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re: Is Water Vapor a Greenhouse Gas? If not what are the implications?

Posted on 3/25/14 at 11:10 am to
Posted by GumboPot
Member since Mar 2009
119114 posts
Posted on 3/25/14 at 11:10 am to
quote:

Mandeville averages lower temperatures


Lower lows and higher highs = Mandeville (when New Orleans in under lake effect conditions) = lower relative humidity = less water vapor concentrations = less negative feedback.

Higher Lows and lower highs = New Orleans (when New Orleans is under lake effect conditions) = higher humidity = more water vapor concentrations = more negative feedback.

Positive feedback exasperates a condition (higher positive and lower negatives). Negative feedback stabilizes a condition (lower positives and higher negatives).

Lake effect on New Orleans occurs when the wind gently blowing out of the north.
Posted by PaddlingTiger
St. Louis, MO
Member since Jun 2010
1066 posts
Posted on 3/25/14 at 11:28 am to
What you are describing is the fact that water vapor (and corresponding clouds) both prevent heat from reaching the surface of the Earth and trap heat on the surface of the Earth. With less clouds and water vapor, more heat hits the Earth (higher highs) and more heat dissipates at night (lower lows). To understand the overall impact, you look at the average temperatures. As you noted, Mandeville has lower average temperatures than New Orleans and corresponding lower water vapor levels. While one example does not prove much of anything, at least in your example, water vapor appears to be a positive feedback loop to surface temperature as it appears, based on the information you posted, more heat is trapped by clouds (higher average surface temperature)than escapes from the lack of clouds. I am not making a broader statement about water vapor, as one example is certainly not enough, this is just analyzing the info you posted.
This post was edited on 3/25/14 at 11:31 am
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