The water balance is the balance of the inputs and outputs of water. The water balance of a specific area can be determined by calculating its input, output, and storage changes. Input normally alludes to rainfall, but may also be river inflow, and groundwater inflow. Output pertains to evaporation, transpiration, river outflow, and groundwater outflow. Lastly, storage pertains to groundwater storage and soil moisture.
In a most ideal situation, water input in a system is matched by water output, resulting in a balanced water system However, changes in the weather, natural processes, and human intervention can all have significant impacts on the water balance.
Water balance can be expressed by the formula P = Q + E +/- S.
S: Change in storage
The water balance has significant implications on the surrounding environment. It also dictates how much water is stored in a particular water system. Assessing the water balance in a given area is an effective method of determining its water input and output. The survey of an area’s water balance can also aid in identifying the factors that play a part in maintaining the water balance. Research and study of the water balance can prove beneficial for the proper management of water as a resource.
Elements of the Water Balance
Precipitation is the condensation of water vapour in the atmosphere that falls to the ground. Precipitation may come in the form of rain, snow, hail, ice pellets, and graupel.
When the atmosphere becomes saturated with water vapour, the water condenses and transforms from its gaseous state to its liquid state. There are two processes that can result into the air being saturated with water vapour–a reduction in the air’s temperature, or the addition of more water vapour. Usually, these two processes occur together and make precipitation possible. Precipitation is heavily reliant on the amount of moisture in the atmosphere, and more moisture increases the chances of precipitation.
Rain is a common form of precipitation and can vary in size, shape, amount and temperature. The characteristics of rainfall depends on the weather conditions present at the time of its formation.
Hail is precipitation that falls in the form of solid water or ice. Hail is created as a result of the repeated cycling of hailstones inside cumulonimbus clouds as a result of strong updrafts of wind. The hailstones inside the cloud gradually build up more layers of ice until it is heavy enough to fall to the ground. Precipitation in the form of hail does not require very low temperatures, as it is more reliant on the process that creates it than it is on temperature.
Snow and snowflakes are precipitation created in cold environments. These kinds of precipitation requires the temperature of the earth below to be near or below freezing. Snowflakes come in many different sizes, shapes and patterns. No two snowflakes are identical.
Evaporation is the process in which water in its liquid state turns into its gaseous state. Liquid water from the ground level evaporates into water vapour which then rises into the atmosphere above.
The rate of evaporation is determined by many factors such as air temperature, the amount of water vapour present in the air (humidity), solar radiation, altitude, and the current state of the ground level. Evaporation occurs the most in places that have high temperatures, brisk air flow, and large surfaces of water.
Evaporation is the water’s phase change from its liquid state to its gaseous state. Liquid water is released into the air as water vapour. Transpiration, on the other hand, is the phase change of water from plants into water vapour. Evapo-tranpiration is simply the combination of these two processes. It is the sum of the amount of moisture released into the atmosphere by both evaporation and transpiration. The rate of evapo-transporation is largely dependent on the surrounding temperature. evapotranspiration dictates all atmospheric conditions and is therefore an essential element in studying the climate.
Potential evapotranspiration (PE)
Potential evapotranspiration is a process dependent on the availability of water. When the amount of moisture sufficiently meets the needs of plants and vegetation, the evaporation that results from this is called potential evapotranspiration. In other words, it is the amount of water that must be evaporated and transpirated in order to maintain optimal environmental conditions.
In any place, the various environmental conditions and their effects produce a demand for water. When the demand for water is greater than the amount of water actually present, the soil will be dry and lack moisture. This poses significant threats on the condition of the area. Plants need a certain amount of water to survive, and are especially vulnerable to the lack of available moisture.
Actual evapotranspiration (AE)
Unlike the former, actual evapotranspiration is the actual amount of water vapour that comes from both evaporation and transpiration. It is dependent on factors such as the amount of available moisture, temperature, and humidity. It can otherwise be understood as the water that is actually being evaporated and transpirated in an area.
The amount of water available also determines the amount of evapotranspiration. If there is no water nor plants in an area, there is no evaporation or transpiration.
Soil moisture storage (ST)
Soil moisture storage is the amount of water that is contained in the soil at any single instance. This amount relies on factors such as the soil’s texture and its organic matter content. Field capacity is the maximum amount of water that soil can contain. Soil with fine grains have larger field capacities than those with coarse grains. This means that in fine-grained soils, there is more water available for evapotranspiration. Soil cannot take in more water than its field capacity. A soil moisture storage of 0 means that the soil contains no water and has dried out.
Change in soil moisture storage (ÄST)
Water that is added or removed from the water stored in the soil results in a change in soil moisture storage. This change in soil moisture storage can lie in between the lower limit of 0, and the upper limit of the field capacity.
Soil moisture deficit is when potential evapotranspiration is greater than actual evapotranspiration. In other words, it is when the demand for water goes beyond what is actually available. Deficit only occurs when the soil contains no moisture at all. This is when soil moisture storage is at 0. Determining the deficit allows one to discover how much water is needed to to balance out the system.
Surplus occurs when precipitation (P) exceeds the amount necessitated by potential evapotranspiration (PE). It is when the amount of water present in an environment is beyond what it actually needs. In a surplus, the soil is at its field limit and can no longer accommodate the water in excess. The surplus water would instead run off the soil’s surface and be deposited in nearby water sources such as streams. This increases the volume of water in a stream, which in turn would also lead to an increase in discharge. Determining the surplus can aid in predicting the flooding of streams in the area’s vicinity.
Surface run-off occurs when soil has reached its full capacity and can no longer absorb excess water. This water flows over land and drains into nearby water sources. Surface run-off is the result of a surplus of water from precipitation such as rainfall. The excess water can also come from the melting of snow, ice, and glaciers. Surface run-off is one of the most important processes in the water cycle.
An area of land that drains surface run-off into a common point is called a watershed.
Surface run-off that happens before a channel is reached is called a nonpoint source. This water can be contaminated by the various chemicals and materials that it encounters on the way to a water source. Contaminants that can be possibly found in the soil include pesticides, fertilisers, and petroleum. This contaminated runoff water can potentially pollute water supplies with harmful chemicals.
Percolation is described as the downward movement of water into soil. However, percolation is not identical to infiltration. Percolation is merely the first stage of infiltration.
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