All CO2 molecules in the atmosphere are warmed to
local air temperature by collision induced conduction to above this temperature.
Not exact matches
These
air temperature reductions have also been projected to improve
local air quality
by reducing smog formation and ozone concentration.
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The difference between ocean and
air temperature also tends to create heavy morning fog during the summer months, known as the marine layer, driven
by an onshore wind created
by the
local high pressure sunny portions of the Salinas Valley, which extend north and south from Salinas and the Bay.
The aspect of the paper that has attracted the most attention is the claim that the retreat of the Kilimanjaro summit glaciers can be explained
by precipitation reduction, without any compelling need to invoke a warming trend in
local air temperature.
An parcel means that the medium is small enough to be isothermal and in
local thermodynamic equilibrium (which then ensures that the population of thermodynamic molecular energy levels will be set
by molecular collisions at the
local atmospheric
temperature), but the parcel is also large enough to contain a large enough sample of molecules to represent a statistically significant mass of
air for thermodynamics to apply.
These stem from a diversity of site - specific conditions, including, but not limited to:
local vegetation; presence of building structures and contributions made
by such structures involving energy use, heating and
air conditioning, etc; exposure to winds, the wind velocities determined
by climatic factors and also whether certain wind directions are more favored than others
by terrain or the presence or absence thereof to bodies of water; proximity to grass, asphalt, concrete or other material surfaces; the physical conditions of the CRS itself which include: the exact location of the
temperature sensors within it, the degree of unimpeded flow of external
air through the CRS, the character of the paint used; the exact height of the instrument above the external surface (noting that when the ground is covered
by 3 feet of snow, the
temperature instrument is about 60 % closer to, or less than 2 feet, above an excellent radiating surface, much closer than it would be under snow - free conditions).
They are backed
by inexorable logic: for every 1 °C rise in
temperature, the potential saturation levels of the
air rise
by 7 %, so where there is water to be evaporated,
local humidity rises with the thermometer.
Local independent weather monitoring stations logged an average of 6 degrees drop in
air temperature lagging peak eclipse point
by approximately 30 minutes.
Air temperature is a nonconservative, intensive variable whose
local value depends not only upon the radiative fluxes driven
by thermalization of insolation, but upon upon the atmoshperic pressure, in accordance with Boyle's law.