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Observed changes in surface atmospheric energy over land
Author(s) -
Peterson Thomas C.,
Willett Katharine M.,
Thorne Peter W.
Publication year - 2011
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2011gl048442
Subject(s) - latent heat , enthalpy , atmosphere (unit) , sigma heat , thermodynamics , kinetic energy , atmospheric sciences , sensible heat , energetics , environmental science , surface energy , climatology , heat flux , physics , heat transfer , geology , classical mechanics , critical heat flux
The temperature of the surface atmosphere over land has been rising during recent decades. But surface temperature, or, more accurately, enthalpy which can be calculated from temperature, is only one component of the energy content of the surface atmosphere. The other parts include kinetic energy and latent heat. It has been advocated in certain quarters that ignoring additional terms somehow calls into question global surface temperature analyses. Examination of all three of these components of atmospheric energetics reveals a significant increase in global surface atmospheric energy since the 1970s. Kinetic energy has decreased but by over two orders of magnitude less than the increases in both enthalpy and latent heat which provide approximately equal contributions to the global increases in heat content. Regionally, the enthalpy or the latent heat component can dominate the change in heat content. Although generally changes in latent heat and enthalpy act in concert, in some regions they can have the opposite signs.