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Albuquerque: Balloonist Paradise
Albuquerque, New Mexico's unique weather characteristics make it a popular destination for hot-air balloonists. While balloonists can control their altitude by warming or venting the air in their balloon, their horizontal travel comes at the mercy of the wind. (Just ask the erstwhile Wizard of Oz.)Β (Image credit: B. Bos; via Physics Today)
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The Misty Mountains by Richard Fox Via Flickr: We had some spectacular misty conditions again on Sunday. I was driving around frantically stopping in various places. This was taken at a brief stop at the top of Loch Ard looking towards stirling.
Occasionally you can see Canada from Ohio. Click to read the full fact.
Landscape Language
Cloud inversion (noun) β a phenomenon when cold air is trapped under a layer of warm air.
Also known as temperature inversions, cloud inversions are a weather phenomenon created when a layer of cold air is trapped under a layer of warm air. Typically, warm air is closer to the earthβs surface. In an inversion, condensed moisture in the cold layer forms clouds that are trapped near the ground. Cloud inversions often form in valleys like those around Mount Rainier. It is not uncommon for it to be cloudy and cool at low elevations and warmer and sunny at higher elevations! Do you have photos of cloud inversions observed around the park?
NPS/S. Redman Photo of a cloud inversion filling the Nisqually Valley, September 2011. Β ~kl
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Karkonosze (Giant Mountains), Poland by daniellamotte
Morning has broken.. by Badge McVid Via Flickr: Looking towards Inverlochlarig & the River Larig from the lower slopes of Beinn Tulaichean. A beautiful morning to be up the hills.
This mesmerizing gif shows a waterfall of mist gently spilling over the sun-illuminated cliffs of West Bay in Dorset, England.
The footage, captured by a drone, shows the effects of a temperature inversion.
A temperature inversion happens when a thin layer of the atmosphere experiences a temperature increase as height increases. Under 'normal' circumstances, atmospheric temperature tends to decrease as height increases.
This warm atmospheric layer acts as a lid; keeping normal convective overturning of the atmosphere from penetrating through the inversion.
As a result of the temperature inversion, clouds below this atmospheric layer are forced to spread out and take on a flattened experience; as we can clearly see in this footage.
-Jean
Full video: https://www.youtube.com/watch?v=BZkYYXx7hEs
