THE AREA WAS ABOUT 100 MILES WIDE AND WAS MOVING TO THE NORTHEAST AT AROUND 25 MPH.

CARRIZO SPRINGS 333 AM CDT TUE MAR 27 2007 . WINTER STORM WARNINGS HAVE
BEEN POSTED FOR A SIGNIFICANT SNOWFALL. STRONG SOUTHERLY WINDS AHEAD OF
A COLD FRONT WILL IMPACT WESTERN UTAH THROUGH NOON. IN THE GUADALUPE
MOUNTAINS.

CORRECTED NATIONAL WEATHER SERVICE SALT LAKE CITY UT 1054 PM MDT MON MAR
26 2007 .

STRONG WINDS ARE ALSO POSSIBLE. VISIBILITIES MAY FALL TO AROUND OR BELOW
3 MILES. AREAS OF FOG WILL CONTINUE. AND WINNFIELD LOUISIANA AROUND 600
AM CDT. SCATTERED SHOWERS WILL CONTINUE TO WEAKEN ACROSS INLAND
SOUTHEAST TEXAS AND CENTRAL LOUISIANA.

THIS PLACES MUCH OF CENTRAL AND NORTHERN UTAH IN A COLD AND MOIST
AIRMASS WHICH COULD PRODUCE A PROLONGED PERIOD OF SNOW TUESDAY NIGHT
THROUGH WEDNESDAY EVENING.

PORTIONS OF SOUTHWEST UTAH. THE STRONGEST WIND WILL OCCUR IN THE TOOELE
VALLEY WHERE GUSTS COULD REACH AROUND 50 MPH.

WHICH IS IN EFFECT FROM WEDNESDAY MORNING THROUGH WEDNESDAY AFTERNOON.
HEAVIER ACCUMULATIONS OF 6 TO 12 INCHES ARE FORECAST FOR THE BENCHES AND
THE WASATCH MOUNTAIN VALLEYS.

EARLY MORNING MOTORISTS SHOULD BE ALERT FOR WET ROADS AND PONDING OF
WATER IN LOW LYING AND POOR DRAINAGE AREAS. WHICH IS IN EFFECT FROM
WEDNESDAY MORNING THROUGH WEDNESDAY AFTERNOON.

MAINLY DURING THE DAYLIGHT HOURS.

GENERALLY ALONG AND EAST OF A JACKSBORO TO GOLDTHWAITE LINE. STRONG MID
LEVEL WINDS AROUND THE BASE OF THIS FEATURE WILL RESULT IN STRONG WINDS
IN THE GUADALUPE MOUNTAINS WEDNESDAY.

HEAVIER ACCUMULATIONS OF 6 TO 12 INCHES ARE FORECAST FOR THE BENCHES AND
THE WASATCH MOUNTAIN VALLEYS.

HIGH WIND WATCH IN EFFECT FROM WEDNESDAY MORNING THROUGH WEDNESDAY
AFTERNOON.

STRONG WINDS EXPECTED IN THE GUADALUPE MOUNTAINS WEDNESDAY.

SHREVEPORT NATIONAL WEATHER SERVICE DOPPLER RADAR INDICATED A LARGE AREA
OF SHOWERS WITH ISOLATED THUNDERSTORMS OVER NORTHEAST TEXAS.

WIND ADVISORY NOW IN EFFECT UNTIL NOON MDT TODAY.

SOME OF THE MODERATE RAIN BANDS WILL PRODUCE BETWEEN ONE-QUARTER AND
ONE-HALF INCH PER HOUR. THE RAIN TODAY IS IN RESPONSE TO AN UPPER-AIR
STORM SYSTEM THAT IS CENTERED OVER FAR SOUTHWEST OKLAHOMA.