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You’re thinking about it too binary though. It affects everywhere. But you keep saying “if location X gets a snowstorm, then it must not be happening there.” And if someone says it’s happening here, they mean zero snow. Maybe for one region it decreases the chances by 10%… for another area they have already low chances of snow so it decreases chances by a percentage point or two. But there’s always a percentage chance the storms happen. It’s like a sliding scale and changing the probabilities. It’s not a binary yes or no.
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Like an injured fawn limping through a field while a wolf salivates from the wood line.
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That’s a good point. I’m not super familiar with Lake George but it’s weird it froze behind schedule, given most other lakes seemed ahead of normal or with larger than normal ice extent. I do know that area is gusty and downslopes on NW flow off the southeastern Adirondacks… was just spitballing for ideas as to why it could be delayed. A lot of wind would lead to more mixing and upwelling, and the water surface is rarely calm.
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There’s nuance to everything… and CC is a charged term that leads to a visceral reaction more than other factors. One could imagine a situation where a variety of factors influence the rate of something occurring, but doesn’t stop it from happening all together. The debate of “no coastal storms anymore due to fast flow and CC” vs “its snowing in the deep south on the coast” is severely lacking in nuance on both sides. It’s binary thinking that ignores context and oversimplifies the issues at hand for both points of the argument.
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Sun angle is ever so slightly higher than it was yesterday .
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Yeah car was covered this morning in the very small flake Arctic upslope stuff this morning… where it feels like the flakes are forming like 500 feet overhead.
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That is weird. Lake Erie by contrast has the most ice in late January in like three decades and is almost fully covered. Wonder if the persistent NW flow causes a lot of wind there and water movement at Lake George?

