A Comparison of Moderate and Extreme ERA‐5 Daily Precipitation With Two Observational Data Sets

Abstract A comparison of moderate to extreme daily precipitation from the ERA‐5 reanalysis by the European Centre for Medium‐Range Weather Forecasts against two observational gridded data sets, EOBS and CMORPH, is presented. We assess the co‐occurrence of precipitation days and compare the full prec...

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Main Authors: Pauline Rivoire, Olivia Martius, Philippe Naveau
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2021-04-01
Series:Earth and Space Science
Subjects:
Online Access:https://doi.org/10.1029/2020EA001633
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author Pauline Rivoire
Olivia Martius
Philippe Naveau
author_facet Pauline Rivoire
Olivia Martius
Philippe Naveau
author_sort Pauline Rivoire
collection DOAJ
description Abstract A comparison of moderate to extreme daily precipitation from the ERA‐5 reanalysis by the European Centre for Medium‐Range Weather Forecasts against two observational gridded data sets, EOBS and CMORPH, is presented. We assess the co‐occurrence of precipitation days and compare the full precipitation distributions. The co‐occurrence is quantified by the hit rate. An extended generalized Pareto distribution (EGPD) is fitted to the positive precipitation distribution at every grid point and confidence intervals of quantiles compared. The Kullback–Leibler divergence is used to quantify the distance between the entire EGPDs obtained from ERA‐5 and the observations. For days exceeding the local 90th percentile, the mean hit rate is 65% between ERA‐5 and EOBS (over Europe) and 60% between ERA‐5 and CMORPH (globally). Generally, we find a decrease of the co‐occurrence with increasing precipitation intensity. The agreement between ERA‐5 and EOBS is weaker over the southern Mediterranean region and Iceland compared to the rest of Europe. Differences between ERA‐5 and CMORPH are smallest over the oceans. Differences are largest over NW America, Central Asia, and land areas between 15°S and 15°N. The confidence intervals on quantiles are overlapping between ERA‐5 and the observational data sets for more than 80% of the grid points on average. The intensity comparisons indicate an excellent agreement between ERA‐5 and EOBS over Germany, Ireland, Sweden, and Finland, and a disagreement over areas where EOBS uses sparse input stations. ERA‐5 and CMORPH precipitation intensity agree well over the midlatitudes and disagree over the tropics.
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spelling doaj.art-e4794ca56beb4abbbaf6ed9c93655a032022-12-21T18:50:00ZengAmerican Geophysical Union (AGU)Earth and Space Science2333-50842021-04-0184n/an/a10.1029/2020EA001633A Comparison of Moderate and Extreme ERA‐5 Daily Precipitation With Two Observational Data SetsPauline Rivoire0Olivia Martius1Philippe Naveau2Oeschger Centre for Climate Change Research and Institute of Geography University of Bern Bern SwitzerlandOeschger Centre for Climate Change Research and Institute of Geography University of Bern Bern SwitzerlandLaboratoire des Sciences du Climat et de l'Environnement CNRS‐CEA‐UVSQ Gif‐sur‐Yvette FranceAbstract A comparison of moderate to extreme daily precipitation from the ERA‐5 reanalysis by the European Centre for Medium‐Range Weather Forecasts against two observational gridded data sets, EOBS and CMORPH, is presented. We assess the co‐occurrence of precipitation days and compare the full precipitation distributions. The co‐occurrence is quantified by the hit rate. An extended generalized Pareto distribution (EGPD) is fitted to the positive precipitation distribution at every grid point and confidence intervals of quantiles compared. The Kullback–Leibler divergence is used to quantify the distance between the entire EGPDs obtained from ERA‐5 and the observations. For days exceeding the local 90th percentile, the mean hit rate is 65% between ERA‐5 and EOBS (over Europe) and 60% between ERA‐5 and CMORPH (globally). Generally, we find a decrease of the co‐occurrence with increasing precipitation intensity. The agreement between ERA‐5 and EOBS is weaker over the southern Mediterranean region and Iceland compared to the rest of Europe. Differences between ERA‐5 and CMORPH are smallest over the oceans. Differences are largest over NW America, Central Asia, and land areas between 15°S and 15°N. The confidence intervals on quantiles are overlapping between ERA‐5 and the observational data sets for more than 80% of the grid points on average. The intensity comparisons indicate an excellent agreement between ERA‐5 and EOBS over Germany, Ireland, Sweden, and Finland, and a disagreement over areas where EOBS uses sparse input stations. ERA‐5 and CMORPH precipitation intensity agree well over the midlatitudes and disagree over the tropics.https://doi.org/10.1029/2020EA001633ERA‐5precipitationreanalysisextended generalized Pareto distributionEOBSCMORPH
spellingShingle Pauline Rivoire
Olivia Martius
Philippe Naveau
A Comparison of Moderate and Extreme ERA‐5 Daily Precipitation With Two Observational Data Sets
Earth and Space Science
ERA‐5
precipitation
reanalysis
extended generalized Pareto distribution
EOBS
CMORPH
title A Comparison of Moderate and Extreme ERA‐5 Daily Precipitation With Two Observational Data Sets
title_full A Comparison of Moderate and Extreme ERA‐5 Daily Precipitation With Two Observational Data Sets
title_fullStr A Comparison of Moderate and Extreme ERA‐5 Daily Precipitation With Two Observational Data Sets
title_full_unstemmed A Comparison of Moderate and Extreme ERA‐5 Daily Precipitation With Two Observational Data Sets
title_short A Comparison of Moderate and Extreme ERA‐5 Daily Precipitation With Two Observational Data Sets
title_sort comparison of moderate and extreme era 5 daily precipitation with two observational data sets
topic ERA‐5
precipitation
reanalysis
extended generalized Pareto distribution
EOBS
CMORPH
url https://doi.org/10.1029/2020EA001633
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