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occurs where precipitation is greater than potential evaporation.
Climate ratio is used to describe the moisture side of climate. It compares the precipitation (P) with the potential evapotranspiration (Ep) for a region. One way to do this is to express the relationship between them as a ratio using the formula: Climate ratio = P / Ep When the potential evaporation is greater than yearly precipitation, this ratio is less than 1. When precipitation is greater than evapotranspiration, the ratio is greater than 1. P: precipitation (in mm) or the amount of moisture available for evapotranspiration, evapotranspiration is the combined process of evaporation and plant respiration. Ep: potential evapotranspiration (in mm) or the amount of moisture needed for evapotranspiration. This value increases as temperature and plant life increase. The climate ratios are used to determine climate type: P/Ep: Less than 0.4: arid climate 0.4 - 0.8: semiarid climate 0.8 - 1.2: subhumid climate Greater than 1.2: humid climate Source: NOAA
soil mositure maybe recharged
The evaporation rate of a desert is much greater than the precipitation rate.
By carrying away moisture the wind allows air with a greater ability to absorb evaporation and so increased evaporation will occur (until equilibrium in vapor pressure is reached).
run off
The advantage of rotary evaporation over stationary evaporation is that there is a greater surface area exposed, and constant agitation of the liquid. This allows for a greater rate of evaporation, thus saving time.
The greater the surface area, the greater the rate of evaporation under identical atmospheric conditions.
The relatively great surface area of a liquid drop impacts the evaporation rate. The greater the surface area, the greater the rate of evaporation. the converse is also true.
occean
A greater water area produce a higher evaporation.
The rain forest precipitation is greater that 150 cm. Rain forest precipitation is basically how much rain falls and collects on earth.