A last word of advice, escrow is a fluid state. It can be a very stressful time. As new information comes in, revisions are needed and situations come up that are out your control. Your escrow officer is there to hold all the strings together like a spider in the center of the web.
119 As the upvalley wind picks up during the day, the upslope winds are turned to a more upvalley direction. there may be a very shallow downslope flow because of the shade provided by the canopy. Downslope winds at night on densely forested slopes are affected by the presence or absence of a dense understory.
In the evening, the mountain slopes cool the surrounding air more quickly than the air found lower in the atmosphere. This creates a high pressure as air becomes more densely packed. The resulting high pressure causes winds to blow down the mountain towards the valley floor. This type of wind pattern is known as a mountain breeze. Thus, in the daytime we typically see valley breezes as winds blow from the valley up towards the mountains. In the night we often see mountain breezes as winds travel from the mountains down towards the valleys.