Not exact matches
The temperature did not change, so the surface temperature -
dependent responses of
atmospheric radiative cooling also did not change.
QRA can be regarded as an extension of the Haurwitz - type mechanism (42) of a strong increase in the amplitude of the midlatitude
atmospheric barotropic wave system
response to stationary external barotropic thermal forcing, with a spatial frequency m approaching the natural stationary spatial frequency k of the wave system, to the case of external barotropic thermal and orographic forcing under a latitude -
dependent u ¯ and an integer m over the midlatitude belt on the spherical Earth.
Radiatively, the only thing that distinguishes a «forcing» from a «feedback» is that injection of the forcing constituent into the climate system does not depend on the
atmospheric temperature, while the feedback constituents are temperature
dependent in
response to local meteorological conditions.