Using Modeling Tools to Better Understand Permafrost Hydrology

Modification of the hydrological cycle and, subsequently, of other global cycles is expected in Arctic watersheds owing to global change. Future climate scenarios imply widespread permafrost degradation caused by an increase in air temperature, and the expected effect on permafrost hydrology is imme...

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Published in:Water
Main Authors: Clément Fabre, Sabine Sauvage, Nikita Tananaev, Raghavan Srinivasan, Roman Teisserenc, José Sánchez Pérez
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2017
Subjects:
Online Access:https://doi.org/10.3390/w9060418
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author Clément Fabre
Sabine Sauvage
Nikita Tananaev
Raghavan Srinivasan
Roman Teisserenc
José Sánchez Pérez
author_facet Clément Fabre
Sabine Sauvage
Nikita Tananaev
Raghavan Srinivasan
Roman Teisserenc
José Sánchez Pérez
author_sort Clément Fabre
collection MDPI Open Access Publishing
container_issue 6
container_start_page 418
container_title Water
container_volume 9
description Modification of the hydrological cycle and, subsequently, of other global cycles is expected in Arctic watersheds owing to global change. Future climate scenarios imply widespread permafrost degradation caused by an increase in air temperature, and the expected effect on permafrost hydrology is immense. This study aims at analyzing, and quantifying the daily water transfer in the largest Arctic river system, the Yenisei River in central Siberia, Russia, partially underlain by permafrost. The semi-distributed SWAT (Soil and Water Assessment Tool) hydrological model has been calibrated and validated at a daily time step in historical discharge simulations for the 2003–2014 period. The model parameters have been adjusted to embrace the hydrological features of permafrost. SWAT is shown capable to estimate water fluxes at a daily time step, especially during unfrozen periods, once are considered specific climatic and soils conditions adapted to a permafrost watershed. The model simulates average annual contribution to runoff of 263 millimeters per year (mm yr−1) distributed as 152 mm yr−1 (58%) of surface runoff, 103 mm yr−1 (39%) of lateral flow and 8 mm yr−1 (3%) of return flow from the aquifer. These results are integrated on a reduced basin area downstream from large dams and are closer to observations than previous modeling exercises.
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genre Arctic
permafrost
Siberia
genre_facet Arctic
permafrost
Siberia
geographic Arctic
Yenisei River
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Yenisei River
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op_source Water; Volume 9; Issue 6; Pages: 418
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spelling ftmdpi:oai:mdpi.com:/2073-4441/9/6/418/ 2025-01-16T20:28:54+00:00 Using Modeling Tools to Better Understand Permafrost Hydrology Clément Fabre Sabine Sauvage Nikita Tananaev Raghavan Srinivasan Roman Teisserenc José Sánchez Pérez agris 2017-06-10 application/pdf https://doi.org/10.3390/w9060418 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/w9060418 https://creativecommons.org/licenses/by/4.0/ Water; Volume 9; Issue 6; Pages: 418 permafrost modeling hydrology water Yenisei River SWAT Text 2017 ftmdpi https://doi.org/10.3390/w9060418 2023-07-31T21:08:18Z Modification of the hydrological cycle and, subsequently, of other global cycles is expected in Arctic watersheds owing to global change. Future climate scenarios imply widespread permafrost degradation caused by an increase in air temperature, and the expected effect on permafrost hydrology is immense. This study aims at analyzing, and quantifying the daily water transfer in the largest Arctic river system, the Yenisei River in central Siberia, Russia, partially underlain by permafrost. The semi-distributed SWAT (Soil and Water Assessment Tool) hydrological model has been calibrated and validated at a daily time step in historical discharge simulations for the 2003–2014 period. The model parameters have been adjusted to embrace the hydrological features of permafrost. SWAT is shown capable to estimate water fluxes at a daily time step, especially during unfrozen periods, once are considered specific climatic and soils conditions adapted to a permafrost watershed. The model simulates average annual contribution to runoff of 263 millimeters per year (mm yr−1) distributed as 152 mm yr−1 (58%) of surface runoff, 103 mm yr−1 (39%) of lateral flow and 8 mm yr−1 (3%) of return flow from the aquifer. These results are integrated on a reduced basin area downstream from large dams and are closer to observations than previous modeling exercises. Text Arctic permafrost Siberia MDPI Open Access Publishing Arctic Yenisei River ENVELOPE(84.738,84.738,69.718,69.718) Water 9 6 418
spellingShingle permafrost
modeling
hydrology
water
Yenisei River
SWAT
Clément Fabre
Sabine Sauvage
Nikita Tananaev
Raghavan Srinivasan
Roman Teisserenc
José Sánchez Pérez
Using Modeling Tools to Better Understand Permafrost Hydrology
title Using Modeling Tools to Better Understand Permafrost Hydrology
title_full Using Modeling Tools to Better Understand Permafrost Hydrology
title_fullStr Using Modeling Tools to Better Understand Permafrost Hydrology
title_full_unstemmed Using Modeling Tools to Better Understand Permafrost Hydrology
title_short Using Modeling Tools to Better Understand Permafrost Hydrology
title_sort using modeling tools to better understand permafrost hydrology
topic permafrost
modeling
hydrology
water
Yenisei River
SWAT
topic_facet permafrost
modeling
hydrology
water
Yenisei River
SWAT
url https://doi.org/10.3390/w9060418