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In the middle of the precipitation range, transition zones occur in which small groves of needle-leaved trees are interspersed with grassland patches in an apparently random manner.
The precipitation range is − 16.0 to 1.58‰ (n = 22) with the highest and lowest values measured at the same location (El Zotz, Guatemala).
Since the variation in climatic parameters such as average annual temperature and precipitation had only a minor effect on the decomposition process, these variables might be neglected for the prediction of CWD mass loss in this temperature and precipitation range.
In addition, climatic parameters such as different temperatures and precipitation at individual sites were found to have only a minor effect on the decomposition process in this temperature and precipitation range (Herrmann et al. 2015).
Secondly, the comparison between observed and simulated land precipitation suggests that anthropogenic forcing most likely caused the redistribution of the repartition of land precipitation, decreasing the extent of arid area (area with precipitation range between 50 and 300 mm/yr), and increasing the extent of area with a precipitation range between 450 and 900 mm/yr.
This was consistent with the findings of other studies that WUE was low at both dry and wet extremes of the annual precipitation range and that peak WUE occurred at moderate precipitation levels [40], [41].
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Annual precipitation ranges from about 35 to 60 inches (900 to 1,500 mm) on the mainland.
Evaporation of precipitation ranges from 20 inches in the northwest to eight inches in the southeast.
Annual precipitation ranges from 60 to 120 inches (1,500 to 3,000 mm) or more.
Average annual precipitation ranges from 20 inches (500 mm) in the east to 28 inches (700 mm) in the west.
The mean annual temperature is 45.5 °F (7.5 °C); average annual precipitation ranges from 22 to 30 inches (550 to 750 mm).
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