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...
Published in: | Water |
---|---|
Main Authors: | , , , , , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2017
|
Subjects: | |
Online Access: | https://doi.org/10.3390/w9060418 |
_version_ | 1821823934397415424 |
---|---|
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. |
format | Text |
genre | Arctic permafrost Siberia |
genre_facet | Arctic permafrost Siberia |
geographic | Arctic Yenisei River |
geographic_facet | Arctic Yenisei River |
id | ftmdpi:oai:mdpi.com:/2073-4441/9/6/418/ |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(84.738,84.738,69.718,69.718) |
op_collection_id | ftmdpi |
op_coverage | agris |
op_doi | https://doi.org/10.3390/w9060418 |
op_relation | https://dx.doi.org/10.3390/w9060418 |
op_rights | https://creativecommons.org/licenses/by/4.0/ |
op_source | Water; Volume 9; Issue 6; Pages: 418 |
publishDate | 2017 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
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 |