Not exact matches
I guess I am surprised that with better understanding of the importance of water vapor feedback, sulfate aerosols, black
carbon aerosols, more rapid than expected declines
in sea ice and attendant decreases
in albedo, effects of the deposition of soot and dust on snow and ice decreasing
albedo, and a recognition of the importance of GHGs that were probably not considered 30 years ago, that the sensitivity has
changed so little over time.
That's pretty alarming, especially when considered
in the context of other positive feedbacks including
changes in albedo from melting icecaps and release of
carbon and methane from thawing permafrost.
I guess I am surprised that with better understanding of the importance of water vapor feedback, sulfate aerosols, black
carbon aerosols, more rapid than expected declines
in sea ice and attendant decreases
in albedo, effects of the deposition of soot and dust on snow and ice decreasing
albedo, and a recognition of the importance of GHGs that were probably not considered 30 years ago, that the sensitivity has
changed so little over time.
The
change in ice volume and climate
changes the planets
albedo (how much sunlight is reflected) and affect
carbon storage.
, (3)
changes in surface
albedo of snow & ice due to
changes in temperature and deposition of mineral and black
carbon particulates, and last, but arguably most significantly (4) the intensity of the positive feedback that comes from the inevitable -LRB-?)
My reasoning was that, iirc, black
carbon has played an important role
in the ice loss by
changing albedo.
Other feedbacks include seasonal shift, latitudinal shift,
changes in ice
albedo and the
carbon sink and many more.
Based on evidence from Earth's history, we suggest here that the relevant form of climate sensitivity
in the Anthropocene (e.g. from which to base future greenhouse gas (GHG) stabilization targets) is the Earth system sensitivity including fast feedbacks from
changes in water vapour, natural aerosols, clouds and sea ice, slower surface
albedo feedbacks from
changes in continental ice sheets and vegetation, and climate — GHG feedbacks from
changes in natural (land and ocean)
carbon sinks.
Broad - scale
changes in vegetation
in general, and tree loss
in particular, have pronounced effects on climate processes through biogeophysical mechanisms such as
albedo, evapotranspiration (ET), and
carbon dioxide exchange with the atmosphere [11].
He'd been studying
changes in Greenland's
albedo (the scientific term for the reflectivity of ice), but hadn't focused on the role of black
carbon.
This leads me to believe that CO2 forcing is a minor component of the temperature rise (even Hansen
in his paper «Global Warming
in the 21st century, an Alternative Scenario» has assigned much warming to e.g. black
carbon, methane etc, and an inquisitive mind might easily think of others such as
albedo change).
And we don't have to go back all that far to get
changes in carbon dioxide
in the atmosphere and quite unknowable
albedo effects.
25 Uncertainties
Changes in atmospheric water vapor —
Changes in cloudiness —
Changes in albedo Carbon budgets Aerosol particles — Direct effects — Impact on clouds — Black
carbon