(1) 14C injected into the stratosphere did have a long residence time and
did equilibrate over a number of years.
Some part of the response
does equilibrate within decades but a lot of the rest (easily half) takes a thousand years to be realized.
Not exact matches
This is basically me on most days, but I feel like I've
equilibrated to the point where it doesn't feel that crazy - hectic to me anymore.
«Third, the «forcing» can not be possibly ever observed in laboratory conditions because the definition of forcing contains three physically unrealizable conditions: (a) CO2 mixes up, but temperature profile stays the same, (b) stratospheric cooling
equilibrates with tropopause conditions before troposphere
does, and (c) troposphere - surface interface is kept frozen.
The phrase «stratospheric cooling
equilibrates with tropopause conditions before troposphere
does» is also meaningless.
How
does cooling in the stratosphere «
equilibrate» with conditions at the tropopause?
The authors speculate that the main reason hurricanes show this delta is that more of the precipitation is coming from high altitude (depleted in O - 18 based on gravitational potential) and in the form of large drops that
do not have time to
equilibrate wrt O - 18 in lower regions of the cloud as they fall.
That layer
does not, as IPCC claims,
equilibrate on a time scale of a year or any other length of time.
I understand that bottom ocean
does not
equilibrate with 5000C of Earth crust because of slow mixing with colder water coming from arctic, as explained by michael sweet@11, thanks!.
Once the ocean has
equilibrated to an impulse of CO2 with a half - life of ~ 5 years, both the ocean and the atmosphere have a higher level of carbon than they
did before.
If it doesn't stay long enough then it can't
equilibrate with others and there is no LTE.
When they finally
equilibrate do they stop radiating??
Kuhnkat: When they finally
equilibrate they
do not stop radiating (transferring energy).
We know that forcings don't instantaneously result in temperature changes - it takes time for the climate to
equilibrate.
The way I interpret that is that the higher climate sensitivity must either involve different heat transfer modes / patterns, or that it involves a different temperature rise path, with more of the increase backloaded (ie if most of the increase for high sensitivity comes after 2070, then there's less time for the oceans to
equilibrate than there would be, if most of the temperature increase was
done by 2030).
In this paper we explore if and how the marginal criticality and radiative constraints
do work together to produce an
equilibrated flow and a tropopause that is internal to the fluid.
While it is no perfect solution either (and there probably is none), the Advocate General's solution of
doing exactly the same thing the other way round — offering the action for damages as consolation for the party that has previously benefitted from an erroneous transformation of EU law by the Member State and now pays the price because of horizontal direct effect excluding the application of a norm of national law they had relied on — has at least a somewhat more
equilibrated approach towards sharing the burden of advantages and disadvantages.