Flood hazard maps in Matucana village under climate change scenarios

Possible effects of climate change on floods magnitude and effects are discussed in this document based on existing data and projected changes in precipitation until 2099. This methodology is applied to Matucana Village, which suffers the effects of floods and debris flows. First, historical peak pr...

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Main Authors: J. W. Cabrera Cabrera, L. F. Castillo Navarro
Format: Article
Language:English
Published: Copernicus Publications 2014-09-01
Series:Proceedings of the International Association of Hydrological Sciences
Online Access:https://www.proc-iahs.net/364/171/2014/piahs-364-171-2014.pdf
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spelling doaj-91cab6cabea849999621990f12e8c9af2020-11-25T00:59:57ZengCopernicus PublicationsProceedings of the International Association of Hydrological Sciences2199-89812199-899X2014-09-0136417117510.5194/piahs-364-171-2014Flood hazard maps in Matucana village under climate change scenariosJ. W. Cabrera Cabrera0L. F. Castillo Navarro1Facultad de Ingeniería Civil, Universidad Nacional de Ingeniería, Lima25, PeruFacultad de Ingeniería Civil, Universidad Nacional de Ingeniería, Lima25, PeruPossible effects of climate change on floods magnitude and effects are discussed in this document based on existing data and projected changes in precipitation until 2099. This methodology is applied to Matucana Village, which suffers the effects of floods and debris flows. First, historical peak precipitation, fitted to Gumbel distribution, was used, After that, percentage projected changes of precipitation were used to obtain the new mean precipitation to each period 2010–2039, 2040–2069 and 2070–2099; these mean precipitations define a new Gumbel distribution for every time period. Then, projected maximal precipitations to 100 years of return period are estimated and the corresponding peak flow hydrographs were built. Finally, hazard maps are plotted. This application is possible because Matucana is located in a climatologically homogeneous basin. The final results suggest an important increase in magnitude and affected area by floods in the next 90 years under the A1FI emission scenario.https://www.proc-iahs.net/364/171/2014/piahs-364-171-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. W. Cabrera Cabrera
L. F. Castillo Navarro
spellingShingle J. W. Cabrera Cabrera
L. F. Castillo Navarro
Flood hazard maps in Matucana village under climate change scenarios
Proceedings of the International Association of Hydrological Sciences
author_facet J. W. Cabrera Cabrera
L. F. Castillo Navarro
author_sort J. W. Cabrera Cabrera
title Flood hazard maps in Matucana village under climate change scenarios
title_short Flood hazard maps in Matucana village under climate change scenarios
title_full Flood hazard maps in Matucana village under climate change scenarios
title_fullStr Flood hazard maps in Matucana village under climate change scenarios
title_full_unstemmed Flood hazard maps in Matucana village under climate change scenarios
title_sort flood hazard maps in matucana village under climate change scenarios
publisher Copernicus Publications
series Proceedings of the International Association of Hydrological Sciences
issn 2199-8981
2199-899X
publishDate 2014-09-01
description Possible effects of climate change on floods magnitude and effects are discussed in this document based on existing data and projected changes in precipitation until 2099. This methodology is applied to Matucana Village, which suffers the effects of floods and debris flows. First, historical peak precipitation, fitted to Gumbel distribution, was used, After that, percentage projected changes of precipitation were used to obtain the new mean precipitation to each period 2010–2039, 2040–2069 and 2070–2099; these mean precipitations define a new Gumbel distribution for every time period. Then, projected maximal precipitations to 100 years of return period are estimated and the corresponding peak flow hydrographs were built. Finally, hazard maps are plotted. This application is possible because Matucana is located in a climatologically homogeneous basin. The final results suggest an important increase in magnitude and affected area by floods in the next 90 years under the A1FI emission scenario.
url https://www.proc-iahs.net/364/171/2014/piahs-364-171-2014.pdf
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