Water Balance - Lab Report Example

The vegetation and near costal topography of Berkeley is different when compared to the hilly continental Terre Haute which earlier had a facilitating water storage with a longer period. Humid and hot air with high pressure characterize Berkeley, which has dry and hot seasons. The indication to this is through the precipitation levels, which are precipitations less than one centimeter in the region during summer and up to 10 centimeters rise in precipitation in the same region during winter. This simply means that there is a rise in precipitation during winter and a fall during summer.

This shifts focus to the earlier mentioned vegetation, which can only survive in one region at a time. When compared to a low-lying coastal stretch California, Indiana has high altitude levels meaning the climatic changes in both regions differ. Precipitation come because of the humid winds that blow from the oceans because of evaporation that continuously take place in oceans. When evaporation takes place in the oceans, winds blowing collect the water in humid form thus bringing about precipitation.

The latter statement suggests that without winds there can be no precipitation explaining why precipitation is less in dry areas but very high in moist and icy areas. There is a higher likelihood of Evapotranspiration taking place brought about by high pressure and temperatures. The two figures explain that when there are high speeds of wind, precipitation goes high and vice versa. Therefore, during the months or November to march when the wind speeds are slightly higher than other months, the precipitation levels are high.

It is during the months of November to march that high temperature levels force water to turn to vapor which ascends to the atmosphere and falls as conventional rainfall after condensation. Science explains that when water moves up in terms of vapor it