Effects of precipitation uncertainty on discharge calculations for main river basins

This study quantifies the uncertainty in discharge calculations caused by uncertainty in precipitation input for 294 river basins worldwide. Seven global gridded precipitation datasets are compared at river basin scale in terms of mean annual and seasonal precipitation. The representation of seasona...

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Published in:Journal of Hydrometeorology
Main Authors: Biemans, H., Hutjes, R.W.A., Kabat, P., Gerten, D., Rost, S.
Format: Article in Journal/Newspaper
Language:English
Published: 2009
Subjects:
Online Access:https://research.wur.nl/en/publications/effects-of-precipitation-uncertainty-on-discharge-calculations-fo
https://doi.org/10.1175/2008JHM1067.1
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spelling ftunivwagenin:oai:library.wur.nl:wurpubs/370916 2024-01-21T10:03:51+01:00 Effects of precipitation uncertainty on discharge calculations for main river basins Biemans, H. Hutjes, R.W.A. Kabat, P. Gerten, D. Rost, S. 2009 application/pdf https://research.wur.nl/en/publications/effects-of-precipitation-uncertainty-on-discharge-calculations-fo https://doi.org/10.1175/2008JHM1067.1 en eng https://edepot.wur.nl/11966 https://research.wur.nl/en/publications/effects-of-precipitation-uncertainty-on-discharge-calculations-fo doi:10.1175/2008JHM1067.1 info:eu-repo/semantics/openAccess Wageningen University & Research Journal of Hydrometeorology 10 (2009) 4 ISSN: 1525-755X availability balance global water-resources impacts runoff space-time climate streamflow validation variability vegetation model info:eu-repo/semantics/article Article/Letter to editor info:eu-repo/semantics/publishedVersion 2009 ftunivwagenin https://doi.org/10.1175/2008JHM1067.1 2023-12-27T23:15:32Z This study quantifies the uncertainty in discharge calculations caused by uncertainty in precipitation input for 294 river basins worldwide. Seven global gridded precipitation datasets are compared at river basin scale in terms of mean annual and seasonal precipitation. The representation of seasonality is similar in all datasets, but the uncertainty in mean annual precipitation is large, especially in mountainous, arctic, and small basins. The average precipitation uncertainty in a basin is 30%, but there are strong differences between basins. The effect of this precipitation uncertainty on mean annual and seasonal discharge was assessed using the uncalibrated dynamic global vegetation and hydrology model Lund-Potsdam-Jena managed land (LPJmL), yielding even larger uncertainties in discharge (average 90%). For 95 basins (out of 213 basins for which measurements were available) calibration of model parameters is problematic because the observed discharge falls within the uncertainty of the simulated discharge. A method is presented to account for precipitation uncertainty in discharge simulations. Article in Journal/Newspaper Arctic Wageningen UR (University & Research Centre): Digital Library Arctic Journal of Hydrometeorology 10 4 1011 1025
institution Open Polar
collection Wageningen UR (University & Research Centre): Digital Library
op_collection_id ftunivwagenin
language English
topic availability
balance
global water-resources
impacts
runoff
space-time climate
streamflow
validation
variability
vegetation model
spellingShingle availability
balance
global water-resources
impacts
runoff
space-time climate
streamflow
validation
variability
vegetation model
Biemans, H.
Hutjes, R.W.A.
Kabat, P.
Gerten, D.
Rost, S.
Effects of precipitation uncertainty on discharge calculations for main river basins
topic_facet availability
balance
global water-resources
impacts
runoff
space-time climate
streamflow
validation
variability
vegetation model
description This study quantifies the uncertainty in discharge calculations caused by uncertainty in precipitation input for 294 river basins worldwide. Seven global gridded precipitation datasets are compared at river basin scale in terms of mean annual and seasonal precipitation. The representation of seasonality is similar in all datasets, but the uncertainty in mean annual precipitation is large, especially in mountainous, arctic, and small basins. The average precipitation uncertainty in a basin is 30%, but there are strong differences between basins. The effect of this precipitation uncertainty on mean annual and seasonal discharge was assessed using the uncalibrated dynamic global vegetation and hydrology model Lund-Potsdam-Jena managed land (LPJmL), yielding even larger uncertainties in discharge (average 90%). For 95 basins (out of 213 basins for which measurements were available) calibration of model parameters is problematic because the observed discharge falls within the uncertainty of the simulated discharge. A method is presented to account for precipitation uncertainty in discharge simulations.
format Article in Journal/Newspaper
author Biemans, H.
Hutjes, R.W.A.
Kabat, P.
Gerten, D.
Rost, S.
author_facet Biemans, H.
Hutjes, R.W.A.
Kabat, P.
Gerten, D.
Rost, S.
author_sort Biemans, H.
title Effects of precipitation uncertainty on discharge calculations for main river basins
title_short Effects of precipitation uncertainty on discharge calculations for main river basins
title_full Effects of precipitation uncertainty on discharge calculations for main river basins
title_fullStr Effects of precipitation uncertainty on discharge calculations for main river basins
title_full_unstemmed Effects of precipitation uncertainty on discharge calculations for main river basins
title_sort effects of precipitation uncertainty on discharge calculations for main river basins
publishDate 2009
url https://research.wur.nl/en/publications/effects-of-precipitation-uncertainty-on-discharge-calculations-fo
https://doi.org/10.1175/2008JHM1067.1
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Journal of Hydrometeorology 10 (2009) 4
ISSN: 1525-755X
op_relation https://edepot.wur.nl/11966
https://research.wur.nl/en/publications/effects-of-precipitation-uncertainty-on-discharge-calculations-fo
doi:10.1175/2008JHM1067.1
op_rights info:eu-repo/semantics/openAccess
Wageningen University & Research
op_doi https://doi.org/10.1175/2008JHM1067.1
container_title Journal of Hydrometeorology
container_volume 10
container_issue 4
container_start_page 1011
op_container_end_page 1025
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