Then there were the “Northers,” which the heavy winds that swept down the Cajon Pass from the Mohave desert were called. They were much more severe then and sometimes very cold, blowing for about three days at a time. Many people treated them as they would rainy weather, and by way of derision, they were sometimes called “Mormon rains,” coming as they did by way of San Bernardino. They often came before the rains and when sheep had been pastured in the early summer the surface of the ground was cut into fine dust and we would have a dust storm which would cover the inside of the houses with dust. Since the land was planted and roads oiled, the “Northers” have lost most of their disagreeable features. Being dry they clear the atmosphere and are one of the beneficial features in our healthy climate.
History of San Bernardino County – John Brown Jr., 1922
If you want to see the desert pick a fine day and go to the desert. It will be cloudless, hot, and asleep and pretty much as you expect it. If you want to be in the desert while it is awake and alive and changing its own character–go when there is drama in the skies and in the wind. Go when its army of clouds cast unshaped shadows of camouflage on its colored hills. Go when rain is pouring down from the heavens in patches and flooding the landscapes and carving the canyons and washes. Go when the wind is blowing sand that scars its cliffs and uprooting the Joshua trees that have become old and weak. Go while the desert is growing, reshaping, and in a dubious struggle with itself. Go then.
Known as Altocumulus Standing Lenticular (ACSL) or Altocumulus Standing Lenticularis clouds, they are associated with waves in the atmosphere that develop when relatively stable, fast moving air is forced up and over a topographic barrier that is oriented more or less perpendicular to the direction from which the upper-level wind is blowing. This deflection creates a gravity wave downwind of the topographic barrier not unlike a wave you might generate by throwing a pebble into a pond. When sufficient moisture is present above mountain-top level, ACSL clouds develop within the crest of these mountain waves where the air is rising. ACSL clouds are continually developing and dissipating in the vicinity of the wave’s crest and immediately downwind of the crest, respectively. That is why they appear to remain stationary (hence the name) even though winds are swiftly (sometimes very swiftly) moving through the entire cloud