NOUS42 KCHS 291000 PNSCHS GAZ087-088-099>101-114>119-137>141-SCZ040-042>045-047>051-301000- PUBLIC INFORMATION STATEMENT NATIONAL WEATHER SERVICE CHARLESTON SC 600 AM EDT TUE MAY 29 2012 ...NATIONAL HURRICANE PREPAREDNESS WEEK CONTINUES... TODAY WE WILL DISCUSS ADDITIONAL HURRICANE HAZARDS INCLUDING FLOODING RAINFALL...TORNADOES AND SURF ZONE IMPACTS SUCH AS RIP CURRENTS...HIGH SURF...AND BEACH EROSION. ...FLOODING RAINFALL... WIDESPREAD TORRENTIAL RAINS...OFTEN EXCEEDING 6 INCHES...CAN PRODUCE DEADLY AND DESTRUCTIVE FLOODS. IN FACT...FRESH WATER FLOODING ACCOUNTS FOR THE MOST DEATHS FROM TROPICAL SYSTEMS. IN 2005...TROPICAL STORM TAMMY PRODUCED BETWEEN 10 AND 15 INCHES OF RAIN AND WIDESPREAD FLOODING ACROSS PORTIONS OF SOUTHEAST GEORGIA. ...TORNADOES... TROPICAL CYCLONES CAN CAUSE TORNADOES IN RAIN BANDS WELL AWAY FROM THE CENTER AS WELL AS NEAR THE CENTER IN AND AROUND THE EYE WALL. IN 2004...THE REMNANTS OF HURRICANE FRANCES...WHICH HAD MADE LANDFALL IN SOUTHEAST FLORIDA...PRODUCED 20 CONFIRMED TORNADOES IN SOUTHEAST SOUTH CAROLINA AND SOUTHEAST GEORGIA. ...RIP CURRENTS/HIGH SURF/BEACH EROSION... TROPICAL CYCLONES...EVEN THOSE THAT REMAIN WELL OFFSHORE...CAN PRODUCE HIGH SURF WHICH IS DANGEROUS TO ANYONE THAT VENTURES INTO THE WATER. THE HIGH SURF CAUSES EXTENSIVE BEACH EROSION AND INCREASES THE RISK OF RIP CURRENTS. RIP CURRENTS ARE NARROW CHANNELS OF WATER WHICH FLOW QUICKLY AWAY FROM LAND AND CAN BE DEADLY...ESPECIALLY FOR INEXPERIENCED SWIMMERS. HIGH SURF ASSOCIATED WITH TROPICAL STORM TAMMY IN 2005 PRODUCED EXTENSIVE BEACH EROSION ALONG THE COAST OF SOUTHERN SOUTH CAROLINA AND SOUTHEAST GEORGIA...AND SEVERAL BEACH HOMES WERE DESTROYED AT EDISTO BEACH. IN ADDITION...HURRICANE EARL IN 2010 CAUSED BREAKERS EXCEEDING 10 FEET AT THE COAST EVEN THOUGH THE STORM REMAINED WELL OFFSHORE. ADDITIONAL INFORMATION CAN BE FOUND ON THE WEB AT THE FOLLOWING ADDRESSES /ALL IN LOWERCASE LETTERS/... NATIONAL HURRICANE CENTER...HTTP://NHC.NOAA.GOV/PREPARE CHARLESTON NATIONAL WEATHER SERVICE...HTTP://WEATHER.GOV/CHS/TROPICAL.SHTML $$