Difference between revisions of "Average surface temperature"

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The '''average surface temperature''' on the earth is 15, maybe 16 degrees [[Celsius]] (60 degrees [[Fahrenheit]])," said Alan Robock, a [[meteorologist]] and climate researcher from [[Rutgers University]]. <ref>http://www.livescience.com/environment/060925_temperatures_high.html</ref>
 
The '''average surface temperature''' on the earth is 15, maybe 16 degrees [[Celsius]] (60 degrees [[Fahrenheit]])," said Alan Robock, a [[meteorologist]] and climate researcher from [[Rutgers University]]. <ref>http://www.livescience.com/environment/060925_temperatures_high.html</ref>
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[[Meteorology|Meteorologists]] find it through measuring the heat in the [[ocean]]s, [[atmosphere]], as well as different places on the land. They use primarily satellites today.
  
 
* The average temperature of the Earth has varied within a range of about 3°C during the past 3,000 years. It is currently increasing as the Earth recovers from a period that is known as the [[Little Ice Age]].<ref>[http://www.oism.org/pproject/s33p36.htm Environmental Effects of Increased Atmospheric Carbon Dioxide]</ref>
 
* The average temperature of the Earth has varied within a range of about 3°C during the past 3,000 years. It is currently increasing as the Earth recovers from a period that is known as the [[Little Ice Age]].<ref>[http://www.oism.org/pproject/s33p36.htm Environmental Effects of Increased Atmospheric Carbon Dioxide]</ref>
 
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==References==
 
==References==
  
 
<References/>
 
<References/>
  
[[Category:Geology]]
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[[Category:Geology]][[Category:Meteorology]][[Category:Climate change]]

Revision as of 17:20, May 23, 2008

The average surface temperature on the earth is 15, maybe 16 degrees Celsius (60 degrees Fahrenheit)," said Alan Robock, a meteorologist and climate researcher from Rutgers University. [1]

Meteorologists find it through measuring the heat in the oceans, atmosphere, as well as different places on the land. They use primarily satellites today.

  • The average temperature of the Earth has varied within a range of about 3°C during the past 3,000 years. It is currently increasing as the Earth recovers from a period that is known as the Little Ice Age.[2]

References