Finding the Optimal Multimodel Averaging Method for Global Hydrological Simulations

Global gridded precipitations have been extensively considered as the input of hydrological models for runoff simulations around the world. However, the limitations of hydrologic models and the inaccuracies of the precipitation datasets could result in large uncertainty in hydrological forecasts and...

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Main Authors: Wenyan Qi, Jie Chen, Chongyu Xu, Yongjing Wan
Format: Article
Language:English
Published: MDPI AG 2021-07-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/13/13/2574
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author Wenyan Qi
Jie Chen
Chongyu Xu
Yongjing Wan
author_facet Wenyan Qi
Jie Chen
Chongyu Xu
Yongjing Wan
author_sort Wenyan Qi
collection DOAJ
description Global gridded precipitations have been extensively considered as the input of hydrological models for runoff simulations around the world. However, the limitations of hydrologic models and the inaccuracies of the precipitation datasets could result in large uncertainty in hydrological forecasts and water resource estimations. Therefore, it is of great importance to investigate the hydrological value of a weighted combination of hydrological models driven by different precipitation datasets. In addition, due to the diversities of combination members and climate conditions, hydrological simulation for watersheds under different climate conditions may show various sensitivities to the weighted combinations. This study undertakes a comprehensive analysis of various multimodel averaging methods and schemes (i.e., the combination of the members in averaging) to identify the most skillful and reliable multimodel averaging application. To achieve this, four hydrological models driven by six precipitation datasets were used as averaging members. The behaviors of 9 averaging methods and 11 averaging schemes in hydrological simulations were tested over 2277 watersheds distributed in different climate regions in the world. The results show the following: (1) The multi-input averaging schemes (i.e., members consist of one model driven by multiple precipitation datasets) generally perform better than the multimodel averaging schemes (i.e., members consist of multiple models driven by the same precipitation dataset) for each averaging method; (2) The use of multiple members can improve the averaging performances. Six averaging members are found to be necessary and advisable, since using more than six members only imrpoves the estimation results slightly, as compared with using all 24 members; (3) The advantage of using averaging methods for hydrological modeling is region dependent. The averaging methods, in general, produced the best results in the warm temperate region, followed by the snow and equatorial regions, while a large difference among various averaging methods is found in arid and arctic regions. This is mainly due to the different averaging methods being affected to a different extent by the poorly performed members in the arid and arctic regions; (4) the multimodel superensemble method (MMSE) is recommended for its robust and outstanding performance among various climatic regions.
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spelling doaj.art-b3e923cd662f472bb9d4ca96d4ffc6b12023-11-22T02:49:14ZengMDPI AGRemote Sensing2072-42922021-07-011313257410.3390/rs13132574Finding the Optimal Multimodel Averaging Method for Global Hydrological SimulationsWenyan Qi0Jie Chen1Chongyu Xu2Yongjing Wan3State Key Laboratory of Water Resources & Hydropower Engineering Science, Wuhan University, Wuhan 430072, ChinaState Key Laboratory of Water Resources & Hydropower Engineering Science, Wuhan University, Wuhan 430072, ChinaDepartment of Geosciences, University of Oslo, 0316 Oslo, NorwayState Key Laboratory of Water Resources & Hydropower Engineering Science, Wuhan University, Wuhan 430072, ChinaGlobal gridded precipitations have been extensively considered as the input of hydrological models for runoff simulations around the world. However, the limitations of hydrologic models and the inaccuracies of the precipitation datasets could result in large uncertainty in hydrological forecasts and water resource estimations. Therefore, it is of great importance to investigate the hydrological value of a weighted combination of hydrological models driven by different precipitation datasets. In addition, due to the diversities of combination members and climate conditions, hydrological simulation for watersheds under different climate conditions may show various sensitivities to the weighted combinations. This study undertakes a comprehensive analysis of various multimodel averaging methods and schemes (i.e., the combination of the members in averaging) to identify the most skillful and reliable multimodel averaging application. To achieve this, four hydrological models driven by six precipitation datasets were used as averaging members. The behaviors of 9 averaging methods and 11 averaging schemes in hydrological simulations were tested over 2277 watersheds distributed in different climate regions in the world. The results show the following: (1) The multi-input averaging schemes (i.e., members consist of one model driven by multiple precipitation datasets) generally perform better than the multimodel averaging schemes (i.e., members consist of multiple models driven by the same precipitation dataset) for each averaging method; (2) The use of multiple members can improve the averaging performances. Six averaging members are found to be necessary and advisable, since using more than six members only imrpoves the estimation results slightly, as compared with using all 24 members; (3) The advantage of using averaging methods for hydrological modeling is region dependent. The averaging methods, in general, produced the best results in the warm temperate region, followed by the snow and equatorial regions, while a large difference among various averaging methods is found in arid and arctic regions. This is mainly due to the different averaging methods being affected to a different extent by the poorly performed members in the arid and arctic regions; (4) the multimodel superensemble method (MMSE) is recommended for its robust and outstanding performance among various climatic regions.https://www.mdpi.com/2072-4292/13/13/2574multimodel averaging methodsprecipitation datasetshydrological modelsglobalclimate regions
spellingShingle Wenyan Qi
Jie Chen
Chongyu Xu
Yongjing Wan
Finding the Optimal Multimodel Averaging Method for Global Hydrological Simulations
Remote Sensing
multimodel averaging methods
precipitation datasets
hydrological models
global
climate regions
title Finding the Optimal Multimodel Averaging Method for Global Hydrological Simulations
title_full Finding the Optimal Multimodel Averaging Method for Global Hydrological Simulations
title_fullStr Finding the Optimal Multimodel Averaging Method for Global Hydrological Simulations
title_full_unstemmed Finding the Optimal Multimodel Averaging Method for Global Hydrological Simulations
title_short Finding the Optimal Multimodel Averaging Method for Global Hydrological Simulations
title_sort finding the optimal multimodel averaging method for global hydrological simulations
topic multimodel averaging methods
precipitation datasets
hydrological models
global
climate regions
url https://www.mdpi.com/2072-4292/13/13/2574
work_keys_str_mv AT wenyanqi findingtheoptimalmultimodelaveragingmethodforglobalhydrologicalsimulations
AT jiechen findingtheoptimalmultimodelaveragingmethodforglobalhydrologicalsimulations
AT chongyuxu findingtheoptimalmultimodelaveragingmethodforglobalhydrologicalsimulations
AT yongjingwan findingtheoptimalmultimodelaveragingmethodforglobalhydrologicalsimulations