Characterization of Future Caribbean Rainfall and Temperature Extremes across Rainfall Zones

End-of-century changes in Caribbean climate extremes are derived from the Providing Regional Climate for Impact Studies (PRECIS) regional climate model (RCM) under the A2 and B2 emission scenarios across five rainfall zones. Trends in rainfall, maximum temperature, and minimum temperature extremes f...

Full description

Bibliographic Details
Main Authors: Natalie Melissa McLean, Tannecia Sydia Stephenson, Michael Alexander Taylor, Jayaka Danaco Campbell
Format: Article
Language:English
Published: Hindawi Limited 2015-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2015/425987
id doaj-2964096f854e47819863e76bc320f3a4
record_format Article
spelling doaj-2964096f854e47819863e76bc320f3a42020-11-24T22:20:50ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172015-01-01201510.1155/2015/425987425987Characterization of Future Caribbean Rainfall and Temperature Extremes across Rainfall ZonesNatalie Melissa McLean0Tannecia Sydia Stephenson1Michael Alexander Taylor2Jayaka Danaco Campbell3The Climate Studies Group Mona, The University of the West Indies, Mona, Kingston 7, JamaicaThe Climate Studies Group Mona, The University of the West Indies, Mona, Kingston 7, JamaicaThe Climate Studies Group Mona, The University of the West Indies, Mona, Kingston 7, JamaicaThe Climate Studies Group Mona, The University of the West Indies, Mona, Kingston 7, JamaicaEnd-of-century changes in Caribbean climate extremes are derived from the Providing Regional Climate for Impact Studies (PRECIS) regional climate model (RCM) under the A2 and B2 emission scenarios across five rainfall zones. Trends in rainfall, maximum temperature, and minimum temperature extremes from the RCM are validated against meteorological stations over 1979–1989. The model displays greater skill at representing trends in consecutive wet days (CWD) and extreme rainfall (R95P) than consecutive dry days (CDD), wet days (R10), and maximum 5-day precipitation (RX5). Trends in warm nights, cool days, and warm days were generally well reproduced. Projections for 2071–2099 relative to 1961–1989 are obtained from the ECHAM5 driven RCM. Northern and eastern zones are projected to experience more intense rainfall under A2 and B2. There is less consensus across scenarios with respect to changes in the dry and wet spell lengths. However, there is indication that a drying trend may be manifest over zone 5 (Trinidad and northern Guyana). Changes in the extreme temperature indices generally suggest a warmer Caribbean towards the end of century across both scenarios with the strongest changes over zone 4 (eastern Caribbean).http://dx.doi.org/10.1155/2015/425987
collection DOAJ
language English
format Article
sources DOAJ
author Natalie Melissa McLean
Tannecia Sydia Stephenson
Michael Alexander Taylor
Jayaka Danaco Campbell
spellingShingle Natalie Melissa McLean
Tannecia Sydia Stephenson
Michael Alexander Taylor
Jayaka Danaco Campbell
Characterization of Future Caribbean Rainfall and Temperature Extremes across Rainfall Zones
Advances in Meteorology
author_facet Natalie Melissa McLean
Tannecia Sydia Stephenson
Michael Alexander Taylor
Jayaka Danaco Campbell
author_sort Natalie Melissa McLean
title Characterization of Future Caribbean Rainfall and Temperature Extremes across Rainfall Zones
title_short Characterization of Future Caribbean Rainfall and Temperature Extremes across Rainfall Zones
title_full Characterization of Future Caribbean Rainfall and Temperature Extremes across Rainfall Zones
title_fullStr Characterization of Future Caribbean Rainfall and Temperature Extremes across Rainfall Zones
title_full_unstemmed Characterization of Future Caribbean Rainfall and Temperature Extremes across Rainfall Zones
title_sort characterization of future caribbean rainfall and temperature extremes across rainfall zones
publisher Hindawi Limited
series Advances in Meteorology
issn 1687-9309
1687-9317
publishDate 2015-01-01
description End-of-century changes in Caribbean climate extremes are derived from the Providing Regional Climate for Impact Studies (PRECIS) regional climate model (RCM) under the A2 and B2 emission scenarios across five rainfall zones. Trends in rainfall, maximum temperature, and minimum temperature extremes from the RCM are validated against meteorological stations over 1979–1989. The model displays greater skill at representing trends in consecutive wet days (CWD) and extreme rainfall (R95P) than consecutive dry days (CDD), wet days (R10), and maximum 5-day precipitation (RX5). Trends in warm nights, cool days, and warm days were generally well reproduced. Projections for 2071–2099 relative to 1961–1989 are obtained from the ECHAM5 driven RCM. Northern and eastern zones are projected to experience more intense rainfall under A2 and B2. There is less consensus across scenarios with respect to changes in the dry and wet spell lengths. However, there is indication that a drying trend may be manifest over zone 5 (Trinidad and northern Guyana). Changes in the extreme temperature indices generally suggest a warmer Caribbean towards the end of century across both scenarios with the strongest changes over zone 4 (eastern Caribbean).
url http://dx.doi.org/10.1155/2015/425987
work_keys_str_mv AT nataliemelissamclean characterizationoffuturecaribbeanrainfallandtemperatureextremesacrossrainfallzones
AT tanneciasydiastephenson characterizationoffuturecaribbeanrainfallandtemperatureextremesacrossrainfallzones
AT michaelalexandertaylor characterizationoffuturecaribbeanrainfallandtemperatureextremesacrossrainfallzones
AT jayakadanacocampbell characterizationoffuturecaribbeanrainfallandtemperatureextremesacrossrainfallzones
_version_ 1725773659034877952