Water is held in the soil and seeps out over time.
Earth/soil holds water depending on its absorbancy ('sponginess'). Even though the ratio of the volume of water seeping out from a volume of soil is generally quite small, it is compounded by the catchment area of the stream - and hence there is a flow of water in the stream for some time after precipitation.
The amount of water in a stream is a factor of the the amount of water being released by the soil, depth of soil, whether there is a non-permiable layer undergound that feeds the catchment, the size of the catchment and amount of recent precipitation.
You could experiment to create streams of different water flow long after precipitation by filling in a valley between two mountains with various types of clay, soil, gravel, sand etc and notice the difference of stream flow in each case after precipitation. Of course, such an exercise would take many months/years to undertake and many millions, if not billions of dollars. There might also be government legislation and local environmental groups who might oppose such an activity.
true!!
Ephemeral streams only have water for a brief time following rain or during periods of spring runoff from higher, surrounding mountains.
Ephemeral
Wadi
During non-storm periods, groundwater can help maintain streamflow by continuing to discharge into the stream. This base flow sustains streamflow levels even when there is no additional surface runoff from precipitation. Groundwater acts as a consistent source of water for streams, rivers, and other bodies of water, ensuring a steady flow throughout the year.
Wadi
During a prolonged drought, the volume of water that passes from groundwater to streams decreases. This is because there is less water available in the groundwater system due to reduced recharge from precipitation. As a result, streams receive less water from groundwater, leading to lower streamflow levels.
Intermittent streams are watercourses in arid areas that flow only during or shortly after precipitation events. These streams often appear and disappear suddenly as they are primarily fed by rainwater and can dry up quickly when there is no rainfall. They play a crucial role in arid ecosystems by supporting wildlife and vegetation during times of water scarcity.
Long periods of unusually low precipitation are called droughts. Droughts can have significant impacts on agriculture, water supply, and ecosystems, leading to food shortages and environmental stress. They are typically defined by the duration and severity of the precipitation deficit relative to normal conditions for a particular region. Monitoring and managing water resources is crucial during such periods to mitigate the effects of drought.
Basal flow refers to the slow movement of water through the ground or surface flow in a river during periods of low precipitation. It is typically more consistent than flashy flow, which occurs during heavy rain events. Basal flow plays a critical role in maintaining streamflow during dry periods.
Groundwater depletion can lower the water table, leading to reduced base flow in streams. This decrease in base flow can impact stream ecosystems, aquatic life, and water quality. Additionally, it can increase the risk of stream drying up during dry periods.
Wind velocity is typically the greatest during a storm or during periods of strong pressure gradients, such as in areas of low pressure systems or jet streams. These conditions can lead to higher wind speeds due to the increased movement of air masses.