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An Air Force Hurricane Hunter aircraft found no evidence of a closed circulation center, [18] and radar from Martinique found no little to no circulation within the bursts of convection. [19] Thus, at 12:00 UTC on July 8, Beryl degenerated into an open trough while located just 60 miles northeast of Martinique. [1]
Hoy No Circula (literally in Spanish: "today [your car] does not circulate", known as No-drive days) is the name of an environmental program intended to improve the air quality of Mexico City. A similar coordinated program operates within the State of México , which surrounds Mexico City on three sides.
Each Air Region is composed of Headquarters, Air Force Bases, Air Force Stations, and other organizations. The Air Force divides the country's territory into four regions: Northwestern ( Mexicali , Baja California ), Northeastern ( Chihuahua , Chihuahua ), Central ( Mexico City ) and Southeastern ( Tuxtla Gutiérrez , Chiapas ); each region is ...
An area of low pressure detached from a frontal zone on August 4 and moved southwestward. After developing a minimal amount of deep convection, an Air Force Reserve Command reconnaissance aircraft found a well-defined low-level circulation on August 8. The depression then moved westward without intensifying for two days.
Much of the US plunged into cold air. A brutally cold blast of Siberian air has caused temperatures to plummet 20 to 30 degrees below normal from the Canadian border to the Mexican border and ...
Beryl made landfall in a sparsely populated region of northeast Mexico, so no official reports of tropical storm force winds were recorded. [1] Moisture from Beryl brought 0.8 in (20 mm) of rain in Corpus Christi , Texas and 0.5 in (13 mm) in Brownsville, Texas in a 48-hour period between August 14 and August 16.
Aug. 4—A decision by the U.S. Air Force to pull a special operations squadron out of Cannon Air Force Base in Eastern New Mexico has raised hackles from residents in nearby Clovis, where the ...
It originates from eastern Mexico and the Bay of Campeche as a post-frontal northerly wind, accelerated southward by cold air damming, that crosses the isthmus and blows through the gap between the Mexican and Guatemalan mountains. The term dates back to at least 1929. [1] This wind can reach gale, storm, even hurricane force.