Fog, rain and snow
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Berlin on a foggy morning.
This shot was taken from a plane over Berlin by my colleague Carl Janssen on a December morning using an Apple iphone 6s.
As the sun started to rise, the fog started to dissipate. Soon islands of trees started to reveal themselves and bask in the morning light. The image here is a 2 image pano. Hope you enjoy!
A bit of fog settled in this evening after a storm went through. This marks the end to another weekend. Have a great week ahead everyone :-)
~ Winfield, Illinois
While heading to the coast I had to drive through this ugly fog bank and the whole time I'm thinking, I'm driving 5 hours to the coast and I won't even be able to see the water. Turns out, I was worried over nothing. About 30 miles from the coast it was clear skies all the way.
Johnson Bay in Lubec, Maine. Lubec is the Easternmost town in the US. The trees peeking through the fog are on Canada's Campobello island.
Shown at 2017 PSA International Exhibition of Photography and India Photo Circuit
Morning fog. Tuscany 31/03/2015.
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Image is under Copyright by Fabrizio Massetti. Pictures can not be used without explicit permission . Contact me by email if you want to buy or use my photographs
Back around on this shot. Adding a little touches in post processing.
Taken at Wildwood Park, Harrisburg, Pennsylvania.
Thanks for stopping to look!
Taken about an hour after sunrise on a cold foggy morning at Red Rock near Colac in Victoria, Australia. It was a photographers morning as the colours continued to change as the sun commenced its climb. . . . .Sigma 70 -300mm f4 -5.6 APO DG Macro
Fog can be considered a cloud at ground level. The processes forming it, however, are usually different from those that form clouds.
Like clouds, fog is made up of condensed water droplets which are the result of the air being cooled to the point (actually, the dewpoint) where it can no longer hold all of the water vapor it contains.
For clouds, that cooling is almost always the result of rising of air, which cools from expansion. But for fog, which occurs next to the ground, there are usually other reasons for this cooling.
For instance, rain can cool and moisten the air near the surface until fog forms.
Or, as is more often the case, infrared cooling of a cloud-free, humid air mass at night can lead to fog formation - this is called "radiation fog". Radiation fog is most common in the fall, when nights get longer, airmasses begin to cool, and land and water surfaces that have warmed up during the summer are still evaporating alot of water into the atmosphere.
Finally, a warm moist air mass blowing over a cold surface (usually snow or ice, or over a cold ocean surface) can also cause fog to form-this is called "advection fog