First let's define the «equilibrium climate sensitivity» as the «equilibrium change in global
mean surface temperature following a doubling of the atmospheric (equivalent) CO2 concentration.
Not exact matches
One common measure of climate sensitivity is the amount by which global
mean surface temperature would change once the system has settled into a new equilibrium
following a doubling of the pre-industrial CO2 concentration.
So, it
follows on phtysical grounds that any
temperature change at the
surface gets amplified aloft which
means that the variability in
temperature (solely the «dry» energy term) is larger aloft than at the
surface.
One common measure of climate sensitivity is the amount by which global
mean surface temperature would change once the system has settled into a new equilibrium
following a doubling of the pre-industrial CO2 concentration.
I for one would like to see a
follow up of the current work by Dr. Benestad that more clearly defines the
means of «cause and effect» and how this is resulting in high
surface temperatures.
where DTHx denotes the global
mean surface temperature change after H years
following an emission of compound x.
The GTP is defined as the ratio between the global
mean surface temperature change at a given future time horizon (TH)
following an emission (pulse or sustained) of a compound x relative to a reference gas r (e.g., CO2):
how much trust do you have in this type of model to predict
mean surface temperature for the next five or ten decades (given an emission scenario
following Hoffman).
Also, were you to speak without your scientific cap on, how much trust do you have in this type of model to predict
mean surface temperature for the next five or ten decades (given an emission scenario
following Hoffman).
equilibrium climate sensitivity refers to the equilibrium change in the annual
mean global
surface temperature following a doubling of the atmospheric equivalent carbon dioxide concentration.
The climate sensitivity parameter (units: °C (W m - 2)-1) refers to the equilibrium change in the annual
mean global
surface temperature following a unit change in radiative forcing.
Climate sensitivity - In Intergovernmental Panel on Climate Change (IPCC) reports, equilibrium climate sensitivity refers to the equilibrium change in the annual
mean global
surface temperature following a doubling of the atmospheric equivalent carbon dioxide concentration.
It is broadly defined as the equilibrium global
mean surface temperature change
following a doubling of atmospheric CO2 concentration IPCC Fourth Assessment Report: Given that CO2 has been going up in a regular stepwise fashion for the last 30 years and there has been an initial jump in temps which was happily aligned with this with Mann like Climate sensitivity, Climate sensitivity might well have been 6.0.
«TCR is defined as the annual
mean global
surface temperature change at the time of CO2 doubling
following a linear increase in CO ₂ forcing over a period of 70 years»
There is very high confidence that models reproduce the general features of the global - scale annual
mean surface temperature increase over the historical period, including the more rapid warming in the second half of the 20th century, and the cooling immediately
following large volcanic eruptions...
How can you tell that the TOA perspective, accurate to «first - order», is accurate enough to calculate the change in the
mean surface temperature (
following an increase in forcing at the
surface) to the first significant figure?
2) The HadCRUT4 global
mean surface temperature dataset shows a warming of 0.6 deg C from 1974 to 2004 as shown in the
following graph.
It is broadly defined as the equilibrium global
mean surface temperature change
following a doubling of atmospheric CO2concentration.»