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- 41ebe049-230e-4ff7-acb1-43de68ace83e definition "Albedo is the ratio of the radiation (radiant energy or luminous energy) reflected by a surface to that incident on it. Snow and cloud surfaces have a high albedo, because most of the energy of the visible solar spectrum is reflected. Vegetation and ocean surfaces have low albedo, because they absorb a large fraction of the energy. Clouds are the chief cause of variations in the Earth's albedo." @default.
- 41ebe049-230e-4ff7-acb1-43de68ace83e id "1661471" @default.
- 41ebe049-230e-4ff7-acb1-43de68ace83e path_id 1eb0ea0a-312c-4d74-8d42-6f1ad758f999 @default.
- 41ebe049-230e-4ff7-acb1-43de68ace83e path_id aa35a52f-e3d9-41bd-abd2-ec7e1a8101d1 @default.
- 41ebe049-230e-4ff7-acb1-43de68ace83e path_id e9f67a66-e9fc-435c-b720-ae32a2c3d8f5 @default.
- 41ebe049-230e-4ff7-acb1-43de68ace83e path_id fa0a36c3-2503-4662-98cd-7f3e74ce9f80 @default.
- 41ebe049-230e-4ff7-acb1-43de68ace83e path_label "CRYOSPHERE" @default.
- 41ebe049-230e-4ff7-acb1-43de68ace83e path_label "EARTH SCIENCE" @default.
- 41ebe049-230e-4ff7-acb1-43de68ace83e path_label "SNOW/ICE" @default.
- 41ebe049-230e-4ff7-acb1-43de68ace83e path_label "Science Keywords" @default.
- 41ebe049-230e-4ff7-acb1-43de68ace83e prefLabel "ALBEDO" @default.
- 41ebe049-230e-4ff7-acb1-43de68ace83e reference "Maunder, W.J. 1994. Dictionary of Global Climate Change, 2nd ed. Chapman and Hall, NY. WMO, 1966. International Meteorological Vocabulary, WMO/OMM/BMO - No. 182 TP. 91, Switzerland." @default.
- 41ebe049-230e-4ff7-acb1-43de68ace83e tag "Science Keywords" @default.