Winds may increase from the northeast around midday and form very shallow drifts (maybe 6 inches deep) that should easily avalanche. They shouldn't be much of a concern and will mainly be interesting to see how yesterday's weak surface snow reacts with a shallow soft slab on top of it. Michael J's ski tracks yesterday show the weak snow very well in the photo below as each ski turn sluffed the weak surface snow. Now, imagine a shallow wind slab resting on that snow.

There is a persistent weak layer of faceted snow and depth hoar near the ground that fractured and produced avalanches through much of December and early January. Since then, this layer has gained a lot of strength, and it is unlikely you can trigger an avalanche on this layer. HOWEVER, a layer like this doesn't magically go away, it slowly strengthens through time and goes mostly dormant.

The somewhat recent avalanche Ted spotted yesterday in Mill Creek is a great reminder that this layer still exists and could produce an avalanche even though it is unlikely.

What to do? I have no worries about this problem below treeline where the snowpack is deep and uniform. Steep, rocky terrain above treeline with a more variable snowpack is where I would worry a little bit. Ride parts of a slope with the deepest snow, carry avalanche rescue gear, expose only one person at at time, and consider where a slide will take you if it does happen.