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Climate Models

These models and simulations have been tagged “Climate”.

Related tagsGreenhouse EffectClimate ChangeSciencePoliticsWeatherEnvironment

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A model of Global Climate Change driven by the impact of Carbon Dioxide on the Greenhouse Effect. This model contains a physical model of energy inflows ☀️ and outflows from the Earth (primary source). And a simple model of carbon dioxide sources and sinks in the atmosphere (primary source).

The energy model assumes inflowing short-wave solar radiation that does not interact with the atmosphere. A fraction of this is reflected immediately (e.g. by snow and ice cover). The remaining is absorbed 🌎 and re-radiated as long-wave infrared which can be captured by the atmosphere ☁️. The fraction captured by the atmosphere is related to the level of Carbon Dioxide in the atmosphere.

This model tracks Carbon Dioxide emissions from burning fossil fuels 🏭 and land use changes 🚜 (e.g. deforestation). It also tracks removal of Carbon Dioxide from the atmosphere into a land sink 🌲 (e.g. vegetation) and the an ocean sink 🏖.

🧪 Experiment with different levels of emissions to see their impact on global average temperatures. You can also compare predicted temperatures and Carbon Dioxide levels to historical data.
Clone of Global Climate Change
Profile photo Kyra Evers
8 months ago
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Causal loop diagram illustrating how the ice-albedo feedback system contributes to arctic ice loss.
Clone of Climate Change Influencer: Arctic Ice Loss (1-Loop; Reinforcing)
Profile photo Albert El-hage
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Model of Earth's Climate System.
Clone of Clone of Clone of Climate System
Profile photo Carina Chan
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Model of Earth's Climate System.
Clone of Clone of Climate System
Profile photo Ethan Patton
3
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Climate change and eels
Profile photo Kristen Steele
Insight diagram
Causal loop diagram illustrating how the ice-albedo feedback system contributes to arctic ice loss.
Clone of Climate Change Influencer: Arctic Ice Loss (1-Loop; Reinforcing)
Profile photo Juan Manuel Valencia
Insight diagram
Causal loop diagram illustrating how the ice-albedo feedback system contributes to arctic ice loss.
Clone of Climate Change Influencer: Arctic Ice Loss (1-Loop; Reinforcing)
Profile photo natasha medawar
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Daisyworld
Profile photo Derek Howell
3 2 months ago
Insight diagram
Causal loop diagram illustrating how the ice-albedo feedback system contributes to arctic ice loss.
Clone of Climate Change Influencer: Arctic Ice Loss (1-Loop; Reinforcing)
Profile photo Albert El-hage
Insight diagram
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
Profile photo David
Insight diagram
Assignment 1- Part 2 Energy Economics and Fossil Fuels
Clone of Clone of Berberian_Energy Economics and Fossil Fuel
Profile photo Lori Berberian
Insight diagram
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
Profile photo Bill shmygol
Insight diagram

THE 2020 MODEL (BY GUY LAKEMAN) EMPHASIZES THE PEAK IN POLLUTION BEING CREATED BY OVERPOPULATION.
WITH THE CARRYING CAPACITY OF ARABLE LAND NOW BEING 1.5 TIMES OVER A SUSTAINABLE FUTURE (PASSED IN 1990) AND NOW INCREASING IN LOSS OF HUMAN SUSTAINABILITY DUE TO SEA RISE AND EXTREME GLOBAL WATER RELOCATION IN WEATHER CHANGES IN FLOODS AND DROUGHTS AND EXTENDED TROPICAL AND HORSE LATTITUDE CYCLONE ACTIVITY AROUND HADLEY CELLS

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.

WORLD2020 to PLANET2020
Profile photo Guy Lakeman
15
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Maybe this will help me figure out my MATLAB code
Clone of Venus Climate Model
Profile photo Phil Resor
Insight diagram
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 Clone of Clone of Aquaworld Radiation Balance
Profile photo Praneesh Datt
Insight diagram
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.
Aquaworld Radiation Balance Model W/ Surface Albedo and the Greenhouse Effect Dependent on Surface Temperature!
Profile photo Sean Bains
Insight diagram
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
Profile photo James Linzel
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This is step 5 in making a climate model based on our insights of how trees actively contribute to the cooling capcacity of the Earth.​

In the prevoious step we added the reflection of sun energy by Clouds 

In this step we added aabsorption of near infrared by clouds and the biotic pump

Present the temperature of the Earth is 288 Kelvin. Without Earth would be 255 Kelvin. So the energy balance of the Earth add 33 Kelvin.
We optimize in step 4 the variable GHG-effect and the optimal number is 0,29625 in this model.


With Our-Green-Spine we have discovered new insights how trees / forest / green structures are part of the managing system of controlling the temperature of our Earth via their cooling capacity by using water and influencing the water cycle. We want to translate our insights in a climate model. People who to join us please send an email to marcel.planb@gmail.com.
Thanks, Marcel de Berg
Backup of workversion Clone of Model 6 integrating Biotic Pump
Profile photo Marcel de Berg
Insight diagram

THE 2017 MODEL (BY GUY LAKEMAN) EMPHASIZES THE PEAK IN POLLUTION BEING CREATED BY OVERPOPULATION WITH THE CARRYING CAPACITY OF ARABLE LAND NOW BEING 1.5 TIMES OVER A SUSTAINABLE FUTURE (PASSED IN 1990) AND NOW INCREASING IN LOSS OF HUMAN SUSTAINABILITY DUE TO SEA RISE AND EXTREME GLOBAL WATER RELOCATION IN WEATHER CHANGES IN FLOODS AND DROUGHTS AND EXTENDED TROPICAL AND HORSE LATTITUDE CYCLONE ACTIVITY AROUND HADLEY CELLS

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 2017 Weather & Climate Extreme Loss of Arable Land and Ocean Fertility by Guy Lakeman - The World3+ Model: Forecaster
Profile photo Rhys Almario
Insight diagram
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
Profile photo Karyssa Arnett
Insight diagram
Causal loop diagram illustrating how the ice-albedo feedback system contributes to arctic ice loss.
Clone of Climate Change Influencer: Arctic Ice Loss (1-Loop; Reinforcing)
Profile photo scarlettchoueiri
Insight diagram
cycle of climate change and how human actions designed to mitigate the effects make the change worse
Climate Change Cycle
Profile photo Edythe
Insight diagram

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
Profile photo Samson Tan
Insight diagram
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.

Step through the story at the bottom of this window.
Aquaworld Radiation Balance
Profile photo Rik Blok
142 10 months ago
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