makes for stressful prep I would imagine - keeping you all in our good thoughts
https://twitter.com/iembot_akq
Mesoscale Precipitation Discussion 0813 NWS Weather Prediction Center College Park MD 1138 AM EDT Sun Sep 09 2018
Areas affected...Virginia Tidewater, Lower Eastern Shore
Concerning...Heavy rainfall...Flash flooding likely
Valid 091536Z - 092130Z
Summary...Thunderstorms and heavy rain showers are likely to persist around the Lower Chesapeake Bay region through much of the day, including the Virginia Tidewater and Lower Eastern Shore. These showers and storms may be nearly stationary at times, and may produce localized extreme rain rates. Although flash flooding may not be widespread, localized flash flooding is expected where stalling storms occur.
Discussion...Surface observations revealed a surface wave or weak low in the vicinity of Wakefield VA, with a complete circulation evident in the wind field. This was forming along an existing quasi-stationary front. From the mouth of the Chesapeake east into the Atlantic, strong, confluent, low-level easterly flow was developing along and north of the surface front, which was leading to a highly focused area of low-level moisture flux and convergence that was maximized in the Tidewater region near and northeast of the surface low. The inflow region was also characterized by precipitable water values over 2 inches, and increasing instability with MLCAPE approaching 2000 j/kg. The RAP forecasts show the surface wave/low slowly drifting north through the day, which should lead to a relatively steady-state mesoscale setup with abundant unstable, moist inflow arriving into a region with significant low-level convergence. This favors continued convective activity into the afternoon hours.
The convergence does not seem to be manifesting as a single, dominant band, but instead is being modified by the shape of the coastline and maximized in very localized areas. There is some evidence of this in the highly variable storm motions on the KAKQ radar at the moment, some quite different from the background mean flow vectors or even Corfidi/Bunkers storm motion vectors. The convection generally seemed to be either anchored on low-level convergence maxima or showing different storm motion along a low-level boundary. This should generally continue into the afternoon hours, with convection anchored at times at points along the complex coastline, perhaps initially in the Tidewater Region, and eventually migrating north with the surface low toward the Northern Neck, Middle Peninsula, and Lower Eastern Shore on the southern portion of the Delmarva Peninsula.
MRMS and KAKQ dual pol radar estimates have shown rain rates occasionally getting as high as 3 in/hr with nearly stationary storms, although some of them have been just over adjacent marine areas. The 12Z HREF neighborhood probability of 3+ inch per hour rain rates generally exceeds 30 percent on most of the daytime hours in some part of the region. And the HREF localized probability matched mean, and recent runs of the operational HRRR, show localized extreme rainfall totals approaching 10 inches by 00Z. Whether totals this high could occur is not certain, the convection at the moment is rather limited in size, and the models may be unable to resolve the very small nature of the convective cells. Nevertheless, there is a strong model signal for locally extreme rainfall rates (3+ in/hr) and that has been supported by radar estimates in real time. These would be more than sufficient to create flash flooding. Whether significant totals can materialize in one or two areas remains to be seen, but is at least a possibility.
Lamers
ATTN...WFO...AKQ...LWX...
ATTN...RFC...MARFC...SERFC...
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