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From | To | Subject | Date/Time | |||
COD Weather Processor | wx-storm | HVYRAIN: Excessive Rainfall Discussion |
July 17, 2019 9:02 AM * |
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This is a multi-part message in MIME format... ------------=_1563354191-51656-12255 Content-Type: text/plain FOUS30 KWBC 170902 QPFERD Excessive Rainfall Discussion NWS Weather Prediction Center College Park MD 502 AM EDT Wed Jul 17 2019 Day 1 Valid 12Z Wed Jul 17 2019 - 12Z Thu Jul 18 2019 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL ACROSS PORTIONS OF THE UPPER MS VALLEY, THE NORTHERN MID ATLANTIC INTO SOUTHERN NEW ENGLAND, AND NORTHERN ALABAMA... ...TN and OH Valley into the northern Mid Atlantic and southern New England... Post-Tropical cyclone Barry will continue moving east northeast across the OH Valley today and into PA by tonight. Plenty of moisture still associated with this system, with an expanse of PWs greater than 2" along and to its east. The best coverage of convection today will likely be along and northeast of Barry from portions of OH, into PA, southern NY and east into southern New England. Will have several factors combining to produce at least a localized flash flood threat across this region. Will have enhanced southwesterly 850mb flow ahead of Barry, a front dropping south helping enhance low level convergence, and an upper jet over northern New England placing the area in the favorable right entrance region for increased upper level divergence. It would appear that we have enough ingredients in place to support the potential for some organized west to east training of convection near the tightening lower level convergence axis. Cells will be very efficient rainfall producers given the high PWs, thus any training would likely result in a flash flood risk. Still some uncertainty with regards to exactly how organized convection is able to get, and whether cells will take on enough of a southward prorogation with time to limit the duration of heaviest rainfall rates. Thus it is possible that the flash flood threat remains localized and restricted to sensitive urban areas...but nonetheless enough ingredients in place to warrant a Slight risk...with at least some potential for more organized clusters of flash flooding. South of the Slight risk the expectation is that convection will be more isolated in nature and quick moving, both which suggest the flash flood risk is isolated and highly localized in nature...with a Marginal risk sufficing. The exception is across northern AL, where we will carry a small Slight risk. Note some tightening of the low level convergence over this area this morning, with building instability upstream advecting into the region. Thus at least some potential for a period of backbuilding cells through the morning hours, which could locally drop 3" or more. This setup does not appear anywhere near as good as what happened over southwest AR last night, but the basic setup is similar, just to a much lesser extent. ...Upper MS Valley... Convection is racing eastward across the Northern Plains this morning, and the environment will remain conducive for additional activity today into tonight. The biggest threat for flash flooding appears to be during the evening into the overnight hours with the nocturnal increase of the low level jet. The convection this morning will likely leave a nice low level boundary in its wake...which will be reinforced into a developing warm front as forcing approaches from the west this evening. With the increasing low level jet into and over this front...expect elevated convection to expand in coverage. Wind fields support backbuilding convection and should have plenty of upstream instability available to support continued convective growth on the southwest flank of developing convection. The magnitude and persistence of 850mb moisture transport, and the presence of an upper jet to the north enhancing upper level divergence, all point to the potential for a widespread, and locally significant, flash flood threat. Some potential that a Moderate risk may need to be considered later today. At this time there is too much spread on the favored axis and exact evolution of convection, that think a Slight risk is best for now. The global models are much further north than the high res...and with this forecast package went with a weighted compromise towards the high res guidance. Although, at times the high res can be too far south when there is strong forcing to the north, as is the case here...so was hesitant to completely buy into some of furthest south solutions. Chenard Day 2 Valid 12Z Thu Jul 18 2019 - 12Z Fri Jul 19 2019 ...