Theoretical study of ice cover phenology at large freshwater lakes based on SMOS MIRAS data

The paper presents a theoretical analysis of seasonal brightness temperature variations at a number of large freshwater lakes: Baikal, Ladoga, Great Bear Lake (GBL), Great Slave Lake (GSL), and Huron, retrieved from Microwave Imaging Radiometer with Aperture Synthesis (MIRAS) data (1.4 GHz) of the S...

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Published in:The Cryosphere
Main Authors: V. Tikhonov, I. Khvostov, A. Romanov, E. Sharkov
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-12-2727-2018
https://www.the-cryosphere.net/12/2727/2018/tc-12-2727-2018.pdf
https://doaj.org/article/dd7d2d1708594a1588db8c38681a236f
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:dd7d2d1708594a1588db8c38681a236f 2023-05-15T16:22:59+02:00 Theoretical study of ice cover phenology at large freshwater lakes based on SMOS MIRAS data V. Tikhonov I. Khvostov A. Romanov E. Sharkov 2018-08-01 https://doi.org/10.5194/tc-12-2727-2018 https://www.the-cryosphere.net/12/2727/2018/tc-12-2727-2018.pdf https://doaj.org/article/dd7d2d1708594a1588db8c38681a236f en eng Copernicus Publications doi:10.5194/tc-12-2727-2018 1994-0416 1994-0424 https://www.the-cryosphere.net/12/2727/2018/tc-12-2727-2018.pdf https://doaj.org/article/dd7d2d1708594a1588db8c38681a236f undefined The Cryosphere, Vol 12, Pp 2727-2740 (2018) envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2018 fttriple https://doi.org/10.5194/tc-12-2727-2018 2023-01-22T19:33:27Z The paper presents a theoretical analysis of seasonal brightness temperature variations at a number of large freshwater lakes: Baikal, Ladoga, Great Bear Lake (GBL), Great Slave Lake (GSL), and Huron, retrieved from Microwave Imaging Radiometer with Aperture Synthesis (MIRAS) data (1.4 GHz) of the Soil Moisture and Ocean Salinity (SMOS) satellite. The analysis was performed using the model of microwave radiation of plane layered heterogeneous nonisothermal medium. The input parameters for the model were real regional climatological characteristics and glaciological parameters of ice cover of the study lakes. Three distinct seasonal brightness temperature time regions corresponding to different phenological phases of the lake surfaces: complete ice cover, ice melt and deterioration, and open water were revealed. The paper demonstrates the possibility to determine the beginning of ice cover deterioration from satellite microwave radiometry data. The obtained results can be useful for setting the operating terms of winter crossings and roads on ice, as with the beginning of ice deterioration, these transportation routes across water bodies (rivers, lakes, water reservoirs) become insecure and cannot be used any more. Article in Journal/Newspaper Great Bear Lake Great Slave Lake The Cryosphere Unknown Great Bear Lake ENVELOPE(-120.753,-120.753,65.834,65.834) Great Slave Lake ENVELOPE(-114.001,-114.001,61.500,61.500) The Cryosphere 12 8 2727 2740
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic envir
geo
spellingShingle envir
geo
V. Tikhonov
I. Khvostov
A. Romanov
E. Sharkov
Theoretical study of ice cover phenology at large freshwater lakes based on SMOS MIRAS data
topic_facet envir
geo
description The paper presents a theoretical analysis of seasonal brightness temperature variations at a number of large freshwater lakes: Baikal, Ladoga, Great Bear Lake (GBL), Great Slave Lake (GSL), and Huron, retrieved from Microwave Imaging Radiometer with Aperture Synthesis (MIRAS) data (1.4 GHz) of the Soil Moisture and Ocean Salinity (SMOS) satellite. The analysis was performed using the model of microwave radiation of plane layered heterogeneous nonisothermal medium. The input parameters for the model were real regional climatological characteristics and glaciological parameters of ice cover of the study lakes. Three distinct seasonal brightness temperature time regions corresponding to different phenological phases of the lake surfaces: complete ice cover, ice melt and deterioration, and open water were revealed. The paper demonstrates the possibility to determine the beginning of ice cover deterioration from satellite microwave radiometry data. The obtained results can be useful for setting the operating terms of winter crossings and roads on ice, as with the beginning of ice deterioration, these transportation routes across water bodies (rivers, lakes, water reservoirs) become insecure and cannot be used any more.
format Article in Journal/Newspaper
author V. Tikhonov
I. Khvostov
A. Romanov
E. Sharkov
author_facet V. Tikhonov
I. Khvostov
A. Romanov
E. Sharkov
author_sort V. Tikhonov
title Theoretical study of ice cover phenology at large freshwater lakes based on SMOS MIRAS data
title_short Theoretical study of ice cover phenology at large freshwater lakes based on SMOS MIRAS data
title_full Theoretical study of ice cover phenology at large freshwater lakes based on SMOS MIRAS data
title_fullStr Theoretical study of ice cover phenology at large freshwater lakes based on SMOS MIRAS data
title_full_unstemmed Theoretical study of ice cover phenology at large freshwater lakes based on SMOS MIRAS data
title_sort theoretical study of ice cover phenology at large freshwater lakes based on smos miras data
publisher Copernicus Publications
publishDate 2018
url https://doi.org/10.5194/tc-12-2727-2018
https://www.the-cryosphere.net/12/2727/2018/tc-12-2727-2018.pdf
https://doaj.org/article/dd7d2d1708594a1588db8c38681a236f
long_lat ENVELOPE(-120.753,-120.753,65.834,65.834)
ENVELOPE(-114.001,-114.001,61.500,61.500)
geographic Great Bear Lake
Great Slave Lake
geographic_facet Great Bear Lake
Great Slave Lake
genre Great Bear Lake
Great Slave Lake
The Cryosphere
genre_facet Great Bear Lake
Great Slave Lake
The Cryosphere
op_source The Cryosphere, Vol 12, Pp 2727-2740 (2018)
op_relation doi:10.5194/tc-12-2727-2018
1994-0416
1994-0424
https://www.the-cryosphere.net/12/2727/2018/tc-12-2727-2018.pdf
https://doaj.org/article/dd7d2d1708594a1588db8c38681a236f
op_rights undefined
op_doi https://doi.org/10.5194/tc-12-2727-2018
container_title The Cryosphere
container_volume 12
container_issue 8
container_start_page 2727
op_container_end_page 2740
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