Furthermore, agreement is widespread that these changes may profoundly
affect atmospheric water vapor concentrations, clouds, precipitation patterns, and runoff and stream flow patterns.
In turn, temperature change
affects atmospheric water vapor as well as the more dynamical components of equator - to - pole insolation and of temperature gradients that vary on timescales of decades to hundreds of years.
Not exact matches
Humans emit gigatons of
water vapor, by burning hydrocarbons, and it doesn't
affect atmospheric H2O, because it's condensable.
That increased
atmospheric water vapor will also
affect cloud cover, though impacts of changes in cloud cover on climate sensitivity are much more uncertain.
CO; 2 Observations of the Infrared Radiative Properties of the Ocean «[I] t is necessary to understand the physical variables contributing to sea surface emitted and reflected radiation to space.The emissivity of the ocean surface varies with view angle and sea state, the reflection of sky radiation also depends on view angle and sea state, and the absorption of
atmospheric constituents such as
water vapor, aerosols, and subdivisible clouds
affect transmittance.»
It is assumed, however, that the
atmospheric vertical thermal and
water vapor structures are implicitly
affected by the actual cloud cover, and that the atmosphere is at a stable steady state of cloud cover.