The phrase «stratospheric
cooling equilibrates with tropopause conditions before troposphere does» is also meaningless.
«Third, the «forcing» can not be possibly ever observed in laboratory conditions because the definition of forcing contains three physically unrealizable conditions: (a) CO2 mixes up, but temperature profile stays the same, (b) stratospheric
cooling equilibrates with tropopause conditions before troposphere does, and (c) troposphere - surface interface is kept frozen.
Not exact matches
How does
cooling in the stratosphere «
equilibrate» with conditions at the tropopause?
Solar forcing has increased over the 20th century and given that the oceans have not yet had time to
equilibrate to the new levels of forcing, it must have contributed some to the recent warming, in fact, that equlibration was further delayed by the
cooling period, so the unrealized climate commitment would have been greater than ordinarily expected given that most of the increase in solar activity occurred in the first half of the century.
Birkeland currents are interesting, although they seem to be a possible correction to direct solar irradiance only at the poles and only in the ionosphere, which is already enormously hot — between 1500C and 2500C — but so tenuous that you wouldn't feel heat if you stuck your arm out into the near vacuum of the ionosphere, you'd feel intense
cooling as your blood started to boil and ordinary thermometers would radiate heat away faster than they would
equilibrate (and hence would read very cold temperatures).
I took a block of ice put it in a 6 day rated
cooler in the shade, allowed 2 hours for temperatures to
equilibrate.