Abstract

The day-to-day variability of the atmospheric circulation over the Caribbean region is investigated in this work through the extraction of frequently occurring atmospheric circulation types. A two-stage cluster analysis technique using Ward’s agglomerative algorithm followed by the k-means algorithm was applied to daily circulation defined by the NCEP/DOE reanalysis wind components at the 850 hPa level for the period 1979–2010. Seven atmospheric circulation types (CTs) were extracted. The daily circulation types are distinguished through the extension and location of the well-known quasi-stationary Atlantic and Pacific anticyclones. However, three of the circulation types show a third anticyclonic feature, a Gulf of Mexico anticyclone which is not observed on monthly scales because it is transient with a mean lifetime of 2–3 days and rarely occurs in the July–September period. Other notable characteristics include the decrease in annual frequency of a circulation type defined by the transient Gulf of Mexico anticyclone, a neutral area over the Greater Antilles islands and weaker than average easterly winds. In addition, a second type with south-easterly winds throughout the Caribbean increases in annual frequency. This latter type also had events lasting as long as 85 days. The monthly frequency of the CTs that prevail during the dry season is correlated with several Atlantic and Pacific based teleconnections. The resulting daily atmospheric circulation types in this work comprise the first atmospheric circulation catalogue, of many to come, for the Caribbean region and may be useful in statistical–dynamical downscaling applications to explain the variability of surface weather variables such as wind speeds.

Highlights

  • The Caribbean atmospheric circulation plays both a direct and an indirect role in Caribbean precipitation by variations in divergence (Gamble and Curtis 2008), influencing sea surface temperatures in the Gulf of Mexico or through air–sea interactions (Wu and Kirtman 2011)

  • We used the extended domain to identify the center of action of an anticyclonic flow over the Gulf of Mexico-Florida region in circulation types (CTs) 1, 3, 5, as well as the extension of the Atlantic anticyclone as this semi-permanent feature directly influences the atmospheric circulation in the Caribbean

  • Seven daily near-surface atmospheric circulation patterns were identified over the Caribbean region from the application of a two-stage cluster analysis technique on daily 850 hPa reanalysis circulation data defined by wind components

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Summary

Introduction

The Caribbean atmospheric circulation plays both a direct and an indirect role in Caribbean precipitation by variations in divergence (Gamble and Curtis 2008), influencing sea surface temperatures in the Gulf of Mexico or through air–sea interactions (Wu and Kirtman 2011). Previous investigations have related the direct influence of these features of Caribbean atmospheric circulation to rainfall characteristics on annual, seasonal, and monthly scales (Amador 2008; Hastenrath 1976; Hastenrath and Lamb 1977; Muñoz et al 2008; Muñoz and Enfield 2011; Wang 2007; Wang and Lee 2007; Cook and Vizy 2010), and have investigated the influence of other major factors such as Atlantic and Pacific sea surface temperatures (SSTs), the El Niño-Southern.

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