Hydrometeorological Discussion
Issued by NWS Tuscaloosa, AL
Issued by NWS Tuscaloosa, AL
655 AGUS74 KWCO 301300 HMDNWC National Hydrologic Discussion - EXPERIMENTAL NWS National Water Center - Tuscaloosa AL 700 AM CST SUN NOV 30 2025 Update... No major changes to the FHO for day one; however, we included a new bullet messaging the return of rainfall late in the week for southeast Texas and southwest Louisiana. The timing of the limited area was not extended due to low confidence in potential impacts. American Samoa remained highlighted as flooding concerns will continue through today. //Smith Previous discussion as follows ...Isolated flash flooding impacts remain possible across American Samoa through tonight... Isolated flash and urban flooding remains possible across southeast Texas into southwest Louisiana this weekend... American Samoa... Periods of heavy rainfall will continue through tonight (local time), likely leading to isolated flash flooding impacts across the islands. Southeast Texas and southern Louisiana... Periods of heavy rainfall are expected across the I-10 corridor tonight, potentially bringing isolated flooding impacts to the region, especially across southeast Texas. Soils remain dry (NASA SPoRT) and most streamflows are below normal (USGS) which should help mitigate widespread flooding issues. Streams in the immediate Houston area are more near normal, so this in combination with the expansive urban area slightly increases confidence in potential flooding impacts in this region. The Limited impacts area remains in place, with overall confidence in flooding impacts being quite low. Confidence has not increased sufficiently to justify expanding the valid period of the limited area beyond day three at this time, but it remains possible that an expansion of the limited area both in time and areal coverage (further northeast into the Southeast) will be possible for the mid-to-late week period next week. //JEC Additional National Water Center products are available at www.weather.gov/owp/operations $$