Matches in climatepub4-kg for { <https://climateKG.org/entity/5bac3ef6-5e30-4f14-a5dc-8065c7fcba55> ?p ?o ?g. }
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- 5bac3ef6-5e30-4f14-a5dc-8065c7fcba55 type Science_Keyword @default.
- 5bac3ef6-5e30-4f14-a5dc-8065c7fcba55 type Variable @default.
- 5bac3ef6-5e30-4f14-a5dc-8065c7fcba55 broader 162e2243-3266-4999-b352-d8a1a9dc82ac @default.
- 5bac3ef6-5e30-4f14-a5dc-8065c7fcba55 broader 1eb0ea0a-312c-4d74-8d42-6f1ad758f999 @default.
- 5bac3ef6-5e30-4f14-a5dc-8065c7fcba55 broader 62019831-aaba-4d63-a5cd-73138ccfa5d0 @default.
- 5bac3ef6-5e30-4f14-a5dc-8065c7fcba55 broader c47f6052-634e-40ef-a5ac-13f69f6f4c2a @default.
- 5bac3ef6-5e30-4f14-a5dc-8065c7fcba55 broader e9f67a66-e9fc-435c-b720-ae32a2c3d8f5 @default.
- 5bac3ef6-5e30-4f14-a5dc-8065c7fcba55 definition "In meteorology the result of radiative cooling of the earths surface and adjacent airRadiational cooling occurs as is typical on calm clear nights whenever the longwave emission from the surface is not balanced by significant amounts of absorbed shortwave radiation or downwelling longwave from the atmosphere above the surface and there are no nonradiative sources of sufficient energy to make up the difference" @default.
- 5bac3ef6-5e30-4f14-a5dc-8065c7fcba55 prefLabel "RADIATIONAL_COOLING" @default.