Reference (potential) evapotranspiration. II: Frequency distribution in humid, subhumid, arid, semiarid, and mediterranean-type climates

Suat Irmak, M. Gabriela Arellano

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Abstract

While evapotranspiration (ET) has been a subject of research for decades, there is insufficient data, analyses and information on frequency (probability) values and distribution of this important variable for various climatic regions. Frequency distributions of grassreference and alfalfa-reference (potential) evapotranspiration (ETo and ETr) were quantified and analyzed using long-term measured climate datasets for five locations in the United States that have significantly different climatic characteristics [Mediterranean-type climate, Davis, CA (ETo); arid, Phoenix, AZ (ETo); humid/subtropical, Gainesville, FL (ETo); a transition zone between subhumid and semiarid climate, Clay Center, NE (ETr); and a semiarid climate, Scottsbluff, NE (ETr)]. Two Nebraska locations presented higher variability of ETref among all locations because of their highly turbulent climatic characteristics with abrupt changes in wind speed, humidity and air temperature. At Davis, the peak ETo month is July with an average of 7.01 ± 1.33 mm=d. During this time, the probability of ETo was between 6 and 8 mm=d with 78% of probability of occurrence. The peak ETo month in Phoenix is June with a long-term average of 7.37 ± 1.26 mm=d. During this time, there is a 51% probability of ETo being between 7 and 8 mm=d, with a 94% of probability if the range is expanded to 6 and 9 mm=d. For the months with higher precipitation, ETref exhibited more variability atributbale to the erratic rain intensity and frequency (July and August ETo estimates present a standard deviation of 1.45 and 1.58 mm=d, respectively). This rainy season produces high ETo variation. ETo frequency curve in Gainesville had more gradual increase and decrease with much smother fluctuations between the months than any other location. Unlike other locations, there is not a clear peak ETo month in Gainesville; May has the highest long-term average ETo (4.6 ± 1.18 mm=d), but June and July averages present less than 0.4 mm=d of difference than May. For May, the probability of ETo being between 4 and 5 mm=d is 44%. For April and June, the probability of this occurrence is 47 and 34%, respectively. The peak ETr month at Clay Center is June with a long-term average of 7.20 ± 1.89 mm=d. The standard deviation of ETr at Clay Center throughout most of the year is higher than those in other locations with the highest values from April to June. ETr estimations in the peak month (June) are between 7 and 8 mm=d with a probability of occurrence of 18.7%. The peak ETr month in Scottsbluff is July (7.78 ± 1.41 mm=d). During this month, the most likely occurrence in ETr is between 7 and 8 mm=d with a probability of 25%; if the ETr range is expanded from 6 to 8 mm=d, the probability of this ETr range increases to 49%. If another 1 mm is added to the frequency interval, the probability would increase to 63%, showing the substantial variability of ETr in this location as a function of abrupt climatic patterns. The ETo and ETr frequency distribution data and information presented in this study are among the first datasets for various climatic conditions and can be invaluable for water resources and planning and allocation, irrigation management as well as designing irrigation systems and other water resources-related infrastructures.

Original languageEnglish (US)
Article number04015066-1
JournalJournal of Irrigation and Drainage Engineering
Volume142
Issue number4
DOIs
StatePublished - Apr 1 2016

All Science Journal Classification (ASJC) codes

  • Civil and Structural Engineering
  • Water Science and Technology
  • Agricultural and Biological Sciences (miscellaneous)

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