SwePub
Sök i LIBRIS databas

  Extended search

onr:"swepub:oai:DiVA.org:su-50109"
 

Search: onr:"swepub:oai:DiVA.org:su-50109" > Why Hasn't Earth Wa...

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

Why Hasn't Earth Warmed as Much as Expected?

Schwartz, Stephen E. (author)
Charlson, Robert J. (author)
Kahn, Ralph A. (author)
show more...
Ogren, John A. (author)
Rodhe, Henning (author)
Stockholms universitet,Meteorologiska institutionen (MISU)
show less...
 (creator_code:org_t)
2010
2010
English.
In: Journal of Climate. - 0894-8755 .- 1520-0442. ; 23:10, s. 2453-2464
  • Journal article (peer-reviewed)
Abstract Subject headings
Close  
  • The observed increase in global mean surface temperature (GMST) over the industrial era is less than 40% of that expected from observed increases in long-lived greenhouse gases together with the best-estimate equilibrium climate sensitivity given by the 2007 Assessment Report of the Intergovernmental Panel on Climate Change (IPCC). Possible reasons for this warming discrepancy are systematically examined here. The warming discrepancy is found to be due mainly to some combination of two factors: the IPCC best estimate of climate sensitivity being too high and/or the greenhouse gas forcing being partially offset by forcing by increased concentrations of atmospheric aerosols; the increase in global heat content due to thermal disequilibrium accounts for less than 25% of the discrepancy, and cooling by natural temperature variation can account for only about 15%. Current uncertainty in climate sensitivity is shown to preclude determining the amount of future fossil fuel CO2 emissions that would be compatible with any chosen maximum allowable increase in GMST; even the sign of such allowable future emissions is unconstrained. Resolving this situation, by empirical determination of the earth's climate sensitivity from the historical record over the industrial period or through use of climate models whose accuracy is evaluated by their performance over this period, is shown to require substantial reduction in the uncertainty of aerosol forcing over this period.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Meteorologi och atmosfärforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Meteorology and Atmospheric Sciences (hsv//eng)

Keyword

OCEAN HEAT-CONTENT; SEA-LEVEL RISE; CLIMATE SENSITIVITY; ANTHROPOGENIC AEROSOLS; OPTICAL-PROPERTIES; ENERGY; SIMULATIONS; IMBALANCE; EMISSIONS; MODELS
Meteorology
Meteorologi
meteorologi
Meteorology

Publication and Content Type

ref (subject category)
art (subject category)

Find in a library

To the university's database

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

Search outside SwePub

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Close

Copy and save the link in order to return to this view