Wouldn't it be a pretty good first approximation to model a one square meter of earth and the atmosphere above
it with average albedo, average solar input, average cloud cover, etc?
Not exact matches
[1] CO2 absorbs IR, is the main GHG, human emissions are increasing its concentration in the atmosphere, raising temperatures globally; the second GHG, water vapor, exists in equilibrium
with water / ice, would precipitate out if not for the CO2, so acts as a feedback; since the oceans cover so much of the planet, water is a large positive feedback; melting snow and ice as the atmosphere warms decreases
albedo, another positive feedback, biased toward the poles, which gives larger polar warming than the global
average; decreasing the temperature gradient from the equator to the poles is reducing the driving forces for the jetstream; the jetstream's meanders are increasing in amplitude and slowing, just like the lower Missippi River where its driving gradient decreases; the larger slower meanders increase the amplitude and duration of blocking highs, increasing drought and extreme temperatures — and 30,000 + Europeans and 5,000 plus Russians die, and the US corn crop, Russian wheat crop, and Aussie wildland fire protection fails — or extreme rainfall floods the US, France, Pakistan, Thailand (driving up prices for disk drives — hows that for unexpected adverse impacts from AGW?)
(Orbital forcing doesn't have much of a global annual
average forcing, and it's even concievable that the sensitivity to orbital forcing as measured in terms of global
averages and the long - term response (temporal scale of ice sheet response) might be approaching infinity or even be negative (if more sunlight is directed onto an ice sheet, the global
average albedo might increase, but the ice sheet would be more likely to decay,
with a global
average albedo feedback that causes warming).
Orbital forcing causes ice ages or ends them by redistributing incoming solar radiation over seasons and latitudes so that ice sheet growth or decay is more or less favorable on a regional basis,
with a resulting global
average albedo feedback.)
So we are left
with little sense of how much some «
average» macrovariables like
albedo, vary day to day and hour by hour as clouds come and go and land use and natural cover vary
That is an
average available
with an assumed fixed
albedo.
Taking the pessimistic assumption that there would eventually be an «ice free summer» in the Arctic, I come up
with a future reduction of the
average albedo of the Earth of:
When the planet's sun is 4 billion years younger it's output is 33 % less than it is today, so under clear skies
with an
albedo for water of 0.1, the
average incident solar energy would be ~ 274 watts / m2.
It is arguably one of the most advanced of the seven in its impacts,
with a 2011 GRL report putting its warming effect as equivalent to around 30 % of atmospheric anthro - CO2, and the recent report putting
albedo loss from arctic sea - ice decline since»79 as providing a forcing equivalent on
average to that from 25 % of the anthro - CO2 levels during the period.
Given a planet
with a certain
albedo, a certain distance from a star of a given luminosity, one can determine what the
average temperature of the planet would be in the absence of a greenhouse effect.
The solar flux is 1366 watts per sq m so
with the hemisphere having twice the cross sectional area this
averages to 688 watts / sq m The
albedo reduces this by 30 % to 478 watts / sq m About half of this energy is incorporated into the Earth systems growing plants creating weather etc leaving 239 watts / sq m which must be returned to space.
The 21st century can be expected to be
with lower solar activity, less deflection of cloud - seeding galactic cosmic rays, higher
average cloud cover, a more reflective planetary
albedo, and a cooler planet..
Given the earth
with an
albedo similar to the moon (i.e. all rocks) it would have an
average surface temperature well below freezing.
In the absence of absorption of terrestrial radiation by the atmosphere (and
with the other caveats about still having the same
albedo and such), that
average temperature would have to be 255 K at the surface because of radiative balance and then the temperature would decrease
with height at the lapse rate from there.
For example, the global
average effect of any change in
albedo from using solar power would be rather small in comparison to mitigation of climate change if that solar power is used (to displace fossil fuels) for a sufficient time period (example: if a 10 % efficient PV panel
with zero
albedo (reflectivity for solar (SW) radiation) covered ground
with an
albedo of 25 — 30 %, the ratio of total increased heating to electricity generation would be similar to that of many fuel - combusting or fission - powered power plants (setting aside inverter and grid efficiency, etc., but still it would be similar).
The problem doesn't go away however because the earth has a non-zero
albedo too and it isn't known nearly as well as the moon's
with, depending on who you ask, an
average albedo in the range of 32 % which is primarily the result of some 70 % being shrouded by clouds of some sort at any given instant.
Obviously, we are currently in transition and our global atmospheric cell structures are going to shift rapidly
with broadly expanding Hadley cell and collapsing Arctic cell leading to meridional migration of
average cloud cover and reduced
albedo.
Hence this wild notion on the problem of
albedo, how do we define the
average colour of your classic redhead in prime condition but
with lots of freckles?
In the almost sure knowledge that the earth never experienced a runaway greenhouse even
with ancient CO2 levels 10 to 20 times greater than today, these anti-science scoundrels insist
with a «high level of confidence» that this amplification is real and it's based on nothing more than faster than expected surface temperature rise in the past few decades which can be TOTALLY explained by multi-decadal cyclic behavior in ocean currents, trade winds, and / or solar magnetic activity causing small global
average albedo changes.