Water cycle changes in reanalyses: a complementary framework

Abstract Climate reanalyses complement traditional surface-based measurements and offer unprecedented coverage over previously inaccessible or unmonitored regions. Even though these have improved the quantification of the global water cycle, their varying performances and uncertainties limit their a...

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Main Authors: Mijael Rodrigo Vargas Godoy, Yannis Markonis
Format: Article
Language:English
Published: Nature Portfolio 2023-03-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-023-31873-5
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author Mijael Rodrigo Vargas Godoy
Yannis Markonis
author_facet Mijael Rodrigo Vargas Godoy
Yannis Markonis
author_sort Mijael Rodrigo Vargas Godoy
collection DOAJ
description Abstract Climate reanalyses complement traditional surface-based measurements and offer unprecedented coverage over previously inaccessible or unmonitored regions. Even though these have improved the quantification of the global water cycle, their varying performances and uncertainties limit their applicability. Herein, we discuss how a framework encompassing precipitation, evaporation, their difference, and their sum could further constrain uncertainty by unveiling discrepancies otherwise overlooked. Ahead, we physically define precipitation plus evaporation to describe the global water cycle fluxes in four reanalysis data sets (20CR v3, ERA-20C, ERA5, and NCEP1). Among them, we observe four different responses to the temperature increase between 1950–2010, with ERA5 showing the best agreement with the water cycle acceleration hypothesis. Our results show that implementing the framework proposed can improve the evaluation of reanalyses’ performance and enhance our understanding of the water cycle changes on a global scale.
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spelling doaj.art-14bcbe7345444646bb839cfc794a4b122023-03-26T11:09:22ZengNature PortfolioScientific Reports2045-23222023-03-0113111210.1038/s41598-023-31873-5Water cycle changes in reanalyses: a complementary frameworkMijael Rodrigo Vargas Godoy0Yannis Markonis1Faculty of Environmental Sciences, Czech University of Life Sciences PragueFaculty of Environmental Sciences, Czech University of Life Sciences PragueAbstract Climate reanalyses complement traditional surface-based measurements and offer unprecedented coverage over previously inaccessible or unmonitored regions. Even though these have improved the quantification of the global water cycle, their varying performances and uncertainties limit their applicability. Herein, we discuss how a framework encompassing precipitation, evaporation, their difference, and their sum could further constrain uncertainty by unveiling discrepancies otherwise overlooked. Ahead, we physically define precipitation plus evaporation to describe the global water cycle fluxes in four reanalysis data sets (20CR v3, ERA-20C, ERA5, and NCEP1). Among them, we observe four different responses to the temperature increase between 1950–2010, with ERA5 showing the best agreement with the water cycle acceleration hypothesis. Our results show that implementing the framework proposed can improve the evaluation of reanalyses’ performance and enhance our understanding of the water cycle changes on a global scale.https://doi.org/10.1038/s41598-023-31873-5
spellingShingle Mijael Rodrigo Vargas Godoy
Yannis Markonis
Water cycle changes in reanalyses: a complementary framework
Scientific Reports
title Water cycle changes in reanalyses: a complementary framework
title_full Water cycle changes in reanalyses: a complementary framework
title_fullStr Water cycle changes in reanalyses: a complementary framework
title_full_unstemmed Water cycle changes in reanalyses: a complementary framework
title_short Water cycle changes in reanalyses: a complementary framework
title_sort water cycle changes in reanalyses a complementary framework
url https://doi.org/10.1038/s41598-023-31873-5
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