ENSO impact on simulated South American hydro-climatology
The variability of the simulated hydro-climatology of the WaterGAP Global Hydrology Model (WGHM) is analysed. Main object of this study is the ENSO-driven variability of the water storage of South America. The horizontal model resolution amounts to 0.5 degree and it is forced with monthly climate va...
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Copernicus Publications
2006
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00033540 2023-05-15T18:18:43+02:00 ENSO impact on simulated South American hydro-climatology Stuck, J. Güntner, A. Merz, B. 2006-02 electronic https://doi.org/10.5194/adgeo-6-227-2006 https://noa.gwlb.de/receive/cop_mods_00033540 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00033494/adgeo-6-227-2006.pdf https://adgeo.copernicus.org/articles/6/227/2006/adgeo-6-227-2006.pdf eng eng Copernicus Publications Advances in Geosciences -- http://www.bibliothek.uni-regensburg.de/ezeit/?2625759 -- http://www.adv-geosci.net/volumes.html -- 1680-7359 https://doi.org/10.5194/adgeo-6-227-2006 https://noa.gwlb.de/receive/cop_mods_00033540 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00033494/adgeo-6-227-2006.pdf https://adgeo.copernicus.org/articles/6/227/2006/adgeo-6-227-2006.pdf https://open-access.net/ uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2006 ftnonlinearchiv https://doi.org/10.5194/adgeo-6-227-2006 2022-02-08T22:45:42Z The variability of the simulated hydro-climatology of the WaterGAP Global Hydrology Model (WGHM) is analysed. Main object of this study is the ENSO-driven variability of the water storage of South America. The horizontal model resolution amounts to 0.5 degree and it is forced with monthly climate variables for 1961-1995 of the Tyndall Centre Climate Research Unit dataset (CRU TS 2.0) as a representation of the observed climate state. Secondly, the model is also forced by the model output of a global circulation model, the ECHAM4-T42 GCM. This model itself is driven by observed monthly means of the global Sea Surface Temperatures (SST) and the sea ice coverage for the period of 1903 to 1994 (GISST). Thus, the climate model and the hydrological model represent a realistic simulated realisation of the hydro-climatologic state of the last century. Since four simulations of the ECHAM4 model with the same forcing, but with different initial conditions are carried out, an analysis of variance (ANOVA) gives an impression of the impact of the varying SST on the hydro-climatology, because the variance can be separated into a SST-explained and a model internal variability (noise). Also regional multivariate analyses, like Empirical Orthogonal Functions (EOF) and Canonical Correlation Analysis (CCA) provide information of the complex time-space variability. In particular the Amazon region and the South of Brazil are significantly influenced by the ENSO-variability, but also the Pacific coastal areas of Ecuador and Peru are affected. Additionally, different ENSO-indices, based on SST anomalies (e.g. NINO3.4, NINO1+2), and its influence on the South American hydro-climatology are analysed. Especially, the Pacific coast regions of Ecuador, Peru and Chile show a very different behaviour dependant on those indices. Article in Journal/Newspaper Sea ice Niedersächsisches Online-Archiv NOA Pacific Advances in Geosciences 6 227 236 |
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article Verlagsveröffentlichung |
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article Verlagsveröffentlichung Stuck, J. Güntner, A. Merz, B. ENSO impact on simulated South American hydro-climatology |
topic_facet |
article Verlagsveröffentlichung |
description |
The variability of the simulated hydro-climatology of the WaterGAP Global Hydrology Model (WGHM) is analysed. Main object of this study is the ENSO-driven variability of the water storage of South America. The horizontal model resolution amounts to 0.5 degree and it is forced with monthly climate variables for 1961-1995 of the Tyndall Centre Climate Research Unit dataset (CRU TS 2.0) as a representation of the observed climate state. Secondly, the model is also forced by the model output of a global circulation model, the ECHAM4-T42 GCM. This model itself is driven by observed monthly means of the global Sea Surface Temperatures (SST) and the sea ice coverage for the period of 1903 to 1994 (GISST). Thus, the climate model and the hydrological model represent a realistic simulated realisation of the hydro-climatologic state of the last century. Since four simulations of the ECHAM4 model with the same forcing, but with different initial conditions are carried out, an analysis of variance (ANOVA) gives an impression of the impact of the varying SST on the hydro-climatology, because the variance can be separated into a SST-explained and a model internal variability (noise). Also regional multivariate analyses, like Empirical Orthogonal Functions (EOF) and Canonical Correlation Analysis (CCA) provide information of the complex time-space variability. In particular the Amazon region and the South of Brazil are significantly influenced by the ENSO-variability, but also the Pacific coastal areas of Ecuador and Peru are affected. Additionally, different ENSO-indices, based on SST anomalies (e.g. NINO3.4, NINO1+2), and its influence on the South American hydro-climatology are analysed. Especially, the Pacific coast regions of Ecuador, Peru and Chile show a very different behaviour dependant on those indices. |
format |
Article in Journal/Newspaper |
author |
Stuck, J. Güntner, A. Merz, B. |
author_facet |
Stuck, J. Güntner, A. Merz, B. |
author_sort |
Stuck, J. |
title |
ENSO impact on simulated South American hydro-climatology |
title_short |
ENSO impact on simulated South American hydro-climatology |
title_full |
ENSO impact on simulated South American hydro-climatology |
title_fullStr |
ENSO impact on simulated South American hydro-climatology |
title_full_unstemmed |
ENSO impact on simulated South American hydro-climatology |
title_sort |
enso impact on simulated south american hydro-climatology |
publisher |
Copernicus Publications |
publishDate |
2006 |
url |
https://doi.org/10.5194/adgeo-6-227-2006 https://noa.gwlb.de/receive/cop_mods_00033540 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00033494/adgeo-6-227-2006.pdf https://adgeo.copernicus.org/articles/6/227/2006/adgeo-6-227-2006.pdf |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Sea ice |
genre_facet |
Sea ice |
op_relation |
Advances in Geosciences -- http://www.bibliothek.uni-regensburg.de/ezeit/?2625759 -- http://www.adv-geosci.net/volumes.html -- 1680-7359 https://doi.org/10.5194/adgeo-6-227-2006 https://noa.gwlb.de/receive/cop_mods_00033540 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00033494/adgeo-6-227-2006.pdf https://adgeo.copernicus.org/articles/6/227/2006/adgeo-6-227-2006.pdf |
op_rights |
https://open-access.net/ uneingeschränkt info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/adgeo-6-227-2006 |
container_title |
Advances in Geosciences |
container_volume |
6 |
container_start_page |
227 |
op_container_end_page |
236 |
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1766195377217732608 |