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WEATHER Year-to-date precipitation as of July 16, 2008 totals 11.11 inches. Torrential rains flooded Hereford late the night of June 28th, with 4.99 inches recorded at KPAN. A hailstorm pounded the city late June 8th with golf-ball sized hail common and baseball to softball-sized in northwest Hereford residential neighborhoods. Thousands of vehicles and hundreds of roofs were damaged. NOAA weather radio from the National Weather Service office in Lubbock is available in Deaf Smith County at 162.50 mhz. The Hereford Mesonet site is located adjacent to the City of Hereford Water Supply site just northwest of the city, and current conditions are available here. Located within the cool-temperate climatic zone, Hereford has a dry steppe climate with mild winters. Mean annual total precipitation is 18.06 inches (1938-2006). The climate is continental, characterized by a wide annual range in temperature. Prevailing winds are south to southwesterly throughout the year although northerly winds are frequent in the colder months. Strong winds will occasionally result in blowing dust, with the strongest sustained winds occurring with the greatest frequency in March and April. Precipitation occurs most frequently in the form of thunderstorms. Monthly and annual totals are extremely variable, with 78% of the mean annual precip falling within the 6-month period, May through October. Monthly rainfall total decrease significantly during the colder season as frequent "northers" cut off the supply of moisture from the Gulf of Mexico. During the colder seasons temperatures also show extreme variability. Cold fronts from the northern Great Plains sweep across the level Panhandle plains at speeds up to 40 miles-per-hour. Temperature drops of 50 to 60 degrees within a 12-hour period have occurred, following the passage of these fast-moving "northers". In spite of occasional near-zero temperatures, winters in Hereford are actually mild when compared to those of the northern Great Plains. Cold spells rarely last longer than 2 or 3 days before southwesterly winds from the high New Mexican plateaus cause rapid warming. The dry air, high elevation and usually clear skies are ideal for insolation and radiational cooling; consequently, there is a large daily range between maximum and minimum temperatures. Hereford is located in the area of highest wind potential in Texas, with sustained winds over 30 mph evident on many days in the fall, winter and spring. Although on the western edge of "tornado alley", tornadoes in the F-4 range have occurred infrequently in the western Panhandle.
Mean annual snowfall is 13 inches, but seasonal amounts vary over a wide range. A few exceptionally heavy snows create a bias in the data and make the arithmetic mean a poor estimate of expected snowfall. An even snow cover is very unusual since strong winds often accompany snowfalls. The snowiest winter on record was 1982-83, when KPAN recorded 51.5 inches of snow. There were two stretches of 12 days each that snow remained on the ground during that December, January and February. During the blizzard of February 1-5, 1956, snow fell to a depth of 26.5 inches at Hereford. Hereford is at elevation of 3840 feet above sea level, at latitude 34 degrees 48 minutes north, 102 degrees 28 minutes west. While mid-afternoon temperatures are sometimes hot in summer, the high altitude and low humidity result in exceptionally pleasant weather during this season. Temperatures drop rapidly after sunset, and mid-summer minima are in the low 60s. Hereford receives about 74% of the total possible sunshine annually. The mean length of the growing season (freeze-free period) is 195 days. Average last date of a freeze in the spring is April 20, and average first date of a freeze in the fall is October 22. Hereford typically experiences temperatures above 100 degrees and below zero each year. Weather Observation History Rainfall and temperature observations began in Hereford in January 1905 and continued through April 1912, according to the National Weather Service. No records are available from that date until a station was established 3 blocks north of the post office on September 11, 1936. On August 20, 1942 the equipment was moved to a site on the lawn at the City Hall, 3 blocks southwest of the post office (at the current location of Dudley Bayne Park). The observing station was moved to the Holly Sugar Plant on November 11, 1964, three miles west of the post office. KPAN became the NOAA Cooperative Weather Observer on February 13, 1981, with instruments located adjacent to the studios at 218 East Fifth.
Precipitation Records - Annual Totals 1938 - 21.37 1958 - 24.31 1978 - 22.22 1939 - 16.84 1959 - 21.46 1979 - 15.29 1940 - 11.90 1960 - 27.92 1980 - 14.51 1941 - 38.95 1961 - 14.46 1981 - 21.58 1942 - 21.5 1962 - 18.02 1982 - 17.29 1943 - 18.0 1963 - 20.93 1983 - 15.53 1944 - 17.62 1964 - 11.47 1984 - 20.69 1945 - 12.26 1965 - 19.89 1985 - 24.74 1946 - 15.88 1966 - 13.68 1986 - 30.56 1947 - 15.2 1967 - 15.78 1987 - 24.90 1948 - 17.97 1968 - 18.0 1988 - 18.22 1949 - 26.19 1969 - 22.5 1989 - 14.65 1950 - 21.79 1970 - 9.3 1990 - 12.36 1951 - 16.87 1971 - 23.0 1991 - 24.47 1952 - 13.54 1972 - 15.6 1992 - 22.17 1953 - 14.54 1973 - 18.0 1993 - 18.34 1954 - 13.07 1974 - 23.1 1994 - 16.98 1955 - 10.01 1975 - 21.0 1995 - 15.36 1956 - 7.71 1976 - 18.19 1996 - 16.26 1957 - 15.70 1977 - 13.83 1997 - 21.76 1998- 16.53 1999-29.11 2000 - 16.91 2001- 17.05 2002-15.40 2003 - 13.36 2004 - 36.64 2005-16.62 2006 - 19.20 2007 - 20.91 Links: National Weather Service-AMA NWS-LUB Bootleg Weather Site West Texas Mesonet
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