A very simple thermodynamic model of a planet, which includes first order approximations of its radiation balance (black bodies), including two radiation modulating effects i.e. albedo and green house and two heat storages (ocean and atmosphere). It is a lumped model which does not consider spatial variations and resulting mass transports - thus no heat exchange between e.g. equatorial and polar regions...
As a consequence all values are surface specific i.e. per square meter. E.g. the energy balance is the balance in W/m² and the heat reservoirs are water and air columns with a cross section of 1 m²...
Clone of AcquaWorld
la deforestación y el efecto invernadero
The fact
that we all strive to reduce psychologically inconsistent thoughts is a well-researched phenomenon. When we hold
two conflicting thoughts in our heads we feel an overwhelming desire to reduce
this conflict. This desire can be a powerful driver in the way we behave. Most
of us are aware at some level that if we took the threat of climate change
seriously we would need to completely change our routines and the way we behave.
Flying off on holiday would be out of the question. Swimming pools would be a
past luxury. Most of us would need to give up our cars and become vegetarians.
The list can be extended almost endlessly. Very often, subconsciously, we try
to reduce troubling and inconvenient facts by minimizing, ignoring or even by denying
them. Could this be why we hardly talk about climate change even in the face of
increasingly frequent extreme weather events and obvious signs that it is
occurring now?
This subject
needs to be openly talked about between us and in the press. The seriousness of global warming makes it a necessity.
Only when this happens will politicians have the space and incentive to
act on our behalf. But before this can happen we need to be aware of the reason
why we avoid talking about this subject – this graph tries to illustrate the
harmful dynamic that could be responsible for it.
Clone of The dynamic that prevents confronting climate change
Capitalism is in crisis and climate
change disruption is now beginning to hit the bottom line. Insurance companies
know this well. According to a report by the Bank of England, insured losses
have risen from $10 000 million in 1985 to $50 000 million in 2015. Climate change
cannot be reversed, and extreme weather events
will undoubtedly get worse in the future strengthening the disruptive effects
shown in the CLD. Another dynamic is that
companies will continue to automate and, as The Economic Policy Institute has shown,
fail to reflect productivity gains in workers' salaries. The result, stagnating
salaries is disastrous for demand, given that capitalism needs endlessly rising demand
and consumption. A further serious problem is that as climate change gets worse
there will be increasing demands for companies to assume their responsibility and
bear the costs of negative externalities. The CLD shows these factors which are likely
to lead to the collapse of the system: when capitalism can no longer generate 'capital'
it has stopped to serves any useful purpose.
DOES THIS DYNAMIC SPELL THE END OF CAPITALISM
Temperature Stress Mortality Simulator: for the older (70+ years) population of West Dorset, UK using the UKCP09 SRES A1B Emission Scenario.
Clone of Temperature Stress Mortality Simulator
There is now substantial evidence that three unstoppable
reinforcing feedback systems that can only accelerate global warming have been
triggered in the Arctic. R2 illustrates a process whereby frozen methane
hydrate, which exists in enormous quantities
on the seabed of the shallow Arctic Ocean shelf, is breaking up as the ocean
warms. This leads to methane gas, a greenhouse gas about 20 times more powerful
than C02, bubbling up to the surface. R1 shows that as the ice cover of the ocean
melts and shrinks, less sunlight is reflected back into space and more is absorbed by the ocean, warming it as a consequence. The
warmer ocean water and warmer air temperature will then melt more ice, but it
will also break up more methane hydrates. R3
describes a similar process where melting permafrost releases methane into the
atmosphere, making the situation even worse. These processes are multiplicative,
they reinforce each other. Below are
links to three articles that provide evidence that this is going on now. Systems
thinking tells us about reinforcing feedback loops and the associated exponential
growth. Taking this and the evidence provided by the articles into account the
conclusion clearly points to increasing and accelerated global warming. The recent
Paris agreement on global warming may have come too late!
http://www.independent.co.uk/news/science/vast-methane-plumes-seen-in-arctic-ocean-as-sea-ice-retreats-6276278.html
http://www.theguardian.com/environment/2005/aug/11/science.climatechange1
https://www.newscientist.com/article/dn23205-major-methane-release-is-almost-inevitable/
Clone of Clone of Accelerated Global Warming
Temperature Stress Mortality Simulator: for the older (70+ years) population of West Dorset, UK using the UKCP09 SRES A1B Emission Scenario.
Eva's Temperature Stress Mortality Simulator
DRAFT conceptual model of climate change connections in Yamuna river project.
Clone of Yamuna River Restoration and Climate Change
Temperature Stress Mortality Simulator: for the older (70+ years) population of West Dorset, UK using the UKCP09 SRES A1B Emission Scenario.
Clone of Temperature Stress Mortality Simulator
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
Narrative influence model sketching influence links in energy-economy-emissions
Basic energy-economy-emissions influence
simulation oc carbon dioxide in the atmosphere
carbon dioxide-1
Changes to V17: capacity retirement updated, fraction of Al in energy intensities endognously calculated; fC repair is now also limited by Al supply gap
3 machines 2026 for materials v19 sensitivity
Clone of Clone of la deforestación y el efecto invernadero
The concept of 'CLOSING A FEEDBACK LOOP'
means that a loop is closed to affect the person or agents that originally
are responsible for an action so that they plainly feel its effects. This almost inevitable leads to corrective
action. One of the reasons why climate change does not arouse passion and action is that it is largely
invisible and most people are not aware of it, although extreme weather events
are beginning to change this somewhat. The schematic representation shows how
systems thinking might help to draw attention to such situations by graphically connecting the dots to promote understand and hopefully action when people realize
that there is a price to be paid for inaction. Please note, however, that the loop does not describe
dynamic behaviour in the normal system dynamics sense.
WHEN THIS LOOP CLOSES SOME WILL SUFFER BADLY
Temperature Stress Mortality Simulator: for the older (70+ years) population of West Dorset, UK using the UKCP09 SRES A1B Emission Scenario.
Clone of Temperature Stress Mortality Simulator
Clone of la deforestación y el efecto invernadero
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.
Comprendre la dynamique du changement climatique
Temperature Stress Mortality Simulator: for the older (70+ years) population of Dorset, Bournemouth and Poole, UK, using the UKCP09 SRES A1B Emission Scenario.
Clone of Temperature Stress Mortality Simulator V2.1
A model of a typical Australian sheep farm, where wool is the primary product, with first-cross fat lambs a secondary product.
This model attempts to model the behaviour in response to stocking rates and finances
MOULINS_VA Farm - System Dynamics Major Project
Temperature Stress Mortality Simulator: for the older (70+ years) population of West Dorset, UK using the UKCP09 SRES A1B Emission Scenario.
Clone of Temperature Stress Mortality Simulator
A model of a typical Australian sheep farm, where wool is the primary product, with first-cross fat lambs a secondary product.
This model attempts to model the behaviour in response to stocking rates and finances
Clone of MOULINS_VA Farm - System Dynamics Major Project
Temperature Stress Mortality Simulator: for the older (70+ years) population of West Dorset, UK using the UKCP09 SRES A1B Emission Scenario.
Clone of Temperature Stress Mortality Simulator