Decadal predictability of river discharge with climate oscillations over the 20th and early 21st century

Long-term hydrological forecasts are important to increase our resilience and preparedness to extreme hydrological events. The skill in these forecasts is still limited due to large uncertainties inherent in hydrological models and poor predictability of long-term meteorological conditions. Here we...

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Bibliographic Details
Main Authors: Wanders, Niko, Wada, Yoshi
Other Authors: Landdegradatie en aardobservatie, Hydrologie, Landscape functioning, Geocomputation and Hydrology
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
AAO
NAO
PDO
Online Access:https://dspace.library.uu.nl/handle/1874/327832
id ftunivutrecht:oai:dspace.library.uu.nl:1874/327832
record_format openpolar
spelling ftunivutrecht:oai:dspace.library.uu.nl:1874/327832 2023-07-23T04:14:21+02:00 Decadal predictability of river discharge with climate oscillations over the 20th and early 21st century Wanders, Niko Wada, Yoshi Landdegradatie en aardobservatie Hydrologie Landscape functioning, Geocomputation and Hydrology 2015-12-28 image/pdf https://dspace.library.uu.nl/handle/1874/327832 en eng 0094-8276 https://dspace.library.uu.nl/handle/1874/327832 info:eu-repo/semantics/OpenAccess AAO climate oscillations discharge ENSO NAO PDO Earth and Planetary Sciences(all) Geophysics Article 2015 ftunivutrecht 2023-07-02T01:37:29Z Long-term hydrological forecasts are important to increase our resilience and preparedness to extreme hydrological events. The skill in these forecasts is still limited due to large uncertainties inherent in hydrological models and poor predictability of long-term meteorological conditions. Here we show that strong (lagged) correlations exist between four different major climate oscillation modes and modeled and observed discharge anomalies over a 100 year period. The strongest correlations are found between the El Niño-Southern Oscillation signal and river discharge anomalies all year round, while North Atlantic Oscillation and Antarctic Oscillation time series are strongly correlated with winter discharge anomalies. The correlation signal is significant for periods up to 5 years for some regions, indicating a high added value of this information for long-term hydrological forecasting. The results suggest that long-term hydrological forecasting could be significantly improved by including the climate oscillation signals and thus improve our preparedness for hydrological extremes in the near future. Article in Journal/Newspaper Antarc* Antarctic North Atlantic North Atlantic oscillation Utrecht University Repository Antarctic
institution Open Polar
collection Utrecht University Repository
op_collection_id ftunivutrecht
language English
topic AAO
climate oscillations
discharge
ENSO
NAO
PDO
Earth and Planetary Sciences(all)
Geophysics
spellingShingle AAO
climate oscillations
discharge
ENSO
NAO
PDO
Earth and Planetary Sciences(all)
Geophysics
Wanders, Niko
Wada, Yoshi
Decadal predictability of river discharge with climate oscillations over the 20th and early 21st century
topic_facet AAO
climate oscillations
discharge
ENSO
NAO
PDO
Earth and Planetary Sciences(all)
Geophysics
description Long-term hydrological forecasts are important to increase our resilience and preparedness to extreme hydrological events. The skill in these forecasts is still limited due to large uncertainties inherent in hydrological models and poor predictability of long-term meteorological conditions. Here we show that strong (lagged) correlations exist between four different major climate oscillation modes and modeled and observed discharge anomalies over a 100 year period. The strongest correlations are found between the El Niño-Southern Oscillation signal and river discharge anomalies all year round, while North Atlantic Oscillation and Antarctic Oscillation time series are strongly correlated with winter discharge anomalies. The correlation signal is significant for periods up to 5 years for some regions, indicating a high added value of this information for long-term hydrological forecasting. The results suggest that long-term hydrological forecasting could be significantly improved by including the climate oscillation signals and thus improve our preparedness for hydrological extremes in the near future.
author2 Landdegradatie en aardobservatie
Hydrologie
Landscape functioning, Geocomputation and Hydrology
format Article in Journal/Newspaper
author Wanders, Niko
Wada, Yoshi
author_facet Wanders, Niko
Wada, Yoshi
author_sort Wanders, Niko
title Decadal predictability of river discharge with climate oscillations over the 20th and early 21st century
title_short Decadal predictability of river discharge with climate oscillations over the 20th and early 21st century
title_full Decadal predictability of river discharge with climate oscillations over the 20th and early 21st century
title_fullStr Decadal predictability of river discharge with climate oscillations over the 20th and early 21st century
title_full_unstemmed Decadal predictability of river discharge with climate oscillations over the 20th and early 21st century
title_sort decadal predictability of river discharge with climate oscillations over the 20th and early 21st century
publishDate 2015
url https://dspace.library.uu.nl/handle/1874/327832
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
North Atlantic
North Atlantic oscillation
genre_facet Antarc*
Antarctic
North Atlantic
North Atlantic oscillation
op_relation 0094-8276
https://dspace.library.uu.nl/handle/1874/327832
op_rights info:eu-repo/semantics/OpenAccess
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