Concentration and thickness of sea ice in the Weddell Sea from SSM/I passive microwave radiometer data

Abstract This study evaluated feasibility statistically and analyzed, during the freezing period, the relationship between brightness temperature (Tb) data of the 37V polarisation and the GR3719 (Gradient Ratio 37V and 19V) obtained by Special Sensor Microwave/Imager from F11 and F13 satellites with...

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Bibliographic Details
Published in:Anais da Academia Brasileira de Ciências
Main Authors: FERNANDO LUIS HILLEBRAND, MARCOS W.D. DE FREITAS, ULISSES F. BREMER, TALES C. ABRANTES, JEFFERSON C. SIMÕES, CLÁUDIO W. MENDES JÚNIOR, FREDERICO SCHARDONG, JORGE ARIGONY-NETO
Format: Article in Journal/Newspaper
Language:English
Published: Academia Brasileira de Ciências 2023
Subjects:
Q
Online Access:https://doi.org/10.1590/0001-3765202320230342
https://doaj.org/article/299bb73d77214aaaa43e195426f0eddb
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Summary:Abstract This study evaluated feasibility statistically and analyzed, during the freezing period, the relationship between brightness temperature (Tb) data of the 37V polarisation and the GR3719 (Gradient Ratio 37V and 19V) obtained by Special Sensor Microwave/Imager from F11 and F13 satellites with sea ice thickness (SIT) data obtained in the Weddell Sea through Antarctic Sea Ice Processes and Climate program. The multiple linear regression (MLR) was applied at 1,520 points, with 70% of these points being randomly separated to generate the MLR and 30% to carry out the validation. To perform the temporal mapping, the MLR was applied only to pixels with sea ice concentration (SIC) ≥ 90%, obtained through the fraction image calculated from the spectral linear mixing model (SLMM) using the Tb in the channels and polarizations 19H, 19V and 37V. The results of the SLMM validation process for estimating the SIC were σ = 10.5%, RMSE = 11.0%, and bias = -2.8%, and the SIT based on the MLR, the results were R² = 0.57, RMSE = 0.268 m, and bias = 0.103 m. In the SIT mapping, we highlight the trend of thickness reduction on the east coast of the Antarctic Peninsula during the period 1992–2009.