forestgnome
New member
I've always called them 'snow clouds'. There must be a name for those clouds of snow that are whipped into the air by strong winds. It's a very powerful image of cold and danger. Picture below.
"Ground Blizzard." Dr. Charles Hosler, professor emeritus of Meteorology here at Penn State, explains what a Ground Blizzard is: "A ground blizzard is basically a blizzard without snow. When skies are clear and no snow is falling, but winds are high enough to blow snow already on the ground fast enough to reduce visibility to less than a quarter mile, you have a ground blizzard. These happen in Antarctica almost everyday. A ground blizzard is like a dust storm, only with snow."
Growing up outside of Buffalo, we would occasionally get ground blizzards. If there was a big snowfall after Lake Erie froze over and strong winds came in off the lake, the snow on the ice would get blown onto land. You'd get a blizzard with the sun shining. I remember getting caught in a complete white out once during a ground blizzard. I couldn't see anything around me, but overhead there were bright blue skies.DougPaul said:If it is heavy, it would be a ground blizzard:
From http://www.personal.psu.edu/users/t/n/tnn107/Tiffanysblizzard.htm...
This dynamic sounds more like windblown snow. Kind of hard to see dynamics in a still photo... But, IMO you are correct, there could be "bubbles" of humid air which form short lived lenticulars.forestnome said:It does look like a lenticular, but I don't think so because I sat and watched this from the road at Pinkham Notch before climbing Boott Spur on Saturday. It would only last for 10 or 20 seconds, then dissappear, then appear and disappear again. It was extremely gusty up above treeline. Then again, don't know if that would eliminate lenticulars.
IIRC, I've only seen the term spindrift in the mountaineering literature. (I'm not a meteorologist, so my reading might be biased...)Until I learn of a recognized meteorological term, I'm going to call them 'snow devils', relating them to dust devils.
A lenticular is a specific kind of cloud. A humid layer of air is blown over a high spot (ridge or peak) and forms a cloud over/slightly downwind of the high spot because the air is forced upward and thus cooled. If you look carefully, you may be able to see it forming on the windward edge and evaporating on the leeward edge. They frequently look like cloud caps and can have multiple layers. In the case of a ridge, you can have several downwind lenticulars at the tops of each wave.Jay H said:Lenticulars, from my understanding is moisture that forms by winds on high mountains, etc. moisture that is from the air, but actual snow that is blown off the peaks from the wind is spindrift...
forestnome said:I've always called them 'snow clouds'. There must be a name for those clouds of snow that are whipped into the air by strong winds. It's a very powerful image of cold and danger. Picture below.
w7xman said:Hey forestnome...
The crew at the summit the other day got some pics of them as well, presumably from the same time you did. I'll post them in a few.
Orographic Stratus
* Distribution: Over hills and mountain ranges worldwide.
* Height: 0 to 1000 feet above ground level.
* Cause: Lifting of moist air mass by landform.
* Associated Weather: May produce fog, light drizzle or light snow showers.
* Hazard Warning: Can be an aviation hazard as it masks terrain.
Orographic clouds are formed when moist air, carried on a prevailing wind, is lifted by an elevated landform, such as a mountain range, to a level where condensation takes place. Among the most common orographic clouds is orographic stratus. This low-level formation occurs most frequently in areas, such as coastal regions, where the air flow is heavily moisture laden. Generally, the landform must be at least 500 feet high to generate cloud, and higher in areas of clean, dry air, such as deserts.
Unlike normal stratus, which is carried about by the external wind field, orographic stratus tends to remain stationary. The wind flows through the area of condensation, constantly regenerating cloud as the air rises and dissipating it as the air descends on the other side of the landform.
The extent of this type of cloud depends on the humidity of the surrounding air mass. If the air contains a high level of moisture, cloud can begin to form well down the windward slope of the landform, wrap around the peak, and extend some distance down the other side. A good example of this type of formation is the "tablecloth" that often drapes the top of Table Mountain near Cape Town in South Africa.
The extent of the cloud is also determined by the steepness and elevation of the landfornn, the strength of the wind, and the direction of the wind relative to the landform. Strong wind blowing at right angles to a steep mountain will create greater uplift and generate more cloud.
Since low-level moisture and high land are essential ingredients in the formation of orographic stratus, areas that have high humidity and steep terrain -- tropical islands such as Hawaii, for example -- are particularly conducive to the formation of these clouds.
Sometimes, there is insufficient moisture in the lower layers of the atmosphere to allow condensation at ground level, but with increasing altitude and lower temperatures, condensation may be possible. In this case, lifting of the air mass by a landform can produce middle-level orographic formations, known as lenticular clouds.
In the Earth’s atmosphere clouds often form on the windward side of mountains and are classified as Orographic Clouds. Orographic clouds are clouds that develop in response to the forced lifting of air by the earth's topography, such as mountains, and fall into the following general categories:
Conjoined orographic clouds - covers entire mountain, forms on windward side.
Orographic Cumulus fractus – usually covering mountain range, large area of clouds covering both windward and lee sides of mountains.
Orographic Stratocumulus and Altocumulus (wave clouds) – form on the lee side of a mountain.
Pileus (Latin for "skullcap") is a smooth cloud found attached to either a mountaintop or growing cumulus tower.
Orographic Clouds. On Earth, large dense clouds often form in mountainous regions and hover over the tops of mountains. Air that flows over a mountain forms airwaves on the leeward side of the mountain. In the back of the wave where the air rises, cools and forms smooth elongated clouds. When moist air reaches colder upper altitudes rapidly cooling causes condensation to occur and clouds form. These clouds will linger over mountainous regions for long periods and move around very little in spite of very strong winds. They are referred to as orographic clouds. Orographic clouds on Earth are often called almond clouds or lenticular clouds [Miller and Thompson, 1970].
Is that what this is:w7xman said:...Those are actually a formation of orographic stratocumulus. Not blowing snow at all, though from afar it looks like blowing snow or spindrift. ....
Pete_Hickey said:"I've looked at clouds from both sides now."
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