####018002187#### AGUS76 KRSA 131915 HMDRSA Hydrometeorological Discussion National Weather Service / California Nevada RFC / Sacramento CA 1215 PM PDT Wed Mar 13 2024 ...UPPER LOW TO GENERATE SCATTERED SHOWERS MAINLY SOUTH/EAST... .METEOROLOGICAL CONDITIONS (SHORT TERM: WED PM - SAT AM)... Thinking remains the same with an upr low dropping into the Great Basin primarily along the UT/NV border before settling in the vicinity of the CA/NV/AZ triple point. At the same time...a strong upr ridge just off the west coast will build toward BC and the Pacific Northwest. This will generate generally dry north to northeast flow for much of the region. In the area where the upr low resides through the end of the week...look for moisture to become entrained into the system and primarily impact the Four Corners states. It does look like enough moisture will wrap around the circulation and make its way across far southern/eastern NV along with portions of southern CA that may generate some scattered showers. Freezing levels will show a sharp gradient from about 10000- to 11000-feet northwest to approx 3500- to 5500-feet east. .METEOROLOGICAL CONDITIONS (LONG TERM: SAT AM - TUE AM)... Guidance continues to forecast the persistent high-low dipole between the Pacific Northwest and the CA/NV/AZ border through the long-term window. The low over the southeastern portions of the forecast region will provide support for light-to-moderate shower and thunderstorm activity with accumulations generally less than a tenth of an inch, though locally higher amounts within thunderstorms. Afternoon forecasts have continued to follow WPC guidance, keeping accumulations low, and only slightly changing due to the uncertainty in exact location, track, and timing of shower activity. Freezing levels generally around 10,000 feet in northern CA and around 5,000- 7,000 feet over southern California and Nevada Saturday before rising to 7,000-9,000 feet over the south on Sunday and into Monday. QPF graphics are available at www.cnrfc.noaa.gov/qpf.php Kozlowski/CH $$