Physically-based distributed modelling of river runoff under changing climate conditions

Physically-based distributed modelling under changing climatic conditions has been carried out for the Northern Dvina River basin using the ECOMAG (ECOlogical Model for Applied Geophysics). The parameters of the model have been adjusted through calibration against runoff hydrographs observed for the...

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Published in:Proceedings of the International Association of Hydrological Sciences
Main Authors: Krylenko, I., Motovilov, Yu., Antokhina, E., Zhuk, V., Surkova, G.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2015
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Online Access:https://doi.org/10.5194/piahs-368-156-2015
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00016625 2023-05-15T16:02:56+02:00 Physically-based distributed modelling of river runoff under changing climate conditions Krylenko, I. Motovilov, Yu. Antokhina, E. Zhuk, V. Surkova, G. 2015-05 electronic https://doi.org/10.5194/piahs-368-156-2015 https://noa.gwlb.de/receive/cop_mods_00016625 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00016580/piahs-368-156-2015.pdf https://piahs.copernicus.org/articles/368/156/2015/piahs-368-156-2015.pdf eng eng Copernicus Publications Proceedings of the International Association of Hydrological Sciences -- https://www.proc-iahs.net/volumes.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2827925 -- 2199-899X https://doi.org/10.5194/piahs-368-156-2015 https://noa.gwlb.de/receive/cop_mods_00016625 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00016580/piahs-368-156-2015.pdf https://piahs.copernicus.org/articles/368/156/2015/piahs-368-156-2015.pdf uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2015 ftnonlinearchiv https://doi.org/10.5194/piahs-368-156-2015 2022-02-08T22:54:04Z Physically-based distributed modelling under changing climatic conditions has been carried out for the Northern Dvina River basin using the ECOMAG (ECOlogical Model for Applied Geophysics). The parameters of the model have been adjusted through calibration against runoff hydrographs observed for the period 2000–2009. Validation of the model has been performed for the period of 1970–1989. Both sensitivity analysis and scenario approaches (based on the CMIP3 projections) have been applied to assess possible hydrological consequences of climate change in the basin. It has been shown that for greenhouse gases emissions A2 scenario, averaged for 11 climate models, annual runoff will not change significantly for the future 50 years. But due to increasing of winter precipitation by up to 15%, the volume of flow in the flood period could increase by up to 20%. Earlier beginning of the flood season is expected because of rising of the air temperature. Article in Journal/Newspaper dvina Niedersächsisches Online-Archiv NOA Proceedings of the International Association of Hydrological Sciences 368 156 161
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Krylenko, I.
Motovilov, Yu.
Antokhina, E.
Zhuk, V.
Surkova, G.
Physically-based distributed modelling of river runoff under changing climate conditions
topic_facet article
Verlagsveröffentlichung
description Physically-based distributed modelling under changing climatic conditions has been carried out for the Northern Dvina River basin using the ECOMAG (ECOlogical Model for Applied Geophysics). The parameters of the model have been adjusted through calibration against runoff hydrographs observed for the period 2000–2009. Validation of the model has been performed for the period of 1970–1989. Both sensitivity analysis and scenario approaches (based on the CMIP3 projections) have been applied to assess possible hydrological consequences of climate change in the basin. It has been shown that for greenhouse gases emissions A2 scenario, averaged for 11 climate models, annual runoff will not change significantly for the future 50 years. But due to increasing of winter precipitation by up to 15%, the volume of flow in the flood period could increase by up to 20%. Earlier beginning of the flood season is expected because of rising of the air temperature.
format Article in Journal/Newspaper
author Krylenko, I.
Motovilov, Yu.
Antokhina, E.
Zhuk, V.
Surkova, G.
author_facet Krylenko, I.
Motovilov, Yu.
Antokhina, E.
Zhuk, V.
Surkova, G.
author_sort Krylenko, I.
title Physically-based distributed modelling of river runoff under changing climate conditions
title_short Physically-based distributed modelling of river runoff under changing climate conditions
title_full Physically-based distributed modelling of river runoff under changing climate conditions
title_fullStr Physically-based distributed modelling of river runoff under changing climate conditions
title_full_unstemmed Physically-based distributed modelling of river runoff under changing climate conditions
title_sort physically-based distributed modelling of river runoff under changing climate conditions
publisher Copernicus Publications
publishDate 2015
url https://doi.org/10.5194/piahs-368-156-2015
https://noa.gwlb.de/receive/cop_mods_00016625
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00016580/piahs-368-156-2015.pdf
https://piahs.copernicus.org/articles/368/156/2015/piahs-368-156-2015.pdf
genre dvina
genre_facet dvina
op_relation Proceedings of the International Association of Hydrological Sciences -- https://www.proc-iahs.net/volumes.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2827925 -- 2199-899X
https://doi.org/10.5194/piahs-368-156-2015
https://noa.gwlb.de/receive/cop_mods_00016625
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00016580/piahs-368-156-2015.pdf
https://piahs.copernicus.org/articles/368/156/2015/piahs-368-156-2015.pdf
op_rights uneingeschränkt
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/piahs-368-156-2015
container_title Proceedings of the International Association of Hydrological Sciences
container_volume 368
container_start_page 156
op_container_end_page 161
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