San Francisco is settling into a distinctly typical pattern for early June, with meteorologists predicting a week of stable weather with temperatures sticking close to the seasonal average. Morning marine layer clouds and patchy fog are expected to occur regularly, followed by breezy onshore winds kicking up each afternoon and evening. The National Weather Service San Francisco indicates that this persistent pattern is largely due to an upper-level ridging starting to erode and becoming incorporated into the larger-scale atmospheric flow over the western United States.
As some coastal areas gear up to potentially remain cool with highs in the upper 50s to middle 60s, inland regions are preparing for warmer temperatures reaching into the middle 80s and some spots potentially tipping just close to 100 degrees. According to a detailed forecast for San Francisco, the city can expect a slight chance of morning drizzle before 11 AM, eventually giving way to sunnier skies with a high near 67 degrees, and winds strong enough to prepare for gusts as high as 28 mph quickly.
The NWS’s short-term forecast assures that the breezy conditions will continue into the night with a slight chance of drizzle returning post 11 PM, maintaining mostly cloudy conditions with lows around 55 degrees. These gusty conditions are even expected to maintain their pace through the week, parallel to the inflow of an enhanced IR satellite imagery that suggests a deeper marine layer causing widespread stratus over the Bay Area and Central Coast.
Moving towards the weekend, the meteorological synopsis predicts that the marine layer will sustain its push inland each night and morning, with the upper-level ridge continuing to erode and the potential for slightly cooler temperatures as a trough moves into the region. “Perhaps Friday and Saturday will see temperatures a few degrees cooler than those from earlier in the week,” a synopsis from NWS San Francisco suggested, underlining the influence of the trough in reinforcing onshore flow and deepening the marine layer.
Copyright for syndicated content belongs to the linked Source link