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- Alpenglow - Wikipedia
Alpenglow (from German: Alpenglühen, lit 'Alps glow'; Italian: enrosadira) is an optical phenomenon that appears as a horizontal reddish glow near the horizon opposite to the Sun when the solar disk is just below the horizon
- What is the Alpenglow and how to observe it - Windy. app
The Alpenglow or Alpine glow belongs to the section of meteorology called “Atmospheric optics” It is a glow that occurs on the mountaintops, on which this effect is best seen, at sunset or dawn when the sun goes behind the horizon or appears from behind it
- Alpenglow - Sunrise Sunset Predictor
Alpenglow v10 1 now includes the ability to view the sun's path across the sky for any day, time and location Alpenglow is updated ready for Apple's latest operating systems Here's what you can find in the latest update How are Sunrise Sunset Forecasts calculated? Forecasts are generated by our friends at SunsetWX
- Alpenglow photos, definition, and cause - SnowSlang. com
Alpenglow, from the German word alpenglühen for “Alp glow”, refers specifically to the rosy hue of mountains after dawn and before dusk It’s especially pronounced when mountains are snow-covered and offer a blank canvas on which the light can play
- ALPENGLOW Definition Meaning - Merriam-Webster
The meaning of ALPENGLOW is a reddish glow seen near sunset or sunrise on the summits of mountains
- EXPLAINER: The phenomenon behind alpenglow - Buckrail
Alpenglow is an atmospheric optical phenomenon that makes mountains appear to glow in a light pink or red hue It occurs just after the Sun sets or just before it rises
- What Is Alpenglow? - Digital Photography School
Alpenglow is simply redirected light Think of the clouds and atmosphere as a giant strobe reflector Think of the sun as a giant strobe (for which, there is no PocketWizard controls) In the image art right, the entire scene is lit from light bouncing off the atmosphere and hitting Seattle and Mt Rainier
- alpenglow - Glossary of Meteorology
Alpenglow has three phases During evening twilight, the first stage is the mountain peak's usual coloration seen at low sun elevations h0 (h0 < 2°) Second is the alpenglow proper that occurs a few minutes after the first color has faded (h0 slightly less than 0°)
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