The rotation of the earth and the diurnal solar wave will create circulation, but not
strong vertical circulation over 10 to 15 km of the troposphere.
Not exact matches
Radiative gases play a critical role in continued
strong vertical convective
circulation below the tropopause.
Stronger vertical mixing invigorates the MOC [Meridonal Overturning
Circulation] by an order of magnitude, increases ocean heat transport by 50 — 100 %, reduces the zonal mean equator - to - pole temperature gradients by up to 6 °C, lowers tropical peak terrestrial temperatures by up to 6 °C, and warms high - latitude oceans by up to 10 °C.»
It should be noted that
strong vertical convective
circulation is not occurring in the stratosphere.
Konrad; Could you please give me a direct yes or no answer to the following question — Do you believe that
strong vertical tropospheric convective
circulation would continue without radiative gases?
An atmosphere without radiative gases will not exhibit
strong vertical tropospheric convective
circulation.
David, could I please have a yes or no answer to the following — Do you believe that
strong vertical tropospheric convective
circulation would continue without radiative gases?
However
strong vertical convective
circulation in the Hadley, Ferrel and Polar tropospheric cells is continuing for all regions of the globe you could point to at this time.
Because of a lack of radiative cooling at height and a lack of
strong vertical convective
circulation, a non radiative atmosphere would be dramatically hotter than our current atmosphere.
Could you please give me a direct yes or no answer to the following question — Do you believe that
strong vertical tropospheric convective
circulation would continue without radiative gases?
-- No that is only the result for near surface regions, assuming continued
strong vertical convective
circulation under the tropopause.
Joel could you please give me a direct yes or no answer to the following question — Do you believe that
strong vertical tropospheric convective
circulation would continue without radiative gases?
Here there is no
strong vertical convective
circulation, the lapse rate reverses and molecular energy rapidly rises.
Konrad; It is IR radiation to space and it's role in
strong vertical convective
circulation.