000 FGUS51 KLWX 061348 RVDLWX DCZ001-MDZ001-003-004-009-501-502-VAZ025>031-038>042-050-051- 055-056-WVZ050>055-501>504-061800- DAILY RIVER AND LAKE SUMMARY NATIONAL WEATHER SERVICE BALTIMORE MD/WASHINGTON DC 948 AM EDT MON JUL 06 2009 THE FRONTAL SYSTEM SLIPPED OFF THE COAST OVERNIGHT...RAINFALL AMOUNTS THIS MORNING WERE OF NONE TO AROUND AN TENTH OF AN INCH IN THE NORTH AND MORE SO OVER THE SOUTH WITH AMOUNTS OF ONE HALF TO THREE QUARTERS OF AN INCH OF RAIN. HIGH PRESSURE WILL BUILT IN FROM THE NORTHWEST. TODAY WILL BE DRY AND SEASONABLE. GENERALLY MINOR STAGE CHANGES ARE EXPECTED ACROSS THE BASINS THROUGH WEDNESDAY. SOME MINOR RISES WILL OCCUR ALONG THE MIDDLE AND LOWER JAMES BASIN IN RESPONSE TO SUNDAY'S RAINFALL. $$ .B WBC 0706 E DC200907060940 DH07/HG/DRH+24/HGIFF/DRH+48/HGIFF/ : : STATION FLOOD 7-8AM 24-HR 7-8AM : ID NAME STAGE STAGE CHANGE FORECASTS : TUE WED : RAPPAHANNOCK BASIN RENV2 :REMINGTON 15.0: 3.4/:-0.01: 3.3 / 3.3 / CLPV2 :CULPEPER 14.0: 1.1/: 0.02: 1.1 / 1.1 / : : POTOMAC & SHENANDOAH BASINS CBEM2 :CUMBERLAND 17.0: 2.8/:-0.01: 2.8 / 2.8 / PETW2 :PETERSBURG 13.0: 3.4/: 0.01: 3.4 / 3.3 / SPRW2 :SPRINGFIELD 15.0: 1.8/:-0.02: 1.8 / 1.8 / PAWW2 :PAW PAW 25.0: 4.5/:-0.07: 4.4 / 4.4 / HNKM2 :HANCOCK 30.0: 3.5/:-0.09: 3.4 / 3.4 / MILW2 :MILLVILLE 13.5: 2.2/:-0.05: 2.1 / 2.1 / BRKM2 :LITTLE FALLS 10.0: 3.2/:-0.05: 3.2 / 3.2 / .END .B WBC 0706 DH12/TW : RIVER WATER TEMPERATURES WLLM2 :WILLIAMSPORT MD 79 DCKM2 :DICKERSON MD 76 BRKM2 :LITTLE FALLS MD 75 MGTM2 :MORGANTOWN MD 72 : :WATER CONDITIONS ABOVE HARPERS FERRY ARE CLEAR. .END THESE FORECASTS DO NOT TAKE INTO ACCOUNT FLUCTUATIONS CAUSED BY CHANGES IN RESERVOIR RELEASES. FORECASTS INCLUDE ALL PRECIPITATION THROUGH 7AM TODAY, PLUS THE EFFECTS OF PROJECTED PRECIPITATION THROUGH THE FOLLOWING 48 HOURS. DURING PERIODS OF HIGH WATER OR FLOODING...CREST FORECAST UPDATES CAN BE OBTAINED IN RIVER FLOOD WARNINGS (WBCFLWLWX) AND RIVER FLOOD STATEMENTS (WBCFLSLWX). UPDATED HYDROLOGIC INFORMATION CAN ALSO BE OBTAINED FROM OUR WEB PAGE AT HTTP://WWW.ERH.NOAA.GOV/LWX $$