Assessment of IMERG Precipitation Estimates over Europe

This paper evaluates Integrated Multi-Satellite Retrievals from GPM (IMERG-F) over Europe for the period 2014−2018 in order to evaluate application of the retrievals to hydrology. IMERG-F is compared with a large pan-European precipitation dataset built on rain gauge stations, i.e., the EN...

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Main Authors: Andrés Navarro, Eduardo García-Ortega, Andrés Merino, José Luis Sánchez, Christian Kummerow, Francisco J. Tapiador
Format: Article
Language:English
Published: MDPI AG 2019-10-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/11/21/2470
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author Andrés Navarro
Eduardo García-Ortega
Andrés Merino
José Luis Sánchez
Christian Kummerow
Francisco J. Tapiador
author_facet Andrés Navarro
Eduardo García-Ortega
Andrés Merino
José Luis Sánchez
Christian Kummerow
Francisco J. Tapiador
author_sort Andrés Navarro
collection DOAJ
description This paper evaluates Integrated Multi-Satellite Retrievals from GPM (IMERG-F) over Europe for the period 2014&#8722;2018 in order to evaluate application of the retrievals to hydrology. IMERG-F is compared with a large pan-European precipitation dataset built on rain gauge stations, i.e., the ENSEMBLES OBServation (E-OBS) gridded dataset. Although there is overall agreement in the spatial distribution of mean precipitation (R<sup>2</sup> = 0.8), important discrepancies are revealed in mountainous regions, specifically the Alps, Pyrenees, west coast of the British Isles, Scandinavia, the Iberian and Italian peninsulas, and the Adriatic coastline. The results show that the strongest contributors to poor performance are pixels where IMERG-F has no gauges available for adjustment. If rain gauges are available, IMERG-F yields results similar to those of the surface observations, although the performance varies by region. However, even accounting for gauge adjustment, IMERG-F systematically underestimates precipitation in the Alps and Scandinavian mountains. Conversely, IMERG-F overestimates precipitation in the British Isles, Italian Peninsula, Adriatic coastline, and eastern European plains. Additionally, the research shows that gauge adjustment worsens the spatial gradient of precipitation because of the coarse resolution of Global Precipitation Climatology Centre data.
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spelling doaj.art-bfe74aee161a49f69336710bb5e94f632022-12-21T17:24:25ZengMDPI AGRemote Sensing2072-42922019-10-011121247010.3390/rs11212470rs11212470Assessment of IMERG Precipitation Estimates over EuropeAndrés Navarro0Eduardo García-Ortega1Andrés Merino2José Luis Sánchez3Christian Kummerow4Francisco J. Tapiador5Atmospheric Physics Group (GFA), Department of Applied Physics, Universidad de León, 24071 León, SpainAtmospheric Physics Group (GFA), Department of Applied Physics, Universidad de León, 24071 León, SpainAtmospheric Physics Group (GFA), Department of Applied Physics, Universidad de León, 24071 León, SpainAtmospheric Physics Group (GFA), Department of Applied Physics, Universidad de León, 24071 León, SpainDepartment of Atmospheric Science, Colorado State University, Fort Collins, CO 80523, USAEarth and Space Sciences Group (ESS), Institute of Environmental Sciences (ICAM), University of Castilla-La Mancha, 45071 Toledo, SpainThis paper evaluates Integrated Multi-Satellite Retrievals from GPM (IMERG-F) over Europe for the period 2014&#8722;2018 in order to evaluate application of the retrievals to hydrology. IMERG-F is compared with a large pan-European precipitation dataset built on rain gauge stations, i.e., the ENSEMBLES OBServation (E-OBS) gridded dataset. Although there is overall agreement in the spatial distribution of mean precipitation (R<sup>2</sup> = 0.8), important discrepancies are revealed in mountainous regions, specifically the Alps, Pyrenees, west coast of the British Isles, Scandinavia, the Iberian and Italian peninsulas, and the Adriatic coastline. The results show that the strongest contributors to poor performance are pixels where IMERG-F has no gauges available for adjustment. If rain gauges are available, IMERG-F yields results similar to those of the surface observations, although the performance varies by region. However, even accounting for gauge adjustment, IMERG-F systematically underestimates precipitation in the Alps and Scandinavian mountains. Conversely, IMERG-F overestimates precipitation in the British Isles, Italian Peninsula, Adriatic coastline, and eastern European plains. Additionally, the research shows that gauge adjustment worsens the spatial gradient of precipitation because of the coarse resolution of Global Precipitation Climatology Centre data.https://www.mdpi.com/2072-4292/11/21/2470precipitationsatellite observationssurface observationsimergeurope
spellingShingle Andrés Navarro
Eduardo García-Ortega
Andrés Merino
José Luis Sánchez
Christian Kummerow
Francisco J. Tapiador
Assessment of IMERG Precipitation Estimates over Europe
Remote Sensing
precipitation
satellite observations
surface observations
imerg
europe
title Assessment of IMERG Precipitation Estimates over Europe
title_full Assessment of IMERG Precipitation Estimates over Europe
title_fullStr Assessment of IMERG Precipitation Estimates over Europe
title_full_unstemmed Assessment of IMERG Precipitation Estimates over Europe
title_short Assessment of IMERG Precipitation Estimates over Europe
title_sort assessment of imerg precipitation estimates over europe
topic precipitation
satellite observations
surface observations
imerg
europe
url https://www.mdpi.com/2072-4292/11/21/2470
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