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The importance of using a high-resolution model to study the climate change on small islands: the Lesser Antilles case Cover

The importance of using a high-resolution model to study the climate change on small islands: the Lesser Antilles case

Open Access
|Dec 2014

Figures & Tables

Fig. 1

The box shows the ALADIN domain (12–20°N and 56–64°W: 850 km×850 km).

Table 1. For each island considered as land by ALADIN: area, highest elevation for ALADIN, CRU and Shuttle Radar Topography Mission (SRTM) and the number of land points in the grid of ALADIN and CRU

Highest elevation (m)Number of land point

IslandArea (km2)ALADINCRU2.0SRTMALADINCRU2.0
Antigua281121140211Montserrat10211022791411Guadeloupe14435674611467157Marie-Galante15884120411Dominica75012271144764Martinique11282402801397106Saint Lucia62024416795064Saint Vincent345416315123422Barbados4319811034052
Fig. 2

Monthly mean precipitation over the area 12–20°N and 56–64°W, obtained from ERA-interim dataset in black with circles (median on 156 sea points), CRU2.0 dataset in black with triangles (median on 28 land points), ALADIN simulation on Land in green with triangles (median on 47 land points), ALADIN simulation on Sea in blue with circle (median on 7128 sea points) for the end of the 20th century. Units are in mm/day.

Fig. 3

Monthly mean Tmax (maximum daily temperature) over the area 12–20°N and 56–64°W, obtained from ERA-interim dataset in black with circles (median on 156 sea points), CRU2.0 dataset in black with triangles (median on 28 land points), ALADIN simulation on Land in green with triangles (median on 47 land points), ALADIN simulation on Sea in blue with circle (median on 7128 sea points) for the end of the 20th century. Units are in °C.

Fig. 4

Monthly mean Tmin (minimum daily temperature) over the area 12–20°N and 56–64°W, obtained from ERA-interim dataset in black with circles (median on 156 sea points), CRU2.0 dataset in black with triangles (median on 28 land points), ALADIN simulation on Land in green with triangles (median on 47 land points), ALADIN simulation on Sea in blue with circle (median on 7128 sea points) for the end of the 20th century. Units are in °C.

Table 2. Anomalies (median on all model points) of the monthly mean temperature between the period 1971–2000 and the period 2071–2100 according to the two scenarios (RCP4.5, RCP8.5)

ScenarioModel pointJanFebMarAprMayJunJulAugSepOctNovDecYear
TminRCP4.5Land1.781.11.31.671.611.82.161.991.781.752.081.721.73Sea1.411.181.11.030.91.011.231.311.271.211.441.31.2RCP8.5Land2.812.552.693.313.193.343.413.453.433.323.73.043.18Sea2.272.122.062.122.022.152.362.582.582.542.542.322.30TmaxRCP4.5Land1.581.451.471.461.431.361.41.481.451.41.521.531.46Sea1.431.181.060.970.8511.231.321.281.181.431.321.19RCP8.5Land2.662.522.662.732.572.542.662.882.932.92.842.752.72Sea2.282.132.032.091.982.162.362.582.582.532.512.342.30

[i] All monthly mean temperature (min and max) increase significantly for all model points.

Fig. 5

Projections of the seasonal mean temperature for the period 2071–2100 relative to the period 1971–2000 baseline underline two scenarios (RCP4.5 in green and RCP8.5 in red) over all islands and Sea (divided in four zones: NW, NE, SE, SW). Units are in °C.

Table 3. Proportion of model points where the monthly mean precipitation increase (↗) or decrease (↘) significantly (at risk α=0.05) between the period 1971–2000 and the period 2071–2100 according to two scenarios (RCP4.5, RCP8.5)

ScenarioTrendModel pointJanFebMarAprMayJunJulAugSepOctNovDecYear
RCP4.5↗Land000000.40.690.020.3100.1900.10Sea0.010000000000.0300↘Land0.040.270.540.50.60.060.10.060.060.0800.420.375Sea00.090.810.8410.940.610.570.280.8900.740.99RCP8.5↗Land000000.40.60.10.150.020.3300.02Sea00.01000000000.0100↘Land0.620.480.940.520.420.080.020.020.10.600.710.56Sea0.750.220.890.610.980.630.740.70.780.860.070.940.99

[i] The sea and the land points are analysed separately. Grey columns indicate months for which trends on land clearly differ from those on sea.

Fig. 6

Projections of the seasonal mean precipitation for the period 2071–2100 relative to the period 1971–2000 baseline underline two scenarios (RCP4.5 in green and RCP8.5 in red) over all islands and Sea (divided in four zones: NW, NE, SE, SW). Units are in %.

Fig. 7

Twenty-two rain-gauge stations (daily precipitation) and the 16 land points of the RCM ALADIN-climate available in Guadeloupe.

Table 4. Comparison of precipitation extreme indices between observation and the output of the RCM at the nearest model point (before and after the q–q plot correction)

cddcwdrr1rr10rr30rr50cumulsdiir1dr3dr5d
Station DOBS8.220.2248.4100.128.611.43425.113.8138.1223.2280.7HIST6.530.9278.341.00.330.071645.35.928.355.076.0HISTcor7.819.1248.499.328.011.23419.713.8138.1192.7244.0Station AOBS13.411.0176.344.410.43.91597.19.094.3142.7168.4HIST4.049.6316.361.20.160.032123.16.724.146.767.4HISTcor12.510.5176.444.310.54.41609.59.1100.8135.8165.8
Fig. 8

Anomalies of indexes between HISTcor and RCPcor in percentage.

Language: English
Page range: 24065 - 24065
Submitted on: Feb 14, 2014
Accepted on: Sep 22, 2014
Published on: Dec 1, 2014
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2014 Philippe Cantet, Michel Déqué, Philippe Palany, Jean-Louis Maridet, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.