresolution
Spatial resolution
Remote sensing
Scatterometer Satellite (SCATSAT-1)
Himalayas
Super-Resolution Mapping (SRM)
Linear Spectral Mixing (LSM)
Language
ISSN
2153-7003
Abstract
The Scatterometer Satellite (SCATSAT-1), launched by ISRO has been utilized in many remote sensing applications to deliver near-real-time monitoring services. To represent the SCATSAT-1 applicability, the major scientific domains include hydrological studies, cryospheric applications, understanding the oceanic dynamics and agriculture applications. SCATSAT-1 offers various levels of data products with the best spatial resolution of ~2 km (Level-4), enhanced via the Scatterometer image reconstruction (SIR) technique. For the same reason, it may restrict the applicability of SCATSAT-1 in extracting different land-cover types. In this work, super-resolution mapping (SRM) has been utilized to estimate and improve the spatial distribution of land cover classes at the sub-pixel level. To achieve the SRM, the linear spectral mixing (LSM) model has been utilized in snow-cover mapping using SCATSAT-1 and MOD02 (MODIS) based normalized difference snow index (NDSI) dataset. This study has been conducted over a part of the rugged terrain Himalayan region (Himachal Pradesh State, India). Results show that satisfactory thematic maps have been generated via the SRM approach. The use of SRM is, therefore, a promising method to improve the spatial representation of the SCATSAT-1 dataset which may enhance the scope of ISRO’s SCATSAT-1 not only in the cryosphere but also in other scientific domains.