eduggs
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Everything posted by eduggs
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On a microscale, no. We still can't pinpoint precipitation boundaries at the scale of individual towns and cities 3 days out. That's why I think it's best to take everything into account. Based on GFS and CMC trends several days ago, some thought good snows would get to PHL and NYC. The NAM was stubborn and resisted the trend. In the end, a blended compromise would have been right. It doesn't always work that way, but it's still almost certainly best to weigh all model outcomes at least a little.
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From a forecasting perspective, discarding individual models runs - without obvious cause - will lead to forecast bias. From a hobbyist perspective, it will lead to false expectations and disappointment. We've seen it a million times. If it's an outlier run, is it unreliable or the first to sniff out a trend? Without knowing the final outcome we cannot know which model runs to consider or discard. That's why it's best to consider all the major model outcomes as plausible and deal in probabilities, not absolutes.
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1. Smaller events are usually shorter events and that means you might not be able to enjoy them due to work or sleep. 2. In places that don't get snow events very often, there can be a feeling like you have to cash in on every chance that you get because you can't count or another to look forward to.
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Yesterday's mid-Atlantic snowstorm had a ton of GOM moisture out ahead of the trof just pumping northward into a wall of cold air. We won't really have that luxury with this one. Here we need to rely on the dynamics of a rapidly deepening SLP and moist easterly inflow. The main precipitation shield is not likely to extend very far NW unless this really wraps up.
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You don't even have to look at the surface to see that guidance has shifted everything east. Look at H5 - best PVA is SE. The surface is just a reflection of the upper level divergence/convergence. Good thing is that if this sharpens up 10 %, the SLP ends up 100 miles NW. There will be plenty more changes.
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We're dealing with a little bit of a transition from the initial inland surface reflection and associated precipitation in PA to the developing coastal low. It's possible I-95 or just inland sees a bit of a precipitation minimum as the transition skips over this area and refocuses closer to the coastal. The precipitation shield as modeled looks to be shrinking and tightening as the SLP winds up.
