When Charon is positioned between the Sun and Pluto, Georgia Tech research indicates that the moon can significantly
reduce atmospheric loss (Credit: NASA / JHUAPL / SwRI)
Not exact matches
Much of the radiation from the
atmospheric gases, also in the infrared range, is transmitted back to the ocean,
reducing the net long wave radiation heat
loss of the ocean.
A steady state would eventually be reached wherein CO2
loss balanced CO2 uptake, because any tendency of plants to absorb more CO2 would
reduce atmospheric concentrations so as to
reduce plant growth.
Thus a change of water vapour, sky radiation and tempcrature is corrected by a change of cloudiness and
atmospheric circulation, the former increasing the reflection
loss and thus
reducing the effective sun heat.
Sea ice
loss in the NH will remain a problem until the AMO and NH
atmospheric temperatures in particular
reduce back to blue.
Ozone
loss in the stratosphere and the consequent increase in penetration of UV into the upper troposphere tends to
reduce the differential between the
atmospheric pressure in the stationary high pressure cell East of Chile and the low over Indonesia tending to move the atmosphere towards a constant El Nino orientation.
A higher
atmospheric temperature
reduces net IR
losses and energy accumulates until
losses are again balanced with evaporation, conduction, increased IR up or all three.
One of the mechanisms discussed at the Woods Hole Oceanographic Institute (that I linked to) was to do with ice
loss in the Arctic influencing
atmospheric and ocean coupling and
reducing thermohaline circulation.
The reduction from three to two orbit planes for
atmospheric moisture and temperature profiling represents a
loss in diurnal sampling (from 4 - to 6 - hour refresh) compared to the pre-Nunn-McCurdy NPOESS baseline, which will
reduce the quality of diurnally averaged climate analyses.