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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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 of America
surface form: 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
National Weather Service
surface form: 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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Syukuro Manabe notableWork Manabe–Wetherald climate model