This includes changes in heat content of the lithosphere (Beltrami et al., 2002), the atmosphere (e.g., Trenberth et al., 2001) and the total heat of fusion due to melting of i) glaciers, ice caps and the Antarctic and Greenland Ice Sheets (see Chapter 4) and ii) arctic sea ice (Hilmer and Lemke, 2000).
Not exact matches
This
includes: Introduction to the particle model Calculating Density Required Practical (Measuring Density)
Change of state Specific
Heat Capacity Specific Latent
Heat Pressure
in Gases Summary / Review lesson (Trilogy
content) Boyle's Law Increasing gas pressure
I also usually try to
include the
change in the Relative Humidity, (if it can be found),
in my graphs as humidity plays a part
in the atmospheric
heat content.
Instead, they discuss new ways of playing around with the aerosol judge factor needed to explain why 20th - century warming is about half of the warming expected for increased
in GHGs; and then expand their list of fudge factors to
include smaller volcanos, stratospheric water vapor (published with no estimate of uncertainty for the predicted
change in Ts), transfer of
heat to the deeper ocean (where
changes in heat content are hard to accurately measure), etc..
However, the spatial pattern of the PDO
includes warming
in some places and cooling
in others;
in fact,
changes consistent with the PDO can be seen
in the geographic pattern of observed ocean
heat content changes.
A
change in ocean
heat content can also alter patterns of ocean circulation, which can have far - reaching effects on global climate conditions,
including changes to the outcome and pattern of meteorological events such as tropical storms, and also temperatures
in the northern Atlantic region, which are strongly influenced by currents that may be substantially reduced with CO2 increase
in the atmosphere.
Scientific confidence of the occurrence of climate
change include, for example, that over at least the last 50 years there have been increases
in the atmospheric concentration of CO2; increased nitrogen and soot (black carbon) deposition;
changes in the surface
heat and moisture fluxes over land; increases
in lower tropospheric and upper ocean temperatures and ocean
heat content; the elevation of sea level; and a large decrease
in summer Arctic sea ice coverage and a modest increase
in Antarctic sea ice coverage.
Apparently, these GCMs can «forecast» climate
change only «a posteriori», that is, for example, if we want to know what may happen with these GCMs from 2012 to 2020 we need first to wait the 2020 and then adjust the GCM model with ad - hoc physical explanations
including even an appeal to an unpredictable «red - noise» fluctuation of the ocean
heat content and flux system (occurring
in the model
in 2055 and 2075!)