Matches in climatepub4-kg for { <https://climateKG.org/entity/250ce118-46e7-4dec-9e44-8054c9318cff> ?p ?o ?g. }
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- 250ce118-46e7-4dec-9e44-8054c9318cff UsedIn 8491e067-951e-4cba-9619-d376b5c628a0 @default.
- 250ce118-46e7-4dec-9e44-8054c9318cff type Science_Keyword @default.
- 250ce118-46e7-4dec-9e44-8054c9318cff type Variable @default.
- 250ce118-46e7-4dec-9e44-8054c9318cff broader 1eb0ea0a-312c-4d74-8d42-6f1ad758f999 @default.
- 250ce118-46e7-4dec-9e44-8054c9318cff broader 23703b6b-ee15-4512-b5b2-f441547e2edf @default.
- 250ce118-46e7-4dec-9e44-8054c9318cff broader c9a5b3eb-7556-41a8-a2b8-c015db80e5b2 @default.
- 250ce118-46e7-4dec-9e44-8054c9318cff broader dc3f297b-8471-4101-b70e-dc5765762061 @default.
- 250ce118-46e7-4dec-9e44-8054c9318cff broader e9f67a66-e9fc-435c-b720-ae32a2c3d8f5 @default.
- 250ce118-46e7-4dec-9e44-8054c9318cff definition "Radiative forcing measured in Watts per square meter can be estimated in different ways for different components For the case of a change in solar irradiance ie solar forcing the radiative forcing is simply the change in the average amount of solar energy absorbed per square meter of the Earths area Since the crosssectional area of the Earth exposed to the sun πr2 is equal to 14 of the surface area of the Earth 4πr2 the solar input per unit area is one quarter the change in solar intensity This must be multiplied by the fraction of incident sunlight that is absorbed F1R where R is the reflectivity or albedo of the Earth equal to approximately 07 Thus the solar forcing is the change in the solar intensity divided by 4 and multiplied by 07" @default.
- 250ce118-46e7-4dec-9e44-8054c9318cff prefLabel "SOLAR_FORCING" @default.