WeatherQuesting
with April Holladay
to solve weather mysteries, your wonders.

Also, WonderQuest with April Holladay
 

Home   Top 10    Newsletter    Fast answers    Site Map

Google
 
Web www.WeatherQuesting.com


RSS Add to Google

Answers about:  

_   Lightning
_ Clouds

Top 10 questions  

1

 Cause of  lightning

2

 Where lightning hits

3

 Hurricane spin

4

 How hot is lightning

5

 Jupiter's surface

6

 How rainbows form

7

 Ball lightning

8

 Hurricane energy

9

 Lightning hits a tornado
10  Orange night skies

Current Column:  A saintly light

st elmo's fire

Why would a lightning-struck tree glow after being hit? It is not on fire and does not give off heat, but glows. 

It was a dark and stormy night.  Chris emails he was walking in the woods  "a little after a thunderstorm" when he noticed the tree.  The tree, shattered by an earlier lightning stroke, stabbed the night like a broken pike.  An eerie glow extended ... Click to continue

Cold mountain

Mountains stick up like islands in the cold atmosphere [Sean Linehan, NOAA]Why is it colder in the mountains than in the valley? The mountains are closer to the sun. Marissa, Mountain Home, Idaho

The Sun’s rays pass right through the atmosphere. Earth’s surface absorbs them and re-radiates the energy in the form of heat that air can absorb. Thus, the Sun warms the air by warming the ground. Air closest to the Earth’s surface is, in general, warmest. Air as high as a mountain is poorly warmed and, therefore, cold.

Mountains stick up like islands in the cold atmosphere.  Photo courtesy of Sean Linehan, NOAA.

Air temperature normally drops 1.8 to 3.6 degrees Fahrenheit (1 to 2 degrees Celsius) for each 1000 feet (300 m) of altitude.

Mountains poke up through the atmosphere like islands above a sea. The temperature of the enveloping atmosphere cools mountain ground even though — you’re right — the Sun warms the high ground. The influence of atmosphere temperature on a mountain is similar to that of the sea’s temperature on an island. The higher and the more isolated the mountain, the closer its temperature is to the cold air around.

Mountain weather, however, is fickle — changing like a shifting kaleidoscope with every passing cloud or gust of wind. The soil surface on a mountain can get hotter than the valley soil surface because of the Sun’s greater intensity up high where the air is thin and clean.

Mountain soil can be as hot as desert dirt. In the Alps at 6800 feet (2070 m), the soil temperature one day shot up to 180 degrees F (80 degrees C) on a dark humus slope near the timberline. The slope faced southwest at a gradient of 35 degrees. Dark humus soil absorbs the Sun’s energy better than light sandy soil. A southwest-facing slope of 35 degrees in the Alps receives the Sun’s rays more directly than does flat ground.

A mere five feet above the warm surface, however, was frigid, cooled by the surrounding atmosphere. Alpine plants grow low to the ground — to stay warm.

Further Surfing:

University of Colorado: Mountain climate by A. Bach

(Answered Feb. 27, 2004; updated Nov.1, 2007)

Click for printer version.

Site Map

Archive Features Info
Question Archive WeatherQuesting's Search
    Ask a question About April

 

  Lightning Rain & snow   Top 10 questions Add RSS feed to Google

 

  Sky wonders  Seasons   Newsletter Contributors
    Extraterrestrial Climate      
    Clouds Winds Correspondents' April's 1000-mile paddle to the Arctic Ocean
    Extremes & freaks Forecasts   Weather forecast at any location April's mountain and desert life
    Atmosphere        
             
             
       

  Copyright 2007 by April Holladay