The corresponding MesoWest analysis shows relatively similar lake-land temperature differences compared to earlier, although a few of the land stations have cooled slightly. Perhaps the most substantial change is the increased flow on the lakeside mountains, for reasons I do not understnd. Concurrently, the flow on the east side as weakened. The HAT-PRP temperature difference is now 8C, consistent with steepening lapse rates observed in the east-side soundings.
We're in business! Our teams will be taking soundings while you sleep. Keep your fingers crossed.