Gregory and Oerlemans (1998) applied
local seasonal temperature changes over 1860 to 1990 calculated by the HadCM2 AOGCM forced by changing greenhouse gases and aerosols (HadCM2 GS in Table 9.1) to the glacier model of Zuo and Oerlemans.
Not exact matches
At
local scales and over shorter periods, annual streamflow responds to
seasonal changes in climate variables (e.g.,
temperature, precipitation) and related processes such as evapotranspiration.
While the
local,
seasonal climate forcing by the Milankovitch cycles is large (of the order 30 W / m2), the net forcing provided by Milankovitch is close to zero in the global mean, requiring other radiative terms (like albedo or greenhouse gas anomalies) to force global - mean
temperature change.