This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Clone of Aquaworld Revised - Surface Albedo, GHG and Temperature
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Credits for original model: Rik Blok
Clone of Aquaworld Radiation Balance-Project 1
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Clone of Aquaworld Radiation Balance
Modelling after Earth, this is a model of the greenhouse effect has in increasing the temperature. By trapping some of the radiation emitted by the planet the atmosphere can is itself a positive feedback loop.
Clone of Influence of Surface Temperature on Albedo and Greenhouse Effect
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
L'idée est de percevoir les "dynamiques" des "systèmes" à l'oeuvre dans le changement climatique à l'échelle planétaire. Pour cela comprendre les stocks, flux, boucles de rétroactions (lorsqu'un phénomène X influx sur un autre Y, qui influx à son tour sur X) permet de faire apparaître les liens de causes à conséquences parfois difficilement perceptibles.
L'idée étant de s'adosser sur le succès de la Fresque du Climat, qui a vulgarisé la compréhension du changement climatique pour désormais l'analyser grâce à la dynamique des systèmes (et comprendre ce qu'est un modèle, son utilité).
Sur la base du travail de Scott Formann-Roe
Mise en système du changement climatique
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
This simple radiation balance model shows the greenhouse effect that an atmosphere can have in warming a planet. By trapping some of the radiation emitted by the planet the atmosphere can cause the surface to become warmer than it otherwise would be.
Clone of Aquaworld Radiation Balance
