The study shows that changes in
heat distribution between the ocean basins is important for understanding future climate change.
Not exact matches
For example, in Earth atmospheric circulation (such as Hadley cells) transport
heat between the warmer equatorial regions to the cool polar regions and this circulation pattern not only determines the temperature
distribution, but also sets which regions on Earth are dry or rainy and how clouds form over the planet.
Examination of the geographical
distribution of the differences in 0 to 700 m
heat content
between the 1977 — 1981 and 1965 — 1969 pentads and the 1986 — 1990 and 1977 — 1981 pentads shows that the pattern of
heat content change has spatial scales of entire ocean basins and is also found in similar analyses by Ishii et al. (2006).
ENSO events, for example, can warm or cool ocean surface temperatures through exchange of
heat between the surface and the reservoir stored beneath the oceanic mixed layer, and by changing the
distribution and extent of cloud cover (which influences the radiative balance in the lower atmosphere).
The uneven
distribution of the
heating / air conditioning
between the passenger and driver's side.
Viva / Karl safety features extend to electronic stability / traction control, anti-skid brakes, electronic brake - force
distribution, hill start assist and lane departure warning, while available features will include GM's IntelliLink touch - screen infotainment system, a
heated steering wheel and front seats, climate - control, a sunroof, fog lights, parking sensors and wheel sizes
between 14 - and 16 - inch.
In the innovative thermal management a computer monitors numerous actuators for the ideal
distribution of the
heat flows
between the engine, transmission and interior in any situation.
ENSO events, for example, can warm or cool ocean surface temperatures through exchange of
heat between the surface and the reservoir stored beneath the oceanic mixed layer, and by changing the
distribution and extent of cloud cover (which influences the radiative balance in the lower atmosphere).
I would suggest comparing peak to peak average temperature captures during weighted El - Nino events (during the time they occur, if they can be compared equally this would be a telling graph), instead of considering year to year records as a means of reducing ENSO effects on the temperature record, ENSO being largely a
heat exchange
between air and sea causing great changes in cloud
distribution world wide.
In contrast, CO2 forcing by layers changes sign
between the surface + troposphere and stratosphere (modulated by the effect of existing solar
heating of the stratosphere), and it may have a different
distribution of RF over the surface + troposphere layer (which would affect convection) and is more evenly distributed horizontally and temporally.
Surface temperature is an imperfect gauge of whether the earth has been warmed by an imbalance
between incoming radiation from the sun, and outgoing radiation, because of the role of ocean currents in the
distribution of
heat between deeper and surface waters.
The atmosphere is analogous to a flexible lens that is shaped by the density
distribution of the gas molecules, of the atmosphere in the space
between the sphere holding them, and space; Incoming
heat gets collected in many ways and places,, primarily by intermittent solar radiation gets stored, in vast quantities, and slowly but also a barrage of mass and energy fluxes from all directions; that are slowly transported great distances and to higher altitudes mostly by oceanic and atmospheric mass flows.
Surface warming is «seasonal warming» associated with the asymmetric
distribution of land (low
heat capacity) and ocean (high
heat capacity)
between the hemispheres.