The spatio-temporal influence of atmospheric teleconnection patterns on hydrology in Sweden

Study region: Sixty-four river gauging stations distributed over Sweden. Study focus: To investigate the influence of climate teleconnection patterns (TP) on streamflow in Sweden. Streamflow data is regionalized and the average hydrographs of each homogeneous region is divided into hydrological seas...

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Main Authors: Cintia B. Uvo, Kean Foster, Jonas Olsson
Format: Article
Language:English
Published: Elsevier 2021-04-01
Series:Journal of Hydrology: Regional Studies
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2214581821000112
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spelling doaj-e83abf153b1b4968b1553a0df25f6fe22021-03-27T04:27:33ZengElsevierJournal of Hydrology: Regional Studies2214-58182021-04-0134100782The spatio-temporal influence of atmospheric teleconnection patterns on hydrology in SwedenCintia B. Uvo0Kean Foster1Jonas Olsson2Lund University, Box 118, SE-221 00, Lund, Sweden; Corresponding author.Lund University, Box 118, SE-221 00, Lund, Sweden; Swedish Meteorological and Hydrological Institute, 601 76, Norrköping, SwedenSwedish Meteorological and Hydrological Institute, 601 76, Norrköping, SwedenStudy region: Sixty-four river gauging stations distributed over Sweden. Study focus: To investigate the influence of climate teleconnection patterns (TP) on streamflow in Sweden. Streamflow data is regionalized and the average hydrographs of each homogeneous region is divided into hydrological seasons. Thereafter the impact of different TPs on the streamflow, per homogeneous region and per hydrological season is analyzed. New hydrological insights for the region: Five homogeneous regions are identified; three located in the north, where snow dominates the hydrological processes, and two located in the south, where rain dominates hydrological processes. The northern hydrographs are separated into three hydrological periods: low streamflow when snow is accumulated, high streamflow during the melting of the snowpack and a transition period in between. The southern hydrographs are characterized by streamflow above the yearly average during the winter and below during the summer. Hydrological periods in different homogeneous regions are influenced by diverse combinations of TPs. Arctic Oscillation, North Atlantic Oscillation and Scandinavian Pattern influence the streamflow in most of the regions during most hydrological periods. The further south and east the region is located, the more TPs influence the streamflow. The resulting streamflow variability is related to the interplay between different TPs both before and during each hydrological period. This interplay may enhance or decrease the individual influence of each TP on streamflow.http://www.sciencedirect.com/science/article/pii/S2214581821000112Climate variabilityTeleconnections patternsHydrological variabilityStreamflowClimateWavelet analysis
collection DOAJ
language English
format Article
sources DOAJ
author Cintia B. Uvo
Kean Foster
Jonas Olsson
spellingShingle Cintia B. Uvo
Kean Foster
Jonas Olsson
The spatio-temporal influence of atmospheric teleconnection patterns on hydrology in Sweden
Journal of Hydrology: Regional Studies
Climate variability
Teleconnections patterns
Hydrological variability
Streamflow
Climate
Wavelet analysis
author_facet Cintia B. Uvo
Kean Foster
Jonas Olsson
author_sort Cintia B. Uvo
title The spatio-temporal influence of atmospheric teleconnection patterns on hydrology in Sweden
title_short The spatio-temporal influence of atmospheric teleconnection patterns on hydrology in Sweden
title_full The spatio-temporal influence of atmospheric teleconnection patterns on hydrology in Sweden
title_fullStr The spatio-temporal influence of atmospheric teleconnection patterns on hydrology in Sweden
title_full_unstemmed The spatio-temporal influence of atmospheric teleconnection patterns on hydrology in Sweden
title_sort spatio-temporal influence of atmospheric teleconnection patterns on hydrology in sweden
publisher Elsevier
series Journal of Hydrology: Regional Studies
issn 2214-5818
publishDate 2021-04-01
description Study region: Sixty-four river gauging stations distributed over Sweden. Study focus: To investigate the influence of climate teleconnection patterns (TP) on streamflow in Sweden. Streamflow data is regionalized and the average hydrographs of each homogeneous region is divided into hydrological seasons. Thereafter the impact of different TPs on the streamflow, per homogeneous region and per hydrological season is analyzed. New hydrological insights for the region: Five homogeneous regions are identified; three located in the north, where snow dominates the hydrological processes, and two located in the south, where rain dominates hydrological processes. The northern hydrographs are separated into three hydrological periods: low streamflow when snow is accumulated, high streamflow during the melting of the snowpack and a transition period in between. The southern hydrographs are characterized by streamflow above the yearly average during the winter and below during the summer. Hydrological periods in different homogeneous regions are influenced by diverse combinations of TPs. Arctic Oscillation, North Atlantic Oscillation and Scandinavian Pattern influence the streamflow in most of the regions during most hydrological periods. The further south and east the region is located, the more TPs influence the streamflow. The resulting streamflow variability is related to the interplay between different TPs both before and during each hydrological period. This interplay may enhance or decrease the individual influence of each TP on streamflow.
topic Climate variability
Teleconnections patterns
Hydrological variability
Streamflow
Climate
Wavelet analysis
url http://www.sciencedirect.com/science/article/pii/S2214581821000112
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