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL ACROSS THE NORTHERN GREAT LAKES REGION... ...Northern Wisconsin/Northern Michigan... At the start of the forecast period, amplifying shortwave at the nose of unseasonably strong 250mb jet that is flat and stretches well back into the Northeast Pacific will be lifting out of the area into Ontario, with a strong surface low pressing the attendant frontal zone across N MN/Lake Superior. However, given the orientation of the deeper flow out of the southwest veering slight west, the frontal zone flattens out across the UP/N WI into south central MN. The 850mb LLJ will be strong across the region at over 40kts and with solid moisture convergence at the inflection where the front flattens will support total PWats AOA 2". The LLJ will continue to be strong throughout day with slight backing supporting moisture flux anomalies over 4 Std.Dev from normal. However, there will be a ongoing convective complex across the Upper Mississippi River Valley and there is growing uncertainty in its evolution on D1. Hi-Res CAMs suggest with high instability and strong LLJ, propagation vectors will have a stronger southerly component potentially across NW IA/N IL into NW IND. Global guidance is quicker to kill off the MCS and favor stronger ascent/forcing near the front and therefore supports stronger convection across N WI into the UP and Northern Portions of the LP of MI. The former would disrupt warm advection of necessary moisture/instability across Lake Michigan for the build up for a complex Thursday evening into Friday morning. Given the uncertainty in the placement, but the very strong synoptic environment for heavy rainfall clearly capable of producing heavy rainfall rates and short-term totals capable of scattered flash flooding conditions warranting a Slight Risk. At this time, given the stronger larger scale signals will favor the global guidance slightly in the placement of the Slight Risk, however, will broaden the Marginal Risk of excessive Rainfall further south and west to account for the backbuilding system. ...New Jersey/NYC... By the start of the forecast period, the deep moisture conveyor belt associated with Post-Tropical Cyclone Barry has pressed eastward offshore into the Northwest Atlantic. However, its remaining sheared shortwave that supported a new surface circulation out of the Mid-Atlantic lee surface trof on Wednesday (not PTC Barry) will be in the vicinity of the Mid-Delaware River Valley, maintaining some near surface moisture. This will result in a tightening deep moisture gradient with 1.75-2" remaining through the total depth by midday. Given a slight trend for eastward press of the moisture, remaining high clouds are likely to eastward as well allowing for increased insolation and instability to build by early afternoon across New Jersey. Hi-Res CAMs and even global models suggest SBCAPEs to exceed 1000 J/kg perhaps reaching as high as 2000 J/kg. As such there is a solid clustering of Hi-Res CAMs suggesting 1-3" totals are possible with slower moving/merging convective cells in the afternoon. As such have maintained a Marginal Risk of Excessive Rainfall for NJ and the low FFG areas near the NYC metro, but have pulled the Risk area out of southern New England where lingering clouds/precipitation is more likely to limit sufficient instability to build back (additionally higher FFG values). Gallina Day 3 Valid 12Z Fri Jul 19 2019 - 12Z Sat Jul 20 2019 ...The Probability of rainfall exceeding flash flood guidance is less than 5 percent... ...Upper Mississippi Valley into Northern Great Lakes... Exceedance of flash flooding is highly contingent on the placement and evolution of multiple convective complexes expected on day 1 and day 2 lowering Flash Flood Guidance values across of convection. A frontal zone will remain stationary through day 2 into day 3, pooling moisture and therefore instability throughout these few days. By day 3, moisture flux convergence will reach a general lull given the LLJ will start to orient more parallel to the boundary. While there will be sufficient moisture (up to 2" total PWats across S MN into N WI), the unseasonably strong polar jet will be fairly flat oriented across the region, reducing upper level shortwave/PVA support. However, convection that does develop will have the tendency to move east along the frontal zone reducing flash flood guidance for any further upstream development that would have the tendency to repeat/train. Currently, the global guidance suggests the best corridor would be from SE MN to the northern LP of MI, but given higher probabilities of convection further south and/or west on D1 and D2 it is hard to support placing a precise Marginal Risk at this time, but will likely change as hydrologic/FFG situation becomes better realized in the coming day or so. Gallina Day 1 threat area: https://www.wpc.ncep.noaa.gov/qpf/94epoints.t... Day 2 threat area: https://www.wpc.ncep.noaa.gov/qpf/98epoints.t... Day 3 threat area: https://www.wpc.ncep.noaa.gov/qpf/99epoints.t... $$ ------------=_1563354191-51656-12255 Content-Type: text/plain; charset="US-ASCII" Content-Disposition: inline Content-Transfer-Encoding: 7BIT = = = To unsubscribe from WX-STORM and you already have a login, go to https://lists.illinois.edu and use the "Unsubscribe" link. 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