Dryland farming systems use only rainfall and snowmelt for water. In areas with less predictable rainfall, farmers use irrigation. The farmers can control the amount of soil moisture available at any given time, but this comes with the cost to irrigate and the risk to deplete aquifers.
Hydrology
Soil moisture is considered the water stored in the soil in the “vadose zone.” This is the layer of soil which has a mixture of soil air and water usually ranging from the surface to 1 m (3’) deep, depending on your location.
The two extremes of soil moisture status are drought and flood. When the soil moisture falls below the wilting point of the local plants, they start to wilt and die, leading to drought conditions which is less than desirable. Drought conditions can lead to wind erosion, if plant life dies off and leaves the soil exposed.
The other extreme is when the soil reaches saturation. Water can start to flow over the surface instead of down into the soil. When this combines with rainfall, flooding can occur. New water has nowhere to go but across the land. Flooding can also occur when water in the soil is frozen. Sometimes flooding occurs when the soil just cannot soak up (infiltrate) heavy rainfalls. Flooding influences the water erosion of the soil, by overland flow.
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