Water Budgets For Berkeley, California And Terre Haute, Indiana Essay Example
The text examines the significance of water as a natural resource and the necessity to guarantee an adequate supply for all needs. It clarifies that different locations calculate water budgets to evaluate the water balance in their specific environments. This assessment aids in comprehending periods of surplus, usage, scarcity, and replenishment within the water system. The research presents and contrasts the water budgets of Berkeley, California and Terre Haute, Indiana for a particular year. The objective is to identify similarities, differences, and potential climatic influences on these disparities.
The tables show the periods of surplus, usage, deficit, and recharge. Both locations had a surplus between January and March, with Terre Haute having a surplus until April. Utilization occurred at similar times for both locations; April to May for Berkeley and May to June for Ha
...ute. The two climates achieved similarities in different ways. At the beginning of the year, Terre Haute experienced a cold winter which led to lower evaporation rates. Consequently, despite receiving less precipitation than Berkeley during the same period, it was stored instead of evaporated.
High precipitation was observed at Berkeley as a result of moisture laden westerly winds from the Pacific creating relief rainfall. However, the high evaporation rates prevented adequate conservation of water, causing the storage to decrease to levels similar to Haute's. Later in the year, spring likely increased water utilization at Terre Haute due to the blooming flowers and leaves.
Despite a slight increase in precipitation, there was a reduced storage. A similar trend was observed in Berkeley during the same time, where a reduction in precipitation and an increase in evaporation
occurred at the start of the dry season. The main distinction can be found in the duration of deficit periods. In Berkeley, precipitation decreased considerably and evaporation increased throughout the dry season, lasting for almost half of the year until around October. This prolonged period of deficit was noteworthy.
Despite experiencing a deficit during the summer months (July to September), Terre Haute swiftly recovered with the arrival of autumn, as cooler temperatures and decreased evaporation prompted an earlier recharge compared to Berkeley. In contrast, Berkeley's recharge started later in the year, towards the end. Ultimately, climate and altitude variations greatly influenced the water balance in these regions. It is essential to comprehend the water balance in order to ascertain trends in water availability in both areas.
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