A global-scale evaluation of extreme event uncertainty in the <i>eartH2Observe</i> project

<p>Knowledge of how uncertainty propagates through a hydrological land surface modelling sequence is of crucial importance in the identification and characterisation of system weaknesses in the prediction of droughts and floods at global scale. We evaluated the performance of five state-of-the...

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Main Authors: T. R. Marthews, E. M. Blyth, A. Martínez-de la Torre, T. I. E. Veldkamp
Format: Article
Language:English
Published: Copernicus Publications 2020-01-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/24/75/2020/hess-24-75-2020.pdf
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author T. R. Marthews
E. M. Blyth
A. Martínez-de la Torre
T. I. E. Veldkamp
author_facet T. R. Marthews
E. M. Blyth
A. Martínez-de la Torre
T. I. E. Veldkamp
author_sort T. R. Marthews
collection DOAJ
description <p>Knowledge of how uncertainty propagates through a hydrological land surface modelling sequence is of crucial importance in the identification and characterisation of system weaknesses in the prediction of droughts and floods at global scale. We evaluated the performance of five state-of-the-art global hydrological and land surface models in the context of modelling extreme conditions (drought and flood). Uncertainty was apportioned between the model used (model skill) and also the satellite-based precipitation products used to drive the simulations (forcing data variability) for extreme values of precipitation, surface runoff and evaporation. We found in general that model simulations acted to augment uncertainty rather than reduce it. In percentage terms, the increase in uncertainty was most often less than the magnitude of the input data uncertainty, but of comparable magnitude in many environments. Uncertainty in predictions of evapotranspiration lows (drought) in dry environments was especially high, indicating that these circumstances are a weak point in current modelling system approaches. We also found that high data and model uncertainty points for both ET lows and runoff lows were disproportionately concentrated in the equatorial and southern tropics. Our results are important for highlighting the relative robustness of satellite products in the context of land surface simulations of extreme events and identifying areas where improvements may be made in the consistency of simulation models.</p>
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spelling doaj.art-12d38b4ebd7d4fd6ad3f390fc2d6be1d2022-12-22T01:13:21ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382020-01-0124759210.5194/hess-24-75-2020A global-scale evaluation of extreme event uncertainty in the <i>eartH2Observe</i> projectT. R. Marthews0E. M. Blyth1A. Martínez-de la Torre2T. I. E. Veldkamp3Centre for Ecology & Hydrology, Maclean Building, Wallingford, OX10 8BB, UKCentre for Ecology & Hydrology, Maclean Building, Wallingford, OX10 8BB, UKCentre for Ecology & Hydrology, Maclean Building, Wallingford, OX10 8BB, UKInstitute for Environmental Studies, Vrije Universiteit Amsterdam, 1081 HV Amsterdam, the Netherlands<p>Knowledge of how uncertainty propagates through a hydrological land surface modelling sequence is of crucial importance in the identification and characterisation of system weaknesses in the prediction of droughts and floods at global scale. We evaluated the performance of five state-of-the-art global hydrological and land surface models in the context of modelling extreme conditions (drought and flood). Uncertainty was apportioned between the model used (model skill) and also the satellite-based precipitation products used to drive the simulations (forcing data variability) for extreme values of precipitation, surface runoff and evaporation. We found in general that model simulations acted to augment uncertainty rather than reduce it. In percentage terms, the increase in uncertainty was most often less than the magnitude of the input data uncertainty, but of comparable magnitude in many environments. Uncertainty in predictions of evapotranspiration lows (drought) in dry environments was especially high, indicating that these circumstances are a weak point in current modelling system approaches. We also found that high data and model uncertainty points for both ET lows and runoff lows were disproportionately concentrated in the equatorial and southern tropics. Our results are important for highlighting the relative robustness of satellite products in the context of land surface simulations of extreme events and identifying areas where improvements may be made in the consistency of simulation models.</p>https://www.hydrol-earth-syst-sci.net/24/75/2020/hess-24-75-2020.pdf
spellingShingle T. R. Marthews
E. M. Blyth
A. Martínez-de la Torre
T. I. E. Veldkamp
A global-scale evaluation of extreme event uncertainty in the <i>eartH2Observe</i> project
Hydrology and Earth System Sciences
title A global-scale evaluation of extreme event uncertainty in the <i>eartH2Observe</i> project
title_full A global-scale evaluation of extreme event uncertainty in the <i>eartH2Observe</i> project
title_fullStr A global-scale evaluation of extreme event uncertainty in the <i>eartH2Observe</i> project
title_full_unstemmed A global-scale evaluation of extreme event uncertainty in the <i>eartH2Observe</i> project
title_short A global-scale evaluation of extreme event uncertainty in the <i>eartH2Observe</i> project
title_sort global scale evaluation of extreme event uncertainty in the i earth2observe i project
url https://www.hydrol-earth-syst-sci.net/24/75/2020/hess-24-75-2020.pdf
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