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A dry line (also called a dew point line, or Marfa front, after Marfa, Texas) [1] is a line across a continent that separates moist air and dry air. One of the most prominent examples of such a separation occurs in central North America, especially Texas, Oklahoma, and Kansas, where the moist air from the Gulf of Mexico meets dry air from the ...
August 1, 2022 at 6:48 AM. Water levels in wells across Texas are running low because of the extreme drought, groundwater experts say. Drought conditions in the state are getting worse by the week ...
The dry line is the boundary between dry and moist air masses east of mountain ranges with similar orientation to the Rockies, depicted at the leading edge of the dew point, or moisture, gradient. Near the surface, warm moist air that is denser than warmer, dryer air wedges under the drier air in a manner similar to that of a cold front wedging ...
An annotated surface weather analysis of northwestern Texas at 7:00 p.m., showing where storms (shaded in red) developed along the dry line (brown scalloped line). [6]The Severe Local Storms Unit (SELS) within the National Severe Storms Forecast Center (NSSFC) of the United States Weather Bureau – tasked with issuing daily outlooks projecting possible severe weather over the U.S. – did not ...
Abnormally warm temperatures, dry grasses, and a sudden windy cold front combined to create the conditions for the destructive wildfires that have raged across parts of Texas this week.
The dry line normally moves eastward during the day and westward at night. A dry line is depicted on National Weather Service (NWS) surface analyses as an orange line with scallops facing into the moist sector. Dry lines are one of the few surface fronts where the pips indicated do not necessarily reflect the direction of motion. [18]
1950s Texas drought. The 1950s Texas drought was a period between 1949 and 1957 in which the state received 30 to 50% less rain than normal, while temperatures rose above average. During this time, Texans experienced the second-, third-, and eighth-driest single years ever in the state – 1956, 1954, and 1951, respectively. [1]
The highest temperature ever measured in Texas was 120 °F (48.9 °C), recorded on August 12, 1936 in Seymour, during the 1936 North American Heatwave, and again on June 28, 1994 in Monahans. The lowest temperature ever measured in Texas was −23 °F (−30.6 °C), recorded on February 8, 1933 in Seminole. [27] Climate data for Texas.