Detection of global runoff changes: results from observations and CMIP5 experiments

This paper assesses the detectability of changes in global streamflow. First, a statistical detection method is applied to observed (no missing data which represent 42% of global discharge) and reconstructed (gaps are filled in order to cover a larger area and about 60% of global discharge) streamfl...

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Main Authors: R. Alkama, L. Marchand, A. Ribes, B. Decharme
Format: Article
Language:English
Published: Copernicus Publications 2013-07-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/17/2967/2013/hess-17-2967-2013.pdf
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spelling doaj-4a2de624414142b7830635bc0be6a5b32020-11-24T22:15:07ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382013-07-011772967297910.5194/hess-17-2967-2013Detection of global runoff changes: results from observations and CMIP5 experimentsR. AlkamaL. MarchandA. RibesB. DecharmeThis paper assesses the detectability of changes in global streamflow. First, a statistical detection method is applied to observed (no missing data which represent 42% of global discharge) and reconstructed (gaps are filled in order to cover a larger area and about 60% of global discharge) streamflow. Observations show no change over the 1958–1992 period. Further, an extension to 2004 over the same catchment areas using reconstructed data does not provide evidence of a significant change. Conversely, a significant change is found in reconstructed streamflow when a larger area is considered. These results suggest that changes in global streamflow are still unclear. Moreover, changes in streamflow as simulated by models from Coupled Model Intercomparison Project 5 (CMIP5) using the historic and future RCP 8.5 scenarios are investigated. Most CMIP5 models are found to simulate the climatological streamflow reasonably well, except for over South America and Africa. Change becomes significant between 2016 and 2040 for all but three models.http://www.hydrol-earth-syst-sci.net/17/2967/2013/hess-17-2967-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author R. Alkama
L. Marchand
A. Ribes
B. Decharme
spellingShingle R. Alkama
L. Marchand
A. Ribes
B. Decharme
Detection of global runoff changes: results from observations and CMIP5 experiments
Hydrology and Earth System Sciences
author_facet R. Alkama
L. Marchand
A. Ribes
B. Decharme
author_sort R. Alkama
title Detection of global runoff changes: results from observations and CMIP5 experiments
title_short Detection of global runoff changes: results from observations and CMIP5 experiments
title_full Detection of global runoff changes: results from observations and CMIP5 experiments
title_fullStr Detection of global runoff changes: results from observations and CMIP5 experiments
title_full_unstemmed Detection of global runoff changes: results from observations and CMIP5 experiments
title_sort detection of global runoff changes: results from observations and cmip5 experiments
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2013-07-01
description This paper assesses the detectability of changes in global streamflow. First, a statistical detection method is applied to observed (no missing data which represent 42% of global discharge) and reconstructed (gaps are filled in order to cover a larger area and about 60% of global discharge) streamflow. Observations show no change over the 1958–1992 period. Further, an extension to 2004 over the same catchment areas using reconstructed data does not provide evidence of a significant change. Conversely, a significant change is found in reconstructed streamflow when a larger area is considered. These results suggest that changes in global streamflow are still unclear. Moreover, changes in streamflow as simulated by models from Coupled Model Intercomparison Project 5 (CMIP5) using the historic and future RCP 8.5 scenarios are investigated. Most CMIP5 models are found to simulate the climatological streamflow reasonably well, except for over South America and Africa. Change becomes significant between 2016 and 2040 for all but three models.
url http://www.hydrol-earth-syst-sci.net/17/2967/2013/hess-17-2967-2013.pdf
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AT lmarchand detectionofglobalrunoffchangesresultsfromobservationsandcmip5experiments
AT aribes detectionofglobalrunoffchangesresultsfromobservationsandcmip5experiments
AT bdecharme detectionofglobalrunoffchangesresultsfromobservationsandcmip5experiments
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