In response to the finding that anthropogenic aerosols create a significant perturbation in the earth's radiative
balance on regional scales, ESRL / GMD expanded its aerosol research program (1992) to include aerosol monitoring stations in regions where significant aerosol forcing was expected.
Not exact matches
That it is possible to construct a metric that doesn't show
regional warming in a certain roughly specified region
on a certain unspecified time
scale with a certain unspecified statistical technique in no way contradicts the assertion that the
balance of observational evidence shows unusual recent global warming, in first order agreement with theoretical, computational, and paleoclimate evidence.
We quantify sea - level commitment in the baseline case by building
on Levermann et al. (10), who used physical simulations to model the SLR within a 2,000 - y envelope as the sum of the contributions of (i) ocean thermal expansion, based
on six coupled climate models; (ii) mountain glacier and ice cap melting, based
on surface mass
balance and simplified ice dynamic models; (iii) Greenland ice sheet decay, based
on a coupled
regional climate model and ice sheet dynamic model; and (iv) Antarctic ice sheet decay, based
on a continental -
scale model parameterizing grounding line ice flux in relation to temperature.
Drivers of the land climate system have larger effects at
regional and local
scales than
on global climate, which is controlled primarily by processes of global radiation
balance.
The impact of land use change
on the energy and water
balance may be very significant for climate at
regional scales over time periods of decades or longer.