Semi-detailed Soil Survey of the LIuidas Vale Area, St. Catherine-St ...
Semi-detailed Soil Survey of the LIuidas Vale Area, St. Catherine-St ...
Semi-detailed Soil Survey of the LIuidas Vale Area, St. Catherine-St ...
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DESCRIPTION OF THE SURVEY AREA<br />
until December. Rainfall peaks are centered around October and June. The<br />
annual R75/PET value for Ewarton is <strong>the</strong> lowest for all mentioned stations.<br />
For <strong>the</strong> hills surrounding <strong>the</strong> basins no climatic data are available from<br />
rainfall stations in <strong>the</strong> survey area. Based on <strong>the</strong> information <strong>of</strong> <strong>the</strong> Agroclimatic<br />
zones map for Jamaica (SSU 1989i), rainfall should be higher and<br />
PET should be lower than in <strong>the</strong> basins. Yearly R75/PET values will be<br />
between 1.00 and 1.25 and <strong>the</strong> dependable growing period will extend for at<br />
least eight months (May-December). The rainfall data from Point Hill are<br />
chosen for <strong>the</strong> hilly part <strong>of</strong> <strong>the</strong> area (Appendix I).<br />
A wide range <strong>of</strong> annual crops can be grown throughout <strong>the</strong> dependable<br />
growing period provided <strong>the</strong>ir growing cycle matches <strong>the</strong> length <strong>of</strong> <strong>the</strong><br />
dependable growing period and <strong>the</strong> temperature is within <strong>the</strong> acceptable<br />
range (see Section 2.2.2). Never<strong>the</strong>less, it should be avoided that crops are in<br />
a stage sensitive to heavy rainfall in <strong>the</strong> months <strong>of</strong> October, September and<br />
May.<br />
Rainfall intensities are not measured in <strong>the</strong> survey area. <strong>St</strong>udies <strong>of</strong> rainfall<br />
data from a wider range <strong>of</strong> stations in <strong>St</strong>. Ca<strong>the</strong>rine, more recent data and<br />
analyses <strong>of</strong> longer records <strong>of</strong> data can be found in different publications (SSU<br />
1987a, SSU 1989h, SSU 1989i).<br />
2.2.2 Daily air temperature^<br />
The daily air temperature, as presented in Appendix I and Table 3, is<br />
calculated with linear regression equations, relating elevation above mean<br />
sea level (msl) to minimum, mean and maximum day temperatures for all<br />
months (SSU 1988a). Temperature requirements <strong>of</strong> <strong>the</strong> different crops are<br />
defined in JAMPLES (see Chapter 5).<br />
Ewarton which is located in <strong>the</strong> <strong>St</strong>. Thomas in <strong>the</strong> <strong>Vale</strong> basin at an elevation<br />
<strong>of</strong> 260 m above msl. has temperatures varying from 17 °C (mean Tmin in<br />
February) to 30 °C (mean Tmax in August), as can be seen in Table 3. The<br />
Liuidas <strong>Vale</strong> basin at an elevation <strong>of</strong> approximately 370 m above msl is<br />
represented by Worthy Park, has approximately <strong>the</strong> same rounded <strong>of</strong>f<br />
values for Tmin and Tmax, but <strong>the</strong> yearly mean temperature is lower.<br />
Generally January to March are <strong>the</strong> coolest months and July to September<br />
<strong>the</strong> hottest months. These periods coincide roughly with <strong>the</strong> driest and <strong>the</strong><br />
wettest periods respectively.<br />
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