The Effects of the Trade Winds on the Distribution of Relative Humidity and the Diurnal Air Temperature Cycle on Oceanic Tropical Islands
Received Date: Jul 09, 2015 / Accepted Date: Jul 30, 2015 / Published Date: Aug 08, 2015
Abstract
On many oceanic tropical islands the trade winds blow from the east and as the air passes over the island it loses moisture to rain. The two hypotheses for this study are that the western part of the island is less humid and has a larger diurnal air temperature cycle. Using data available on the Internet, the two hypotheses were assayed 7 times on 6 different islands in the Pacific and Caribbean. The islands used in this study are Puerto Rico, Hispaniola, the Big Island of Hawaii, Maui, Oahu, and Kauai. The first hypothesis was tested only on Hispaniola and is true. The second hypothesis was tested on all the islands and is true on all the islands except on the Big Island of Hawaii and Maui. Using a p-value of 0.05, these hypotheses are as predicted 5 of the 7 times, which has a p-value of 6 x 10-6. These findings should apply to thousands oceanic tropical islands where data are sparse.
Keywords: Rain shadow; Oceanic; Tropical; Islands; Trade winds
Citation: Richards RT, Emiliano A, Mendez-Tejeda R (2015) The Effects of the Trade Winds on the Distribution of Relative Humidity and the Diurnal Air Temperature Cycle on Oceanic Tropical Islands. J Earth Sci Clim Change 6: 288. Doi: 10.4172/2157-7617.1000288
Copyright: © 2015 Richards RT, et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
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