The phrase
"climate response" refers to the actions or measures taken to address or adapt to the changes happening in the Earth's climate. It involves different strategies and efforts aimed at minimizing the negative impacts of climate change and ensuring a sustainable and resilient future.
Full definition
Each mechanism fails to generate the expected
climate response in important respects, although some relations are found.
The growing research area of extreme event attribution has provided pertinent scientific evidence for a number of such warm events for which the
forced climate response rises above internal climatic variability.
Any increase in our estimate of the
natural climate responses to past forcings points to a more variable future path with larger average changes.
So if you're concerned about climate change as a major issue then you may want to consider switching to a party that supports
climate responses more readily.
Corporate Climate Response events bring together companies, regulators and other carbon experts to discuss how companies can best reduce their overall carbon emissions.
There are probably
other climate responses that different models treat differently, even though they all tend to generate temperature responses to doubled CO2 of about 1.2 C.
The remaining two — on sustainable habitat and strategic knowledge — are service missions and seek to create more knowledge on
useful climate responses.
Since the atmospheric lifetime of black carbon is only a few days, reducing black carbon emissions can bring about a
rapid climate response in a short amount of time.
We test how well our model can reproduce these observations, and thus gauge its ability to simulate long -
term climate responses to solar variations.
Hansen, J.; Russell, G.; Lacis, A.; Fung, I.; Rind, D. & Stone, P.
Climate Response Times: Dependence on Climate Sensitivity and Ocean Mixing Science, 1985, 229, 857 - 859.
The observationally constrained transient
climate response at the time of doubling of atmospheric CO2 following a 1 % per year increase in CO2 was estimated by Stott et al. (2006c) to lie between 1.5 °C and 2.8 °C (Section 9.6.2, Figure 9.21).
An additional set of modelling uncertainties is introduced into climate scenarios through differences in the global and
regional climate responses simulated by different AOGCMs for the same forcing.
The inter-model correlation of transient
climate response with ocean heat uptake efficacy is greater than its correlation with equilibrium climate sensitivity in an ensemble of climate models used for the 3rd and 4th IPCC assessments.
You're right that a climate sensitivity of 3 degrees is not derived from first principles, but from various
observed climate responses (volcanoes, LGM, etc) a value not too far removed from 3 is deemed most likely.
The pattern and spatial gradients of forcing affect global and regional temperature responses as well as other aspects of
climate response such as the hydrologic cycle.
GCMs often play a conservative role as a counterpoint to speculation or idealized modeling regarding «tipping points» or abrupt climate change, in favor of gradual, more
linear climate response to external forcing.
Phrases with «climate response»