Manabe–Wetherald climate model

E181508

The Manabe–Wetherald climate model is a pioneering one-dimensional radiative–convective model that first quantified how increasing atmospheric carbon dioxide affects Earth’s temperature and vertical temperature profile.

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Manabe–Wetherald climate model canonical 1

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Statements (51)

Predicate Object
instanceOf climate model ⓘ
one-dimensional climate model ⓘ
radiative–convective model ⓘ
assumption fixed relative humidity in much of the troposphere ⓘ
one-dimensional vertical column atmosphere ⓘ
parameterized convection to maintain a lapse rate ⓘ
radiative–convective equilibrium in the troposphere ⓘ
atmosphericComponent stratosphere ⓘ
troposphere ⓘ
countryOfDevelopment United States ⓘ
developer Richard T. Wetherald NERFINISHED ⓘ
Syukuro Manabe ⓘ
dimension one-dimensional ⓘ
field atmospheric science ⓘ
climate physics ⓘ
climatology ⓘ
focus climate sensitivity to carbon dioxide ⓘ
surface temperature response to greenhouse gases ⓘ
vertical temperature profile of Earth’s atmosphere ⓘ
influenced development of simplified energy balance models ⓘ
later general circulation models of climate ⓘ
subsequent studies of climate sensitivity ⓘ
inputParameter atmospheric carbon dioxide concentration ⓘ
cloud properties ⓘ
solar constant ⓘ
water vapor distribution ⓘ
institution Geophysical Fluid Dynamics Laboratory ⓘ
Princeton University ⓘ
U.S. Weather Bureau ⓘ
notableFor establishing vertical structure of temperature response to CO2 increase ⓘ
first quantitative estimate of warming from increased CO2 using a radiative–convective model ⓘ
pioneering study of greenhouse effect on Earth’s climate ⓘ
output outgoing longwave radiation ⓘ
radiative fluxes ⓘ
surface air temperature ⓘ
vertical temperature profile ⓘ
primaryProcessRepresented convection ⓘ
radiative transfer ⓘ
radiative–convective equilibrium ⓘ
publicationVenue Journal of the Atmospheric Sciences ⓘ
publicationYear 1967 ⓘ
relatedTo climate sensitivity ⓘ
greenhouse effect ⓘ
radiative forcing ⓘ
vertical lapse rate ⓘ
water vapor feedback ⓘ
spatialRepresentation globally averaged atmosphere ⓘ
timeScale equilibrium climate response ⓘ
uses convective adjustment scheme ⓘ
infrared radiative transfer calculations ⓘ
shortwave radiative transfer calculations ⓘ

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Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Syukuro Manabe → notableWork → Manabe–Wetherald climate model ⓘ