This is not purely a thermodynamic response to the reduction
in planetary albedo at these latitudes.
This study uses satellite radiation budget measurements along with satellite microwave sea ice data to document the Arctic - wide decrease
in planetary albedo and its amplifying effect on the warming.
Greenhouse warming that is stronger over land and in the Northern Hemisphere tends to strengthen the monsoon, but increases
in planetary albedo over the continent due to aerosol forcing and / or land - use change tend to weaken it.
Rayleigh - Benard Convection cloud physics result in changes
in planetary albedo.
, a change
in planetary albedo (forest die off?)
The identified atmospheric feedbacks including changes
in planetary albedo, in water vapour distribution and in meridional latent heat transport are all poorly represented in zonal energy balance model as the one used in [7] whereas they appear to be of primary importance when focusing on ancient greenhouse climates.
It is well known that multiple factors are involved, including the change
in planetary albedo, change in nitrous oxide concentration, change in methane concentration, and change in CO2 concentration.
This implies that the CRF levels must have systematically decreased over time, causing a long - term decrease in the low cloud fraction and hence a long - term reduction
in the planetary albedo, that again would be responsible for the warming.
Not exact matches
Nicholson says that even if research agencies under Trump avoid research into geoengineering techniques such as
albedo modification, the U.S. intelligence community might remain interested, especially
in whether other countries are pursuing their own
planetary cooling technologies, which could affect many nations.
The solar radiative forcing is TSI
in Watts per square meter (W - m - 2) divided by 4 to account for spherical geometry, and multiplied by 0.7 to account for
planetary albedo (Meehl 2002).
For each
planetary candidate, the equilibrium surface temperatures are derived from «grey - body spheres without atmospheres... [and] calculations assume a Bond
albedo of 0.3, emissivity of 0.9, and a uniform surface temperature... [with uncertainties of] approximately 22 %... because of uncertainties
in the stellar size, mass, and temperature as well as the
planetary albedo.»
The idea was that the resulting increase
in aerosol would increase the brightness and lifetime of low maritime clouds, increasing the
planetary albedo.
To make such statements wouldn't we have to know the 3 - D dust field
in the LGM and the impact of those aerosols on clouds (and
planetary albedo)?
These findings are remarkable insofar as they indicate that anthropogenic perturbations of the
planetary albedo, such as sulphur emissions and / or land - use changes, or natural variations
in insolation and CO2 concentration could trigger abrupt transitions between different monsoon regimes.
«Our results suggest that,
in contrast to other proposals to increase
planetary albedo, offsetting mean global warming by reducing marine cloud droplet size does not necessarily lead to a drying, on average, of the continents.
However, even a smaller figure (I had calculated about 0.17 W / m ^ 2 based on your inflated figure for total
planetary albedo, but you can check it out) is still significant when compared with the total flux imbalance, which I think is a more informative comparison than an arbitrarily selected change
in cloud cover, because it compares the sea ice reduction with the effects of all climate variations that have been operating
in recent years..
The real «flat plate» GHE is between 11 and 17 K depending on your estimate of present
albedo and
planetary emissivity
in the absence of GHGs.
Found Joseph Postma's derivation of the formulae for calculating
planetary temperature very helpful, even if I think he has made a small mistake
in failing to account for both
albedo and emissivity.
But whether someone chooses to use the term
Albedo or Bond albedo it doesn't appear as though anyone has actually got right the values for the Bond albedo on any planetary body or any object in space - and as result still getting a ballpark n
Albedo or Bond
albedo it doesn't appear as though anyone has actually got right the values for the Bond albedo on any planetary body or any object in space - and as result still getting a ballpark n
albedo it doesn't appear as though anyone has actually got right the values for the Bond
albedo on any planetary body or any object in space - and as result still getting a ballpark n
albedo on any
planetary body or any object
in space - and as result still getting a ballpark number.
The cause could be any short or long term change
in a number of things solar output, ocean heat release,
planetary albedo, vapor, whatever.
Increased biomass can lead to increased emissions of biogases such as dimethyl sulfide and isoprene, which when oxidized
in the atmospheric form sulphate and organic aerosols that can nucleate clouds, increasing cloud cover and
planetary albedo — the CLAW Hypothesis.
In order to determine the solar contribution, we have to start with the solar radiative forcing, which is the change in total solar irradiance (TSI) in Watts per square meter (W / m2) divided by 4 to account for spherical geometry, and multiplied by 0.7 to account for planetary albedo (Meehl 2002
In order to determine the solar contribution, we have to start with the solar radiative forcing, which is the change
in total solar irradiance (TSI) in Watts per square meter (W / m2) divided by 4 to account for spherical geometry, and multiplied by 0.7 to account for planetary albedo (Meehl 2002
in total solar irradiance (TSI)
in Watts per square meter (W / m2) divided by 4 to account for spherical geometry, and multiplied by 0.7 to account for planetary albedo (Meehl 2002
in Watts per square meter (W / m2) divided by 4 to account for spherical geometry, and multiplied by 0.7 to account for
planetary albedo (Meehl 2002).
Global temps vary for many reasons beyond CO2 levels including but not limited to:
planetary motion, changes
in albedo, stratospheric aerosols, and solar variability to name a few, but the only area of genuine study by the IPCC has been rising CO2 levels.
Planetary albedo: The fraction of incident solar radiation that is reflected by the Earth - atmosphere system and returned to space, mostly by back scatter from clouds
in the atmosphere.
The authors» argue that early life may perform a vital regulating function on an early
planetary environment by impacting both the planet's
albedo (how much light it reflects from the sun) and the greenhouse gases present
in its atmosphere.
quote from the article: For example,
in the analysis, not only does the amount of CO2 not enter
in (Earth has 0.04 %, Venus a whopping 96.5 %), but the
albedo (from either cloud tops or the
planetary surface) does not either (Venus has dense clouds that reflect much of the incident visible radiation, while Earth does not, and Earth's surface is 70 % deep ocean, while Venus is solid crust).
In the past few years several attempts have been made to assess changes in the Earth's planetary albedo, and claims of global dimming and more recently brightening have been debated in journal articles and blogs alik
In the past few years several attempts have been made to assess changes
in the Earth's planetary albedo, and claims of global dimming and more recently brightening have been debated in journal articles and blogs alik
in the Earth's
planetary albedo, and claims of global dimming and more recently brightening have been debated
in journal articles and blogs alik
in journal articles and blogs alike.
Part of the changes
in the spatial correlations is expected to be due to convection and clouds, which too play a role for the GHG,
in addition to influencing the
planetary albedo.
I would not regard heat being stored
in the ocean and melting snow / ice but not completely melting it (and thereby changing the surface
albedo), since this does not have any sort of direct change to the
planetary radiative fluxes.