It’s been an interesting spring as the La Niña conditions of this past winter continue to abate. One of the characteristics of this diminishing pattern has been for low pressure systems to drop southeastward from the eastern Pacific and west coast and then across the southwestern states. Springtime low pressure systems routinely move across the southwest and bring strong winds to Arizona and these systems have been quite normal in that respect, that is, it’s been very windy.
But they have also brought the core of the low pressure system farther south than is typical and across Arizona. The result has been a combination of below normal temperatures and above normal rain along with snow in the higher elevations.
We had three days of snow last week — but only trace amounts fell across the area — and now we are having a real bona fide snow event. A few inches of snow have accumulated at elevations above 7000 feet.
Will this be the final event of this winter-like spring? Or will we see snow again? The record books show that snow isn’t rare in May at these elevations — and snow in June has happened on a number of occasions, too.
We’re all looking forward to spring finally arriving before the calendar says summer.
The weather across much of the country has been very dramatic the past few days with snow storms, ice storms, strong winds, and brutal cold. Across Arizona we experienced exceptionally cold weather as the Arctic air mass settled in across the area. Strong northeast winds at the surface and aloft helped to drive the cold air across the Rocky Mountain barrier and deep into the southwest.
The northeast winds also created some fantastic wave clouds over the San Francisco Peaks, located to the north of Flagstaff. Normally, strong southwest winds roll across the Peaks and the best wave clouds are located to the northeast but this wind reversal resulted in a reversal of the wave clouds as well.
Even more interesting were the clouds that were forming just below the tops of the peaks. Strong winds from the northeast drove cold air into the Inner Basin on the east side then up and over the top of the peaks. As the air ascended thin wispy clouds would form. Just as quicky the air descended on the southwest slopes and the clouds evaporated.
The rapidly changing clouds and detailed structure were fascinating to watch. A time-lapse movie clearly shows this incredible dance of the clouds as it moves across the Peaks.