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- Dec 22, 2012
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Most of you probably remember me speaking of evapotranspiration. I don't think any of you realize how serious of an influence it is on stationary meteorological station, most of which are close enough to metro areas to be highly influenced.
I have looked and looked. Maybe I'm just not good at searching. All I find is evapotranspiration changes by changing the landscape with things like crops. I have looked for the influence of this phenomena regarding the replacement of the natural landscape with asphalt, concrete, and building.
My searches have yielded no results. Anyone care to help?
I did some quick calculations one day pertaining to where I live in the Portland metropolitan area. We have an average rainfall of 42 inches. Before mankind ever changed the land, a significant portion of this rainfall would end up evaporating from the land, or released from plants into the atmosphere. What didn't return to the atmosphere, would make its way to steams, rivers, etc. and back to the ocean.
I will assume for calculations, with a wide error margin, that 70% of this rainfall would end up back into the atmosphere before 1850, and 20% in present times. This assumes a 50% loss of the evaporative cooling potential from 21 inches of rain for the year in the Portland metro area.
The warmers (deniers of science) will find some way to deny the facts.
To convert to W/m^2, we need the heat of vaporization and seconds per year.
Seconds per year: 31,536,000 (60 x 60 x 24 x 365)
Heat of vaporization: 2257 joules/gram
21" of water represent 0.53 cubic meters. This water weighs 530 kg.
530,000 x 2257 = 1,196,210,000 joules of energy over a 1 meter patch of earth.
1,196,210,000 / 31,536,000 = 37.9 W/m^2 of energy. No wonder the urban heat island effect is so strong.
I'm sure the deniers of science will find reason to scoff at my calculations here, so by all means, do it yourself.
Of course the winds mix the air from areas not affected, but this is a huge change for many metropolitan areas.
I have looked and looked. Maybe I'm just not good at searching. All I find is evapotranspiration changes by changing the landscape with things like crops. I have looked for the influence of this phenomena regarding the replacement of the natural landscape with asphalt, concrete, and building.
My searches have yielded no results. Anyone care to help?
I did some quick calculations one day pertaining to where I live in the Portland metropolitan area. We have an average rainfall of 42 inches. Before mankind ever changed the land, a significant portion of this rainfall would end up evaporating from the land, or released from plants into the atmosphere. What didn't return to the atmosphere, would make its way to steams, rivers, etc. and back to the ocean.
I will assume for calculations, with a wide error margin, that 70% of this rainfall would end up back into the atmosphere before 1850, and 20% in present times. This assumes a 50% loss of the evaporative cooling potential from 21 inches of rain for the year in the Portland metro area.
The warmers (deniers of science) will find some way to deny the facts.
To convert to W/m^2, we need the heat of vaporization and seconds per year.
Seconds per year: 31,536,000 (60 x 60 x 24 x 365)
Heat of vaporization: 2257 joules/gram
21" of water represent 0.53 cubic meters. This water weighs 530 kg.
530,000 x 2257 = 1,196,210,000 joules of energy over a 1 meter patch of earth.
1,196,210,000 / 31,536,000 = 37.9 W/m^2 of energy. No wonder the urban heat island effect is so strong.
I'm sure the deniers of science will find reason to scoff at my calculations here, so by all means, do it yourself.
Of course the winds mix the air from areas not affected, but this is a huge change for many metropolitan areas.