Evaluating TMPA Rainfall over the Sparsely Gauged East African Rift

dc.contributor.authorMonsieurs, Elise
dc.contributor.authorKirschbaum, Dalia Bach
dc.contributor.authorTan, Jackson
dc.contributor.authorMateso, Jean-Claude Maki
dc.contributor.authorJacobs, Liesbet
dc.contributor.authorPlisnier, Pierre-Denis
dc.contributor.authorThiery, Wim
dc.contributor.authorUmutoni, Augusta
dc.contributor.authorMusoni, Didace
dc.contributor.authorBibentyo, Toussaint Mugaruka
dc.contributor.authorGanza, Gloire Bamulezi
dc.contributor.authorMawe, Guy Ilombe
dc.contributor.authorBagalwa, Luc
dc.contributor.authorKankurize, Clairia
dc.contributor.authorMichellier, Caroline
dc.contributor.authorStanley, Thomas
dc.contributor.authorKervyn, Francois
dc.contributor.authorKervyn, Matthieu
dc.contributor.authorDemoulin, Alain
dc.contributor.authorDewitte, Olivier
dc.date.accessioned2024-04-29T17:00:47Z
dc.date.available2024-04-29T17:00:47Z
dc.date.issued2018-09-01
dc.description.abstractAbstract Accurate precipitation data are fundamental for understanding and mitigating the disastrous effects of many natural hazards in mountainous areas. Floods and landslides, in particular, are potentially deadly events that can be mitigated with advanced warning, but accurate forecasts require timely estimation of precipitation, which is problematic in regions such as tropical Africa with limited gauge measurements. Satellite rainfall estimates (SREs) are of great value in such areas, but rigorous validation is required to identify the uncertainties linked to SREs for hazard applications. This paper presents results of an unprecedented record of gauge data in the western branch of the East African Rift, with temporal resolutions ranging from 30 min to 24 h and records from 1998 to 2018. These data were used to validate the Tropical Rainfall Measuring Mission (TRMM) Multisatellite Precipitation Analysis (TMPA) research version and near-real-time products for 3-hourly, daily, and monthly rainfall accumulations, over multiple spatial scales. Results indicate that there are at least two factors that led to the underestimation of TMPA at the regional level: complex topography and high rainfall intensities. The TMPA near-real-time product shows overall stronger rainfall underestimations but lower absolute errors and a better performance at higher rainfall intensities compared to the research version. We found area-averaged TMPA rainfall estimates relatively more suitable in order to move toward regional hazard assessment, compared to data from scarcely distributed gauges with limited representativeness in the context of high rainfall variability.
dc.description.sponsorshipWe are grateful to all institutions, research projects, and people who shared rain gauge data, including Appalachian State University (USA), Centre de Recherches en Hydrobiologie (DR Congo), EAGLES (http://www.eagles-kivu.be/project.htm) and CHOLTIC projects (BELSPO, Belgium), Meteo Rwanda (Rwanda), National Oceanic and Atmospheric Administration (USA), Observatoire Volcanologique de Goma (DR Congo), Pères Blancs Bukavu (DR Congo), University of Burundi (Burundi), Université Polytechnique de Gitega (Burundi), and United States Geological Survey (USA). Special thanks go to our partners at Centre de Recherche en Sciences Naturelles de Lwiro (DR Congo), Université Officielle de Bukavu (DR Congo), Kahuzi-Biega National Park (DR Congo; Mr. Radar Nishuli), and Mountains of the Moon University (Uganda), who are dedicated to maintaining and regularly collecting data from the gauge network in sometimes difficult field conditions. We thank Thom Bogaard for the fruitful discussions on the validation results. We also thank the Civil Protection in DR Congo and Olivier Machiels, who shared their insights on landslide hazard in the study area and made it possible to execute fieldwork. We thank George Huffman for sharing his expertise on the TMPA algorithms. The authors acknowledge NASA Goddard Earth Sciences Data and Information Services Center for providing full access to the precipitation datasets exploited in this study. Datasets can be accessed at https://discbeta.gsfc.nasa.gov/. Financial support came from BELSPO for RESIST (SR/00/305), AfReSlide (BR/121/A2/AfReSlide), and GeoRisCA (SD/RI/02A) research projects (http://resist.africamuseum.be/, http://afreslide.africamuseum.be/, http://georisca.africamuseum.be/), and an F.R.S.-FNRS PhD scholarship for E.M. The Belgian American Education Foundation facilitated a one-year research stay for E.M. at the Hydrological Sciences Laboratory at NASA Goddard Space Flight Centre. J.T. is supported by an appointment to the NASA Postdoctoral Program at Goddard Space Flight Center, administered by USRA through a contract with NASA (NNH15CO48B). Finally, we thank the reviewers for their help in improving the content of the paper.
dc.description.urihttps://journals.ametsoc.org/view/journals/hydr/19/9/jhm-d-18-0103_1.xml
dc.format.extent22 pages
dc.genrejournal articles
dc.identifierdoi:10.13016/m2xvht-2gt9
dc.identifier.citationMonsieurs, Elise, Dalia Bach Kirschbaum, Jackson Tan, Jean-Claude Maki Mateso, Liesbet Jacobs, Pierre-Denis Plisnier, Wim Thiery, et al. “Evaluating TMPA Rainfall over the Sparsely Gauged East African Rift.” Journal of Hydrometeorology 19, no. 9 (September 1, 2018): 1507–28. https://doi.org/10.1175/JHM-D-18-0103.1.
dc.identifier.urihttps://doi.org/10.1175/JHM-D-18-0103.1
dc.identifier.urihttp://hdl.handle.net/11603/33366
dc.language.isoen_US
dc.publisherAMS
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC GESTAR II
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
dc.rightsPublic Domain
dc.rights.urihttps://creativecommons.org/publicdomain/mark/1.0/
dc.titleEvaluating TMPA Rainfall over the Sparsely Gauged East African Rift
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0003-2288-0363

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