Global warming and CO2 hotspots?

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SUMMARY

This discussion centers on the relationship between CO2 emissions from industrial sites and their impact on global warming, specifically addressing the existence of CO2 hotspots and coldspots. Jos de Laat's research highlights localized effects of industrial emissions, while historical studies, such as those by Priestley (1966), discuss the limitations of temperature due to evaporation. The conversation also explores the dynamics of water vapor and its role in climate feedback mechanisms, concluding that the energy required for increased evaporation may counterbalance the effects of CO2-induced warming, thus preventing runaway feedback loops.

PREREQUISITES
  • Understanding of CO2 emissions and their sources, particularly from industrial activities.
  • Familiarity with climate feedback mechanisms, including the role of water vapor.
  • Knowledge of the Clausius-Clapeyron relationship regarding temperature and evaporation.
  • Basic comprehension of energy balance in climatic systems.
NEXT STEPS
  • Research the findings of Jos de Laat on localized climate effects in industrial areas.
  • Study the Clausius-Clapeyron equation and its implications for climate science.
  • Examine the historical context of temperature limitations due to evaporation as discussed by Priestley (1966).
  • Investigate the energy dynamics of evaporation and its relationship to greenhouse gas concentrations.
USEFUL FOR

Climate scientists, environmental researchers, policymakers, and anyone interested in the intricate relationships between industrial emissions, water vapor, and climate feedback mechanisms.

battery
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If CO2 produced by industry is causing global warming then wouldn't there be hotspots above major industrial sites where the CO2 is most concentrated?
And wherever in the world CO2 is washed out of the air by heavy rainfall, shouldn't there be CO2 coldspots too?
If CO2 warming is increasing average wind speeds then are the increases in wind speeds around CO2 hotspots greater than elsewhere?
I read on wikipedia that if the Earth warms up then more water vapour is produced and this in turn leads to more heat being trapped and more water vapour forming and so on.What stops this positive feedback cycle from getting out of control? Do clouds form when the air reaches a certain humidity level and do the clouds then reflect sunlight back into space?
 
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battery said:
If CO2 produced by industry is causing global warming then wouldn't there be hotspots above major industrial sites where the CO2 is most concentrated?
And wherever in the world CO2 is washed out of the air by heavy rainfall, shouldn't there be CO2 coldspots too? If CO2 warming is increasing average wind speeds then are the increases in wind speeds around CO2 hotspots greater than elsewhere?

Jos de Laat has done some research to local effects on industrial areas here:
http://www.knmi.nl/~laatdej/2006joc1292.pdf

I read on wikipedia that if the Earth warms up then more water vapour is produced and this in turn leads to more heat being trapped and more water vapour forming and so on.What stops this positive feedback cycle from getting out of control? Do clouds form when the air reaches a certain humidity level and do the clouds then reflect sunlight back into space?

In the old days, the physics of water vapor was quite different:

Priestley, C.H.B., 1966. The Limitation of Temperature by Evaporation in Hot Climates. Agricultural Meteorology, 3 (1966) 241-246.

From general considerations of energy balance it is argued that one might expect a rather sharply defined upper limit to which screen air temperature will rise above a well-watered underlying surface of sufficient extent. A study of world-wide climatic data supports this view and identifies the limiting temperature as about 92F (+/- 1F). Temperatures over wet terrain within a few degrees of this limit occur widely and frequently.

the logic of which is in the Clausius Clappeyron exponential relationship between temperature and evaporation for a constant relative humidity.

For ballpark figures, from http://www.usclivar.org/Organization/Salinity_WG/workshoppresentations/Evp-salinityLisanYu.pdf let's assume average annual evaporation of a meter per year. That's 2.74 liters (2740 g) per m2 per day or 114 g per hour is 0.032 gram per second. It takes 2500 joule to evaporate one gram of water, so for 0.032 gram that's 79 joule per second per square meter or 79 W/m2

Now to keep relative humidity constant when increasing the ambient temperature of 15 C to 16 C, suppose a dewpoint of about 9 degrees we see http://www.humirel.com/All_about_humidity-calculation2.htm a decrease of 67% to 63%. Obviously we also have to raise the dewpoint one degree to get back to 67% Now the absolute humidity calculated http://www.humirel.com/All_about_humidity-calculation4.htm goes from 9 gram/m3 at a dewpoint of 9 degrees to 9.6 gram/m3 at a dewpoint of 10 degrees, an increase of 7%. To sustain an increase of 7% more water vapor in the atmospere it seems logical that the rate of evaporation also has to increase by 7% as well, which in turn requires 7% more energy. Hence I'd need 7% of 79 W/m2 or 5.5 W/m2 extra to maintain constant relative humidity. However the additional energy associated with doubling CO2 is about 3.4-4.0 W/m2

So it appears that the exponential increase of energy required for evaporation exceeds the increase due the enhanced greenhouse effect, killing the positive feedback.
 
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