potential evapotranspiration वाक्य
उदाहरण वाक्य
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- However, observations revealed that actual evaporation was 1.26 times greater than potential evaporation, and therefore the equation for actual evaporation was found by taking potential evapotranspiration and multiplying it by \ alpha.
- "' Potential evaporation "'or "'potential evapotranspiration ( PET ) "'is defined as the amount of evaporation that would occur if a sufficient water source were available.
- It recognizes the significance of temperature in allowing colder places such as northern Canada to be seen as humid with the same level of precipitation as some tropical deserts because of lower levels of potential evapotranspiration in colder places.
- Potential evapotranspiration is usually measured indirectly, from other climatic factors, but also depends on the surface type, such as free water ( for lakes and oceans ), the soil type for bare soil, and the vegetation.
- The only source of water in the warm deserts is an oasis; this creates an arid climate in the area distinguishable by the lack of moisture in the soil due to annual precipitation being less than half of the annual potential evapotranspiration.
- Rainfall and snowfall are generally slight due to the low vapor pressure of water in the chilly atmosphere, but as a rule potential evapotranspiration is extremely low, allowing soggy terrain of swamps and bogs even in places that get precipitation typical of deserts of lower and middle latitudes.
- Where the water deficiency d is calculated as the sum of the monthly differences between precipitation and potential evapotranspiration for those months when the normal precipitation is less than the normal evapotranspiration; and where n stands for the sum of monthly values of potential evapotranspiration for the deficient months ( after Huschke, 1959 ).
- Where the water deficiency d is calculated as the sum of the monthly differences between precipitation and potential evapotranspiration for those months when the normal precipitation is less than the normal evapotranspiration; and where n stands for the sum of monthly values of potential evapotranspiration for the deficient months ( after Huschke, 1959 ).
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