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Title: Impacts of Local Convective Processes on Rain on the Caribbean Island of Puerto Rico

Journal Article · · Journal of Geophysical Research: Atmospheres
ORCiD logo [1];  [2];  [2]; ORCiD logo [3]
  1. Department of Mathematics, Engineering, and Computer Science LaGuardia Community College Long Island City NY USA
  2. NOAA CREST and Department of Mechanical Engineering The City College of New York New York NY USA
  3. Department of Agronomy ‐ Crop, Soil and Environmental Sciences, and Department of Earth, Atmospheric and Planetary Sciences Purdue University West Lafayette IN USA
+ Show Author Affiliations

Abstract This study aims to determine the impacts of tropical island processes on local convective storms. An analysis of rain events on the island of Puerto Rico between 1 June 2015 and 31 July 2016 showed that local island‐enhanced western storms accounted for 89 of 322 storms. This period is of particular importance for the Caribbean as 2015 was one of the driest years on record. While large‐scale influences such as the El Niño–Southern Oscillation, the North Atlantic Oscillation, African easterly waves, and Saharan dust transport modulate moisture conditions in the region, correlations between precipitation and El Niño–Southern Oscillation (−0.14), North Atlantic Oscillation (−0.42), and Saharan dust (0.1) for 1980–2016 ranged from weak to moderate. Local data for the island of Puerto Rico from weather stations, the Convection, Aerosol, and Synoptic‐Effects in the Tropics field campaign, and the North American Mesoscale model support the initiation or enhancement of convective rain events due to local island processes. In particular, analysis of surface wind speed/direction, convective available potential energy, lifted index, and the bulk Richardson number substantiate local instability due to surface heating, orographic uplift, and sea breeze trade‐wind convergence. These convective forcings along with available precipitable water in excess of 50 mm ultimately led to intense storms despite severe rainfall‐mitigating dust episodes for which aerosol optical thickness exceeded 0.4. These results may have major implications for considering the impacts of local air‐sea‐land interactions on rainfall over other tropical islands.

Sponsoring Organization:
USDOE
OSTI ID:
1560187
Alternate ID(s):
OSTI ID: 1560191
Journal Information:
Journal of Geophysical Research: Atmospheres, Journal Name: Journal of Geophysical Research: Atmospheres Journal Issue: 12 Vol. 124; ISSN 2169-897X
Publisher:
American Geophysical Union (AGU)Copyright Statement
Country of Publication:
United States
Language:
English

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