In order to maintainEarth'swater balance, evaporation exceeds precipitation over oceans.
Evaporation exceeds precipitation.
Because this would only occur at a regional scale. Water from elsewhere would move in to replace the miniscule amount that was evaporated. This way, sea level is roughly in balance in terms of evaporation and precipitation.
When precipitation exceeds evaporation, there will be an accumulation of water in the environment, leading to increased levels of surface water bodies such as rivers, lakes, and groundwater. This excess water can potentially result in flooding and waterlogging in certain areas.
Its not actually called a type of a climate but it actually creates snow and in regions like southern Manitoba, Saskatchewan and Alberta, the evaporation exceeds precipitation.A desert.
it is called desert because there is high level of sunshine and of course evaporation with little rain.
The deserts biome is an example where evaporation rates often exceed precipitation rates. These regions receive limited rainfall, resulting in higher evaporation due to the intense heat and lack of moisture in the air.
Deserts receive less tha 10 inches (250mm) of precipitation per year. Deserts have an evaporation rate that far exceeds the precipitation rate.
Arid and semiarid climates typically occur in regions where precipitation is less than potential evaporation, leading to water scarcity. However, when precipitation exceeds potential evaporation, it can result in wetter conditions that may support more vegetation and diverse ecosystems, often classifying the area as semi-humid or humid. Such regions can experience seasonal variations, where periods of higher rainfall can temporarily alleviate aridity, but the overall climate remains influenced by the surrounding arid conditions. Thus, while precipitation may exceed evaporation at times, the long-term climate classification is determined by the overall balance between these factors.
The Mojave receives less than 10 inches of rain on average per year and the evaporation rate exceeds the precipitation rate. Both are descriptions of a desert.
Large deposits of rocks formed by evaporation, such as salt deposits, typically form in arid or desert climates where the rate of evaporation exceeds the rate of precipitation. The lack of rainfall allows water to evaporate leaving behind concentrated mineral deposits.
When precipitation exceeds evaporation, it leads to an increase in water availability in the environment. This surplus water can result in the saturation of soil, leading to surface runoff, which may contribute to flooding in low-lying areas. Additionally, ecosystems may thrive due to the added moisture, but prolonged excess can disrupt habitats and impact water quality.
When precipitation exceeds potential evaporation, soil moisture levels are likely to increase. The excess water from precipitation saturates the soil, leading to higher moisture content and potentially contributing to groundwater recharge. If the soil reaches saturation, excess water may also result in surface runoff. This condition can enhance plant growth, as more moisture is available for uptake.