Questo modello di bilancio delle radiazioni emesse e assorbite mostra l'effetto serra che l'atmosfera può avere nel riscaldamento di un pianeta simile alla terra. Trattenendo parte della radiazione emessa dal pianeta, l'atmosfera può far sì che la superficie diventi più calda di quanto non sarebbe altrimenti.
Passate attraverso la storia in fondo a questa finestra.
Clone of Effetto Serra
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
The World3 model is a detailed simulation of human population growth from 1900 into the future. It includes many environmental and demographic factors.
Use the sliders to experiment with the initial amount of non-renewable resources to see how these affect the simulation. Does increasing the amount of non-renewable resources (which could occur through the development of better exploration technologies) improve our future? Also, experiment with the start date of a more environmentally focused policy.
WORLD: The World3 Model: Classic World Simulation
The World3 model is a detailed simulation of human population growth from 1900 into the future. It includes many environmental and demographic factors.
Use the sliders to experiment with the initial amount of non-renewable resources to see how these affect the simulation. Does increasing the amount of non-renewable resources (which could occur through the development of better exploration technologies) improve our future? Also, experiment with the start date of a low birth-rate, environmentally focused policy.
Clone of The World3 Model: A Detailed World Forecaster
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.
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Clone of Effetto Serra
The World3 model is a detailed simulation of human population growth from 1900 into the future. It includes many environmental and demographic factors.
Use the sliders to experiment with the initial amount of non-renewable resources to see how these affect the simulation. Does increasing the amount of non-renewable resources (which could occur through the development of better exploration technologies) improve our future? Also, experiment with the start date of a low birth-rate, environmentally focused policy.
Clone of My World3
The World3 model is a detailed simulation of human population growth from 1900 into the future. It includes many environmental and demographic factors.
THIS MODEL BY GUY LAKEMAN, FROM METRICS OBTAINED USING A MORE COMPREHENSIVE VENSIM SOFTWARE MODEL, SHOWS CURRENT CONDITIONS CREATED BY THE LATEST WEATHER EXTREMES AND LOSS OF ARABLE LAND BY THE ALBEDO EFECT MELTING THE POLAR CAPS TOGETHER WITH NORTHERN JETSTREAM SHIFT NORTHWARDS, AND A NECESSITY TO ACT BEFORE THERE IS HUGE SUFFERING.
BY SETTING THE NEW ECOLOGICAL POLICIES TO 2015 WE CAN SEE THAT SOME POPULATIONS CAN BE SAVED BUT CITIES WILL SUFFER MOST.
CURRENT MARKET SATURATION PLATEAU OF SOLID PRODUCTS AND BEHAVIORAL SINK FACTORS ARE ALSO ADDED
Use the sliders to experiment with the initial amount of non-renewable resources to see how these affect the simulation. Does increasing the amount of non-renewable resources (which could occur through the development of better exploration technologies) improve our future? Also, experiment with the start date of a low birth-rate, environmentally focused policy.
Clone of 2014 Weather & Climate Extreme Loss of Arable Land and Ocean Fertility - The World3+ Model: Forecaster
The World3 model is a detailed simulation of human population growth from 1900 into the future. It includes many environmental and demographic factors.
Use the sliders to experiment with the initial amount of non-renewable resources to see how these affect the simulation. Does increasing the amount of non-renewable resources (which could occur through the development of better exploration technologies) improve our future? Also, experiment with the start date of a low birth-rate, environmentally focused policy.
Updated World3 Model: A Detailed World Forecaster
The World3 model is a detailed simulation of human population growth from 1900 into the future. It includes many environmental and demographic factors.
Use the sliders to experiment with the initial amount of non-renewable resources to see how these affect the simulation. Does increasing the amount of non-renewable resources (which could occur through the development of better exploration technologies) improve our future? Also, experiment with the start date of a low birth-rate, environmentally focused policy.
Clone of The World3 Model: A Detailed World Forecaster
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 Revised - Surface Albedo, GHG and Temperature
The World3 model is a detailed simulation of human population growth from 1900 into the future. It includes many environmental and demographic factors.
Use the sliders to experiment with the initial amount of non-renewable resources to see how these affect the simulation. Does increasing the amount of non-renewable resources (which could occur through the development of better exploration technologies) improve our future? Also, experiment with the start date of a low birth-rate, environmentally focused policy.
Clone of The World3 Model: A Detailed World Forecaster
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 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 Revised - Surface Albedo, GHG and Temperature
