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What's rotating around that monsoonal high, that's why they call it the monsoonal high. And the cirrus that you're getting are the blow off from yesterday's thunderstorms over the high sea eras. Because there's some easterly flow in the upper levels around that high. And there you go, there's your, that thin high thin cirrus is what blows off the top of the anvil, shaped at the top of a thunderhead. And many times that's what ends up in the valley the next day there. Yeah, I know we have a lot of draw down in the evenings. We'll have a lot of draw down into the valley out of the cirrus. And that whenever we have wildfires we have a lot of air.