Not exact matches
Modifying the vegetation cover alters the surface properties — such as the amount of heat dissipated by
water evaporation and the level of radiation
reflected back into space — which has a knock - on effect on local surface temperature.
Their analysis reveals that the conversion of broadleaved forests to coniferous forests caused significant changes in evapotranspiration, the
evaporation of
water through leaves, and albedo, the amount of solar energy
reflected from the Earth back into space.
Losses leave primarily through
reflected energy, which is sent back into space, and
evaporation of
water.
Consistent with how I was reading things, pleasantly — barring some cautious hedging I'd made, based on the possibility that salinity could
reflect mass changes, either when fresh
water was added to the ocean via glacial melt or impoundment decreases (ocean mass increase) or via increased
evaporation rates (ocean mass decrease).
As you know, salinity affects
evaporation and / or may
reflect an influx (or lack) of fresh
water (by precipitation, riverine, or runoff).
These effects are relatively well understood in the lowest level of the atmosphere, the troposphere, where increased warming leads to greater
evaporation, causing more
water vapour and so further warming, although this is offset to some extent through the formation of clouds that
reflect incoming sunlight back into space.
As the planet warms, increasing levels of
water vapour in the atmosphere caused by higher
evaporation levels form more clouds and snow increasing the albedo of the planet,
reflecting heat back into space more efficiently, thus working to regulate the temperature downward.