What is the TXHPET Network?
The Texas High Plains ET Networks (North Plains and South Plains networks) were established in the 1990’s to provide convenient and timely access to agriculturally based meteorological data for use by producers, agricultural researchers, and others interested in agriculturally relevant meteorological data.
The Texas High Plains Evapotranspiration Network is the result of intensive collaboration and cooperation between the North Plains Evapotranspiration Network and the South Plains Evapotranspiration (ET) Network. The Texas North Plains and South Plains ET Networks are comprised of meteorological stations located throughout the Texas North Plains and South Plains region. The two networks have been effectively combined to form the Texas High Plains ET Network. Under the combined operations, the TXHPET operates 18 meteorological stations located in 15 Texas counties, and regional coverage is estimated at four million irrigated acres. Additional meteorological stations, representing a substantial increase in area coverage, may be added to the TXHPET network in the future. The network disseminates meteorological data, including ET-based crop water use information used by agricultural producers and consultants in irrigation scheduling, on a daily basis. Currently, these data are disseminated primarily through fax and / or on-line web access to over 825 data users per day (approx. 300,000 downloads and faxes annually).
Bushland (JBF)Chillicothe
Dalhart
Dimmitt
Earth
Etter
Farwell
Halfway
Lamesa
Lockney
Lubbock
Morse
Munday
Pecos
Perryton
W.T. Feedlot
Wellington
White Deer

What is evapotranspiration (ET)?
Evapotranspiration is a term that describes crop or plant water demand by combining evaporation and transpiration. Evaporation is the process through which water is removed from moist soil and wet surfaces (such as dew on leaves). Transpiration is the process through which water is drawn up through the plant (roots extract water from the soil, and water is eventually removed through stomata on the leaves.) ET is an estimate of crop water demand and is driven primarily by meteorological conditions, including air temperatures, humidity, solar irradiance and wind. These data are acquired through use of specially equipped meteorological "weather" stations. Strategically located meteorological stations comprise the ET networks. Data from these stations are applied to an ET model (equation) to calculate reference crop (well watered grass or alfalfa) ET.
What is Reference ET (PET)?
Reference crop evapotranspiration, also referred to as Potential Evapotranspiration (PET), is an estimate of water requirement for a well watered reference crop. This reference crop (grass or alfalfa) is essentially an idealized crop used as a basis for the ET model. Reference ET is calculated by applying climate data (temperature, solar radiation, wind, humidity) in a model (equation). It is helpful to note that reference ET is only an estimate of the water demand for this idealized crop, based upon weather station data at a given location. The Texas High Plains ET Network uses an idealized grass reference crop.



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