Hydrometeorological Discussion
Issued by NWS Tuscaloosa, AL
Issued by NWS Tuscaloosa, AL
086 AGUS74 KWCO 191522 HMDNWC National Hydrologic Discussion - EXPERIMENTAL NWS National Water Center - Tuscaloosa AL 1015 AM CDT WED JUN 19 2024 .Synopsis... Considerable flooding expected in Texas... Locally considerable flooding is possible in the Northern Plains, Upper Midwest, and Upper Great Lakes... Isolated flooding possible in the Central Plains... Localized urban flooding possible in the Northeast... Snow-melt induced flooding in Alaska... .Discussion... .Texas... Tropical Storm Alberto will bring considerable flash, urban, and riverine flooding to portions of southern TX through day 2 (Thu), with the bulk of the rainfall expected today. Although conditions are expected to gradually improve as we head into the weekend, there is the potential for the wet weather pattern to continue through at least early next week. Widespread QPF totals for this event range from 5 - 10", with locally higher possible. Antecedent soil conditions are dry across south TX and streamflows are running at normal to much below normal mean annual flows, allowing for some infiltration and in-channel storage capacity for the initial rounds of expected rainfall. This will help buffer initial hydrologic responses, but with high forecasted rainfall totals and high rainfall rates, considerable flooding impacts are still likely. The TX Hill Country will be an area to watch, as basins are flashier due to the high relief and the area is currently forecast to get 2 - 3"+ over the duration of the event. Considering the current reservoir capacities are below 30% across the region (except near Victoria where reservoirs are near capacity), this rainfall will be generally beneficial outside of areas where heavy tropical rainfall may develop. As for river flooding, HEFS ensemble guidance continues to show minor to moderate river flooding in south TX, with isolated minor to moderate flooding already being forecast. The HRRR-forced National Water Model (NWM) Short Range Forecast (SRF) is beginning to pick up on the QPF for this event and is showing a similar story as the NWM MRF over the past couple of days. Rapid-onset flooding probabilities continue to be fairly low-end (less than 50%), likely due to the dry antecedent conditions and the QPF not being fully captured. Scattered annual exceedance probabilities (AEPs) below 20% from the High Flow Magnitude Forecast (HFMF) suggest considerable responses through normally dry streams and arroyos across south TX, which implies that flooding impacts are expected in areas that do not typically flood. The NBM-forced version of the NWM is showing scant signals considering the amount of rainfall forecast, which is due to the high ARI value from the NWM in TX. The GFS-forced version of the NWM is much more aggressive, with widespread AEPs less than 20% being signaled. These signals are likely overdone in their wide areal coverage, but isolated occurrences of these extreme signals are possible should the rainfall exceed current forecasts, also supporting the potential for locally considerable flooding impacts. Flash and urban flooding, regardless of antecedent conditions, are still likely wherever repeated rounds of heavy rainfall occur. .Northern Plains, Upper Midwest, and Upper Great Lakes... Flash, urban, and river flooding, with the potential for locally considerable impacts, are expected this week and through the weekend from a multi-day storm system bringing repeat rounds of heavy rainfall sets up across the region. The first round of heavy rainfall is forecast starting on day 2 (Thu) and will continue through day 4 (Sat), peaking on day 3 (Fri). A brief lull is then expected on day 5 (Sun) before additional rounds on days 6 - 7 (Mon - Tue), although this rainfall should be less significant. Current guidance places the axis of heaviest rainfall (7-day totals) across eastern SD, southern MN, and central WI (3 - 5", locally higher possible). The region remains hydrologically active and vulnerable having received 150 - 200% of its normal rainfall over the past 30 days (CPC). USGS streamgages are reporting widespread above normal flows both historically and for this time of year. Soil moisture down to the 100 cm layer remains on the wet side as well (65 - 80% RSM, NASA SPoRT), suggesting limited infiltration capacity. Given these conditions, it will not take much rainfall to generate immediate runoff and subsequent flooding of small streams and creeks, as well as low-lying and poorly drained locations in urban areas. Each additional round of rainfall will serve to further compound the flood potential. Additionally, isolated moderate to major river is ongoing or forecast across the Minnesota, Upper Mississippi, and Crow river basins in southern MN, with ensemble guidance (HEFS 30%) indicating additional rises along the Mississippi and any tributaries affected by this heavy rain. Many locations along the Mississippi River will approach flood stage towards next weekend. Both the NBM- and GFS-forced NWM are responding accordingly with widespread responses and the potential for rapid-onset flooding. Both models show good agreement with the placement of the rainfall, however, the GFS is much more aggressive with the overall magnitude of the responses. .Central Plains and Mid-Mississippi Valley... Slow-moving convection with the potential for enhanced rainfall rates will continue to impact portions of the OK Panhandle into southern IA through late this evening, bringing a renewed threat of isolated flash, urban, and minor river flooding. Antecedent conditions are variable, with recent periods of drought leaving much of NE/KS/OK dry. However, recent rainfall has helped to moisten soils and elevate streamflows across eastern portions of NE/KS into IA (50 - 65% RSM, 0 - 100 cm, NASA SPoRT). With the ongoing rainfall, there may be a few isolated areas of more saturated soils not yet reflected by NASA SPoRT. While this suggests infiltration capacity remains available, locally heavy rainfall rates may be able to overcome this, pushing runoff into already elevated smaller streams and rivers and produce sharp rises as well as flash flooding. The NWM SRF continues to signal the potential for rapid-onset flooding across the OK Panhandle/southeast KS with 12-hr probabilities between 50 - 75%, and more low-end probabilities through central KS into southwest IA (mostly less than 25%), however, these signals will likely continue to increase as the storm develops throughout the day. The NWM SRF HFMF is indicating fairly widespread streamflow AEPs as low as 4% across the Panhandle north to Dodge City, KS, where high water flows are ongoing. While these signals are likely overdone to an extent, these AEPs align with the region of highest probabilities for small stream responses, increasing confidence in flooding impacts in this region. Any areas where intense rainfall rates persist or repeat will see the greatest threat for flooding impacts. .Northeast... The potential exists for localized flooding impacts in primarily urban areas on days 3 - 5 (Fri - Sun) as showers and thunderstorms develop across the region. Outside of sensitive urban areas, near normal relative soil moisture values (50 - 60%, 0 - 100 cm, NASA SPoRT) and near to below mean annual streamflows (USGS) suggest sufficient infiltration capacity overall to capture runoff. These factors, combined with modest rainfall amounts (less than 2"), will help to mitigate any widespread hydrologic responses and limit the threat to urban, low-lying, and poor drainage areas. .Alaska... Warm daytime and overnight temperatures are causing significant snow and ice melt at high elevations, leading to minor flooding on the Chilkat River near Klukwan, which is expected to persist due to diurnal temperature trends, and localized flooding in the Yetna and Skwetna river basins. Similar flooding is anticipated along the Nuyakuk River. These warm conditions are projected to continue through early next week in southwest, southcentral, and southeast areas of the state, further increasing the rate of snowmelt runoff into rivers. //Freeman $$