Simulation of Active Layer Dynamics, Upper Kolyma, Russia, using the Hydrograph Hydrological Model

ABSTRACT Freeze/thaw simulations were performed for seven permafrost sites at the Kolyma Water Balance Station (KWBS), northeast Russia, using the hydrological model Hydrograph equipped with a heat transfer analytical solution that accounts for soil profile phase changes. The study sites include slo...

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Published in:Permafrost and Periglacial Processes
Main Authors: Lebedeva, Liudmila, Semenova, Olga, Vinogradova, Tatyana
Other Authors: Russian Foundation for Basic Research, Russian-German Otto-Schmidt Laboratory
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2014
Subjects:
Online Access:http://dx.doi.org/10.1002/ppp.1821
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.1821
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.1821
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spelling crwiley:10.1002/ppp.1821 2024-09-15T17:34:55+00:00 Simulation of Active Layer Dynamics, Upper Kolyma, Russia, using the Hydrograph Hydrological Model Lebedeva, Liudmila Semenova, Olga Vinogradova, Tatyana Russian Foundation for Basic Research Russian-German Otto-Schmidt Laboratory 2014 http://dx.doi.org/10.1002/ppp.1821 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.1821 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.1821 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 25, issue 4, page 270-280 ISSN 1045-6740 1099-1530 journal-article 2014 crwiley https://doi.org/10.1002/ppp.1821 2024-08-09T04:20:57Z ABSTRACT Freeze/thaw simulations were performed for seven permafrost sites at the Kolyma Water Balance Station (KWBS), northeast Russia, using the hydrological model Hydrograph equipped with a heat transfer analytical solution that accounts for soil profile phase changes. The study sites include slopes and plateaus with thaw depths of 0.5 to 1.8 m. Landscape conditions are characterised as rocky talus, mountain tundra with dwarf tree brush, moss‐lichen cover and sparse‐growth forest or larch forest. Soil horizons are distinguished as moss‐lichen cover, peat layer, clay with a high stone content and weathered clayey shale. Schematisation of soil‐vegetation profiles and model parameters were developed for each landscape. Parameterised model output was verified using time series of observed active layer thickness for the period of 1950 to 1990. The simulated values agree well with the observed values at the study sites. The results suggest that the soil profile schematisation and model parameters, along with the proposed algorithm of heat transfer, effectively simulate active layer dynamics under various landscape conditions at the KWBS and are suitable for hydrological modelling in the permafrost zone. The modelling efforts and results are highly relevant because the natural conditions at the KWBS are representative of large areas of northeastern Russia. Copyright © 2014 John Wiley & Sons, Ltd. Article in Journal/Newspaper Active layer thickness Peat permafrost Permafrost and Periglacial Processes Tundra Wiley Online Library Permafrost and Periglacial Processes 25 4 270 280
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description ABSTRACT Freeze/thaw simulations were performed for seven permafrost sites at the Kolyma Water Balance Station (KWBS), northeast Russia, using the hydrological model Hydrograph equipped with a heat transfer analytical solution that accounts for soil profile phase changes. The study sites include slopes and plateaus with thaw depths of 0.5 to 1.8 m. Landscape conditions are characterised as rocky talus, mountain tundra with dwarf tree brush, moss‐lichen cover and sparse‐growth forest or larch forest. Soil horizons are distinguished as moss‐lichen cover, peat layer, clay with a high stone content and weathered clayey shale. Schematisation of soil‐vegetation profiles and model parameters were developed for each landscape. Parameterised model output was verified using time series of observed active layer thickness for the period of 1950 to 1990. The simulated values agree well with the observed values at the study sites. The results suggest that the soil profile schematisation and model parameters, along with the proposed algorithm of heat transfer, effectively simulate active layer dynamics under various landscape conditions at the KWBS and are suitable for hydrological modelling in the permafrost zone. The modelling efforts and results are highly relevant because the natural conditions at the KWBS are representative of large areas of northeastern Russia. Copyright © 2014 John Wiley & Sons, Ltd.
author2 Russian Foundation for Basic Research
Russian-German Otto-Schmidt Laboratory
format Article in Journal/Newspaper
author Lebedeva, Liudmila
Semenova, Olga
Vinogradova, Tatyana
spellingShingle Lebedeva, Liudmila
Semenova, Olga
Vinogradova, Tatyana
Simulation of Active Layer Dynamics, Upper Kolyma, Russia, using the Hydrograph Hydrological Model
author_facet Lebedeva, Liudmila
Semenova, Olga
Vinogradova, Tatyana
author_sort Lebedeva, Liudmila
title Simulation of Active Layer Dynamics, Upper Kolyma, Russia, using the Hydrograph Hydrological Model
title_short Simulation of Active Layer Dynamics, Upper Kolyma, Russia, using the Hydrograph Hydrological Model
title_full Simulation of Active Layer Dynamics, Upper Kolyma, Russia, using the Hydrograph Hydrological Model
title_fullStr Simulation of Active Layer Dynamics, Upper Kolyma, Russia, using the Hydrograph Hydrological Model
title_full_unstemmed Simulation of Active Layer Dynamics, Upper Kolyma, Russia, using the Hydrograph Hydrological Model
title_sort simulation of active layer dynamics, upper kolyma, russia, using the hydrograph hydrological model
publisher Wiley
publishDate 2014
url http://dx.doi.org/10.1002/ppp.1821
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.1821
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.1821
genre Active layer thickness
Peat
permafrost
Permafrost and Periglacial Processes
Tundra
genre_facet Active layer thickness
Peat
permafrost
Permafrost and Periglacial Processes
Tundra
op_source Permafrost and Periglacial Processes
volume 25, issue 4, page 270-280
ISSN 1045-6740 1099-1530
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/ppp.1821
container_title Permafrost and Periglacial Processes
container_volume 25
container_issue 4
container_start_page 270
op_container_end_page 280
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