Using information from 2 locations, Berkeley, California and Terre Haute, Indiana, a comparison of the water balance will be completed between the 2 sites. The data includes precipitation, potential and actual evapotranspiration, soil water storage, deficit and surplus.
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To compare the water balance between Berkeley, California, and Terre Haute, Indiana, we need data on precipitation, potential evapotranspiration (PET), actual evapotranspiration (AET), soil water storage, deficit, and surplus for both locations.
1. Precipitation: This refers to the amount of rainfall and/or snowfall that occurs at each location. You can obtain this data from weather resources like the National Weather Service or online databases that provide historical weather data.
2. Potential Evapotranspiration (PET): PET represents the maximum amount of water that could be evaporated and transpired by plants under optimal conditions. It is influenced by factors like temperature, humidity, wind speed, and solar radiation. You can calculate PET using methods like the Penman-Monteith equation or obtain it from weather stations or meteorological databases.
3. Actual Evapotranspiration (AET): AET is the actual amount of water that is evaporated and transpired by plants in a given area. This value depends on factors like vegetation type, soil type, and water availability. AET can be estimated using methods such as remote sensing or by using data from weather stations equipped with specific sensors.
4. Soil Water Storage: This refers to the amount of water stored in the soil. It can be measured using soil moisture sensors or obtained from soil moisture monitoring networks if available.
5. Deficit: The deficit represents the amount of water needed to replenish the soil moisture back to its field capacity. It is calculated by subtracting the soil moisture from the field capacity.
6. Surplus: The surplus indicates the excess water present in the soil after it reaches its field capacity. It is calculated by subtracting the field capacity from the soil moisture.
Once you have collected the data for precipitation, PET, AET, soil water storage, deficit, and surplus for both Berkeley, California, and Terre Haute, Indiana, you can compare the water balance between the two locations. This comparison will help you understand the differences in water availability and usage between the two regions.