A methodology is presented for generating surrogate climate-change sce
narios with a regional climate model. The procedure is simple to imple
ment and dynamically consistent. It entails (i) adopting a realized or
simulated atmospheric flow evolution and (ii) prescribing specific th
ermodynamic modifications of this realization to a regional model's in
itial fields and externally-specified time-dependent lateral boundarie
s fields. The resulting scenarios can be used for process and paramete
rization studies, to calibrate the regional response to a putative glo
bal climate change, and to intercompare different models. The approach
is illustrated with two month-long regional climate model simulations
. The experiment is designed to explore the response within Europe to
a pseudo-global warming of 2 K with an accompanying increase in atmosp
heric water vapor content. Analysis reveals that there is a spatially-
differentiated preciptation increase consonant with the domain-average
d increase of about 16% in the water vapor content.