By Mike Godsey


ZZ7D67D7E6You don’t see much sign of the NNE
winds at the surface
but they impact the wind distribution and strength.

by Mike Godsey

Have you ever noticed that on days when my forecast prattles on about the impact of AM NNE winds on the Bay Area winds you actually don’t see much sign of NNE winds? For example take a look at the wind map from early this morning in the top image.

All you really see NW wind out at the ocean buoys and some NNW wind closer to shore while inside the bay the winds are weak and random. So where is the NNE wind?

The issue is that the NNE wind coming down the Central Valley and over the  ridges is relatively warm air so when it hits the Bay Area ridges it tends to lift and does not come down to the sensor level.

But now look at the 2nd image. Notice the NNE winds hitting some of the ridge tops and hitting the NPHridgeNLYcvalleysensor in the Central Valley where the terrain is very flat.

NNEwinds ValleyAM So if that wind is mostly just aloft how can it impact our surface wind? Well to get useful wind inside the Bay Area this afternoon we need that ocean wind to be sucked though the gaps in the coast range and head towards the Central Valley.

But this NNE wind aloft does several things to delay and weaken that process.

  1. First remember that NNE wind develops when the NPH pushes a ridge towards the Pacific Northwest which also causes the winds near the Bay Area coast to switch from NW to more NNW which makes it harder for the winds to get to shore.
  2. Then visualize the NNE winds just aloft pushing the NNW ocean wind away from shore which delays the arrival of our afternoon winds.
  3. The NNE winds also encourage the Central Valley thermal low to migrate towards the coast which spoils the pressure gradient

Then in the afternoon the NNE winds typically fade away and the 3 processes above subside somewhat. The problem is that the valley low pressure often does not fully retreat to the Central Valley and hangs near the East Bay. So the pressure gradient is focused between the ocean and sites closer to the coast from Treasure Island westward.

You can see all of this happen in the 2 animations.

Mike Godsey