The importance of using a high-resolution model to study the climate change on small islands: the Lesser Antilles case
High-resolution climate change simulations over the Lesser Antilles are performed using the ALADIN-Climate regional climate model nested within the global model ARPEGE (Météo-France). Three sets of simulations are conducted at 10 km grid spacing for reference (1971–2000) and future climate (2071–210...
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2014-10-01
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doaj-bdbda3c6b04a4c3590020bd3230f65592020-11-24T21:46:48ZengTaylor & Francis GroupTellus: Series A, Dynamic Meteorology and Oceanography1600-08702014-10-0166011110.3402/tellusa.v66.2406524065The importance of using a high-resolution model to study the climate change on small islands: the Lesser Antilles casePhilippe Cantet0Michel Déqué1Philippe Palany2Jean-Louis Maridet3 Météo France DIRAG, Morne Desaix – BP 645, FR-97262 Fort-de-France Cedex, France CNRM-GAME (Météo-France, CNRS), Toulouse, France Météo France DIRAG, Morne Desaix – BP 645, FR-97262 Fort-de-France Cedex, France Météo France DIRAG, Morne Desaix – BP 645, FR-97262 Fort-de-France Cedex, FranceHigh-resolution climate change simulations over the Lesser Antilles are performed using the ALADIN-Climate regional climate model nested within the global model ARPEGE (Météo-France). Three sets of simulations are conducted at 10 km grid spacing for reference (1971–2000) and future climate (2071–2100) under two CMIP5 scenarios (RCP4.5 and RCP8.5). With the dynamical downscaling, islands of Lesser Antilles are considered as land by the model, whereas, for the driving model, there is only sea over the domain. Temperature and precipitation change are analysed on land and on sea separately. For temperature, the warming is greater on land than on sea, especially for the minimum daily temperature (3.2°C vs. 2.3°C for the RCP85 scenario). For precipitation, projections are less reliable because the seasonality is not well reproduced by the model. Nevertheless, simulations exhibit the fact that projections on land differ from one island to the other and disagree with those on sea notably during the wet season. This underlines the importance of the dynamical downscaling to study the climate on small islands. Statistical downscaling has been performed on the Guadeloupe Island to study changes in extreme precipitation indices. The projections provided by the regional climate model suggest an increase in extreme rainfall events: longer dry periods, a bigger annual total precipitation, more frequent very heavy daily precipitation and a stronger 1 d maximum precipitation, whereas for the driving Global Climate Model, these trends are less intense.http://www.tellusa.net/index.php/tellusa/article/download/24065/pdf_1climate changeregional climate modelRCP scenariosLesser Antillestemperatureprecipitation |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Philippe Cantet Michel Déqué Philippe Palany Jean-Louis Maridet |
spellingShingle |
Philippe Cantet Michel Déqué Philippe Palany Jean-Louis Maridet The importance of using a high-resolution model to study the climate change on small islands: the Lesser Antilles case Tellus: Series A, Dynamic Meteorology and Oceanography climate change regional climate model RCP scenarios Lesser Antilles temperature precipitation |
author_facet |
Philippe Cantet Michel Déqué Philippe Palany Jean-Louis Maridet |
author_sort |
Philippe Cantet |
title |
The importance of using a high-resolution model to study the climate change on small islands: the Lesser Antilles case |
title_short |
The importance of using a high-resolution model to study the climate change on small islands: the Lesser Antilles case |
title_full |
The importance of using a high-resolution model to study the climate change on small islands: the Lesser Antilles case |
title_fullStr |
The importance of using a high-resolution model to study the climate change on small islands: the Lesser Antilles case |
title_full_unstemmed |
The importance of using a high-resolution model to study the climate change on small islands: the Lesser Antilles case |
title_sort |
importance of using a high-resolution model to study the climate change on small islands: the lesser antilles case |
publisher |
Taylor & Francis Group |
series |
Tellus: Series A, Dynamic Meteorology and Oceanography |
issn |
1600-0870 |
publishDate |
2014-10-01 |
description |
High-resolution climate change simulations over the Lesser Antilles are performed using the ALADIN-Climate regional climate model nested within the global model ARPEGE (Météo-France). Three sets of simulations are conducted at 10 km grid spacing for reference (1971–2000) and future climate (2071–2100) under two CMIP5 scenarios (RCP4.5 and RCP8.5). With the dynamical downscaling, islands of Lesser Antilles are considered as land by the model, whereas, for the driving model, there is only sea over the domain. Temperature and precipitation change are analysed on land and on sea separately. For temperature, the warming is greater on land than on sea, especially for the minimum daily temperature (3.2°C vs. 2.3°C for the RCP85 scenario). For precipitation, projections are less reliable because the seasonality is not well reproduced by the model. Nevertheless, simulations exhibit the fact that projections on land differ from one island to the other and disagree with those on sea notably during the wet season. This underlines the importance of the dynamical downscaling to study the climate on small islands. Statistical downscaling has been performed on the Guadeloupe Island to study changes in extreme precipitation indices. The projections provided by the regional climate model suggest an increase in extreme rainfall events: longer dry periods, a bigger annual total precipitation, more frequent very heavy daily precipitation and a stronger 1 d maximum precipitation, whereas for the driving Global Climate Model, these trends are less intense. |
topic |
climate change regional climate model RCP scenarios Lesser Antilles temperature precipitation |
url |
http://www.tellusa.net/index.php/tellusa/article/download/24065/pdf_1 |
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