FGUS71 KRNK 170059 ESFRNK NCC005-009-033-157-169-171-189-193-197-VAC005-009-011-017-019-021- 023-029-031-035-037-045-063-067-071-077-083-089-121-141-143-155- 161-163-173-185-197-530-580-590-640-678-680-690-750-770-775- WVC025-055-063-089-240100- Winter/Spring Flood Potential Outlook National Weather Service Blacksburg VA 859 PM EDT Thu Mar 16 2023 ...Winter/Spring Flood Outlook...Number 6 ...River Flood Potential is Near Average/Normal... Each winter and early spring, the National Weather Service office in Blacksburg, Virginia issues a series of routine flood potential outlooks. These outlooks estimate the potential for river flooding (not flash flooding) across the Blacksburg Hydrologic Service Area (HSA). The HSA includes 40 counties covering parts of southwest Virginia, far northwest North Carolina, and far southeast West Virginia. Major river basins in the HSA include all or parts of the New, Greenbrier, Tennessee, James, Roanoke, Dan, and Yadkin. This outlook is based on the current assessment of hydrometeorological factors which contribute to river flooding. These factors include but are not limited to recent precipitation, soil moisture, snow cover and snow water equivalent, streamflows, river ice, and expected future weather conditions. In this part of the southern Appalachian and Mid Atlantic region, heavy rainfall is the primary factor that leads to river flooding. Heavy rainfall can rapidly cause river flooding at any time of the year even when overall river flood potential is considered low. Snowmelt can contribute to the flooding as it did dramatically in January 1996 when rain on top of rapid snowmelt produced record flooding throughout parts of the Mid Atlantic region, including the Greenbrier River. Flood Potential Outlook: For the Blacksburg HSA, the river flood potential is near average/normal for the next two weeks (through March 30). Precipitation over the winter has been frequent, making for streamflows and soil moisture mainly in the normal range. More recently, the passage of multiple low pressure systems during the middle of February resulted in rounds of prolonged and some- times heavy precipitation, as well as minor river flooding in the New, the upper James and the Clinch basins. Since then however, precipitation has been below normal for most of the HSA, resulting in decreased stream flows and soil moisture. Remaining snow cover is hydrologically insignificant to produce river flooding, and no frozen ground or river ice exists within the HSA. Streamflows and soil moisture are generally in the normal range. There are no storms systems expected within the next 7 days that will be capable of producing river flooding, though precipitation in the 6-10 and the 8-14 day periods are expected to be above normal. Current Flooding: There is no flooding occurring or forecast at this time. Recent Precipitation: Precipitation through the month of March has generally been below-normal for most of the HSA, particularly for portions of the southern Piedmont of Virginia, where precipitation totals have ranged from 0.75 to 1.0 inches, or between 20 to 30 percent of normal. Only localized area have received above-normal precipitation during the month, particularly along the crest of the Blue Ridge and portions of the New River Valley, each of which has received amounts ranging from 100 to 150 percent of normal. During February, rainfall ranging from one quarter to two-thirds of an inch was observed on February 1-2. On February 11-12, a deep low pressure system triggered widespread precipitation ranging from 1.5 to 2.5 inches, which brought several rivers to near- bankfull. This was followed by 1.5 to 2.5 inches of rainfall on February 16-17 from the Alleghany Highlands through southeast West Virginia and western Virginia that resulted in minor flooding along portions of several rivers, including the Clinch, the Bluestone, the East, the Cowpasture and the Greenbrier Rivers. Only modest precipitation was observed through the remainder of the month. For January 2023, precipitation ranged between 2 to 3 inches across the mountains north of Highway 460, and between 3 and 5 inches elsewhere within the HSA. Looking at the extremes, the driest area was the upper James basin, with amounts that were less than 75 percent of normal, while pockets of the Roanoke and Dan River basins recorded amounts that were over 125 percent of normal. Precipitation elsewhere within the HSA was within 25 percent of normal. Precipitation events were light in intensity through the month and usually spaced 1-3 days apart. Nearly all precipitation fell in the form of rain. No flooding was reported. For December 2022, precipitation fell mainly in the form of rain, and ranged between 3 and 5 inches for the eastern three quarters of the HSA. These amounts were anywhere between 75 and 125 percent of normal. The western-most quarter of the HSA was driest, which includes the mountains from western Greenbrier County through Watauga County, where only 2 to 3 inches of precipitation were observed. These amounts were anywhere between 50 and 75 percent of normal. Drought: The March 14, 2023 rendition of the weekly U.S. Drought Monitor (issued March 16) indicates no drought or abnormally dry conditions anywhere within the HSA. Please visit the www.droughtmonitor.unl.edu/ for access to the drought maps and additional information. Snow cover: The only snow cover remaining within the HSA is confined to the higher ridgetops of mainly the New River basin, from southeast West Virginia to the Highlands of North Carolina. The remaining snow cover is hydrologically insignificant however, with depths of 2 inches or less as of the morning of March 16. Snow depth continues to diminish rapidly. Please visit www.nohrsc.noaa.gov for detailed information on snow cover and snow water equivalent. River ice: There is currently no river ice anywhere within the HSA at this time. Streamflows: Average streamflows for much of the HSA are in the normal range at the 7-, 14-, and 28-day timeframes. The exception is for locations east of the Highway 29 corridor of central Virginia, as well as portions of the upper James River basin, where streamflows are slightly below-normal for those same timeframes. For more detailed information on streamflow conditions see the USGS WaterWatch website: https://waterwatch.usgs.gov Soil Moisture: Per the Climate Prediction Center, soil moisture across nearly all of the HSA is near-normal, with localized areas where moisture is slightly below-normal. For additional soil moisture information see: http://www.cpc.ncep.noaa.gov Reservoirs: Major water supply reservoirs including John H. Kerr, W. Kerr Scott, Philpott Lake, Lake Moomaw, Smith Mountain Lake, and the Western VA Water Authority reservoirs near Roanoke are near full capacity and guide curves where applicable. Future Weather Conditions: Precipitation amounts through March 23 are expected to be 0.50 inch or less across most of the HSA, with locally higher amounts possible. The WPC Quantitative Precipitation Forecast is updated frequently and is available at: www.wpc.ncep.noaa.gov/#page=qpf The 6 to 10 day outlook from the NWS Climate Prediction Center during the period March 21-25 indicates a weather pattern where temperatures are favored to be below-normal, while precipitation is favored to be above-normal. The 8 to 14 day outlook from March 23-29 indicates a weather pattern where temperatures are likely to be near-normal, and precipitation is favored to be above-normal. Probabilistic/Ensemble river forecasts: The Meteorological Model Ensemble River Forecasts (MMEFS) valid through about March 25 indicate that all rivers will remain below bankfull, although within-bank rises are likely. Ensemble river forecasts (MMEFS) are available at: www.weather.gov/erh/mmefs Summary: Flood Potential Outlook: For the Blacksburg HSA, the river flood potential is near average/normal for the next two weeks (through March 30). Next issuance: This is expected to be the final winter/spring flood potential outlook of the 2023 season. For additional hydrologic or weather information, visit our website at www.weather.gov/blacksburg. $$ NF/WP $$