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You are part of a team that discovered a nFigure 4.6 Schematic of energy flow on a planet with a two - layer atmosphere, W with values in which are based 2' m on our Earth's values of solar constant and albedo.ew planet in our solar system and decided to call it Planet Assoca. This new planet has no atmosphere, a solar constant (S) of 1500 W/m2, an albedo (\alpha) of 0.5, and a radius of 4, 500 km. Future research indicates that Planet Assoca has a two -layer atmosphere. Draw a diagram (like Figure 4.6 in your textbook) that shows the energy flows for Planet Assoca. Use the values for Planet Assoca listed above (i.e. solar constant, albedo, etc.) . Make sure each arrow is labelled with the energy flow. Figure 4.6 Schematic of energy flow on a planet with a two-layer atmosphere, with values in W/m², which are based on our Earth's values of solar constant and albedo. Sun 238 upper atmosphere ↑ lower atmosphere 714 476 476 238 238

You are part of a team that discovered a nFigure 4.6 Schematic of energy flow on a planet with a two - layer atmosphere, W with values in which are based 2' m on our Earth's values of solar constant and albedo.ew planet in our solar system and decided to call it Planet Assoca. This new planet has no atmosphere, a solar constant (S) of 1500 W/m2, an albedo (\alpha) of 0.5, and a radius of 4, 500 km. Future research indicates that Planet Assoca has a two -layer atmosphere. Draw a diagram (like Figure 4.6 in your textbook) that shows the energy flows for Planet Assoca. Use the values for Planet Assoca listed above (i.e. solar constant, albedo, etc.) . Make sure each arrow is labelled with the energy flow. Figure 4.6 Schematic of energy flow on a planet with a two-layer atmosphere, with values in W/m², which are based on our Earth's values of solar constant and albedo. Sun 238 upper atmosphere ↑ lower atmosphere 714 476 476 238 238

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
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You are part of a team that discovered a nFigure 4.6 Schematic of energy flow on a planet with a two-layer atmosphere, W with values in which are based m² on our Earth's values of solar constant and albedo.ew planet in our solar system and decided to call it Planet Assoca. This new planet has no atmosphere, a solar constant (S) of 1500 W/m2, an albedo (\alpha) of 0.5, and a radius of 4, 500 km. Future research indicates that Planet Assoca has a two-layer atmosphere. Draw a diagram (like Figure 4.6 in your textbook) that shows the energy flows for Planet Assoca. Use the values for Planet Assoca listed above (i.e. solar constant, albedo, etc.). Make sure each arrow is labelled with the energy flow. Figure 4.6 Schematic of energy flow on a planet with a two-layer atmosphere, with values in W/m², which are based on our Earth's values of solar constant and albedo. Sun 238 upper atmosphere 476 lower atmosphere 714 476 238 238
Transcribed Image Text:You are part of a team that discovered a nFigure 4.6 Schematic of energy flow on a planet with a two-layer atmosphere, W with values in which are based m² on our Earth's values of solar constant and albedo.ew planet in our solar system and decided to call it Planet Assoca. This new planet has no atmosphere, a solar constant (S) of 1500 W/m2, an albedo (\alpha) of 0.5, and a radius of 4, 500 km. Future research indicates that Planet Assoca has a two-layer atmosphere. Draw a diagram (like Figure 4.6 in your textbook) that shows the energy flows for Planet Assoca. Use the values for Planet Assoca listed above (i.e. solar constant, albedo, etc.). Make sure each arrow is labelled with the energy flow. Figure 4.6 Schematic of energy flow on a planet with a two-layer atmosphere, with values in W/m², which are based on our Earth's values of solar constant and albedo. Sun 238 upper atmosphere 476 lower atmosphere 714 476 238 238
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