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Climatic conditions are markedly different on the Atlantic and Pacific sides of western Panama, especially in the amount and seasonal distribution of rainfall. On the Caribbean slopes of the Tabasará Mountains, which face the rain-bearing trade winds, average rainfall is approximately twice as heavy as on the leeward Pacific slopes. The Caribbean coast receives 60–140 inches (1,500–3,550 mm) per year, while the more populated Pacific region receives 45–90 inches (1,140–2,290 mm). Furthermore, on the Caribbean side rain falls almost throughout the year, while on the Pacific side there is more seasonal variation—in Chiriquí province, for example, there is a pronounced ...(100 of 11680 words)