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THE
SOUTHWEST MONSOON IN SOUTHERN NEW MEXICO AND FAR WESTERN TEXAS by John Park and Joe Rogash NWS El Paso |
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![]() A thunderstorm with heavy rains and strong winds moves across El Paso Texas (photo by John Fausett). |
![]() This thunderstorm, photographed from El Paso, produced flash flooding further east over Hudspeth County, Texas. Most flash floods over southern New Mexico and far western Texas occur during the late afternoon and evening. ( Photographed by John Fausett) |
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The climate of the southwestern United States, including southern New Mexico
and far western Texas, is considered semi-arid or desert, since compared
to most areas of the country, this region has abundant sunshine and
little rainfall. El Paso, Texas is called the "Sun City" for
good reason; according to solar radiation statistics it is the fifth
sunniest city in the United States, receiving 83% of the possible
sunshine. And in most years, from October through the middle of June, the
threat of heavy rainfall is low because during this period the
prevailing wind flow across the southwestern United States is from west
to east. As a result, most of the moisture from the Pacific Ocean is
blocked by the mountains to the west while moisture from the Gulf of
Mexico is literally blown far to the east. This circulation pattern keeps the weather mostly sunny, warm and dry from
early autumn
through early summer. This pressure field generates southeasterly and
southerly winds in the lower and sometimes middle layers of the
atmosphere, which transport moisture from the Gulf of Mexico and Gulf of
California into southern New Mexico and far western Texas. The increase
in moisture, combined with the usual warm temperatures, produces an
unstable air mass favorable for thunderstorms which may generate flash
flooding, hail, damaging winds and even an isolated tornado. |
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