potential evapotranspiration वाक्य
उदाहरण वाक्य
मोबाइल
- The difference between potential evapotranspiration and precipitation is used in irrigation scheduling.
- In these conditions, the actual evapotranspiration would match the Penman rate of potential evapotranspiration.
- Precipitation is well in excess of potential evapotranspiration, except for about a month in midsummer.
- The average annual precipitation is about 635 mm, while annual potential evapotranspiration is about 1623 mm.
- Where PET is the potential evapotranspiration and P is the average annual precipitation ( UNEP, 1992 ).
- Potential evapotranspiration supplements the measurement of precipitation in providing a scientific measurement-based definition of a desert.
- If potential evapotranspiration is greater than actual precipitation, then soil will dry out, unless irrigation is used.
- This allows for both actual and potential evapotranspiration to be calculated on a pixel-by-pixel basis.
- The increased drought risk is attributed to a combination of increased temperature and potential evapotranspiration not being balanced by precipitation.
- Potential evapotranspiration, then, is the amount of water that " could " evaporate in any given region.
- Potential evapotranspiration ( PET ) is the amount of water that would be evaporated and transpired if there were sufficient water available.
- Often a value for the potential evapotranspiration is calculated at a nearby climate station on a reference surface, conventionally short grass.
- This value is called the reference evapotranspiration, and can be converted to a potential evapotranspiration by multiplying with a surface coefficient.
- The mid-latitude steppes can be summarized by hot summers and cold winters, averaging of potential evapotranspiration must also be taken into account.
- Potential evapotranspiration ( PET ), is the evaporation and transpiration that potentially could occur if a field of the crop had an ideal unlimited water supply.
- Potential evapotranspiration is also higher on windy days because the evaporated moisture can be quickly moved from the ground or plant surface, allowing more evaporation to fill its place.
- Water deficiencies and extended periods of drought are uncommon, and much of the region has a positive water balance ( i . e . the precipitation exceeds the potential evapotranspiration ).
- Potential evapotranspiration is higher in the summer, on less cloudy days, and closer to the equator, because of the higher levels of solar radiation that provides the energy for evaporation.
- Kimba is located within a dry ( arid and semi arid ) climate zone ( Koppen classification " BSh " ), where precipitation is less than the total potential evapotranspiration.
- Precipitation in the Puna region averages less than a year while potential evapotranspiration ranges from a year, owing to the high insolation, strong winds, and low humidity that exacerbates the dry conditions.
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