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Earth System Sensitivity

Annual global temperatures from 1850-2017. The colour scale represents the change in global temperatures covering 1.35°C. Credit: Climate Lab Book, 2018



The Earth System

Earth is a complex dynamic system. Earth system dynamics can be understood in terms of trajectories between alternate states separated by thresholds that are controlled by nonlinear processes, interactions, and feedbacks. For example, over the past 1.2 million years Earth has remained in a state of glacial and interglacial cycles. The current temperature change at 1,2°C above a preindustrial baseline has already pushed Earth out of the next glaciation cycle.

Furthermore, Earth is a water planet and incredibly inert. The time lag between cause and effect, between the heating and the final change in temperature, is large. The full warming effect of a large emission pulse may not be felt for several decades or centuries. As a result, the currently observed change in temperature represents only a part of the eventual expected increase in temperature resulting from already released greenhouse gas emissions.

Exactly where a potential planetary threshold, between a livable state and a hothouse state, might be is uncertain. Steffen et al. (2018) suggests 2°C as the critical limit, stating that passing two degrees could trigger tipping elements in the Earth System that could cascade, triggering further tipping elements, causing rapid warming beyond human control. 

Thus, actions taken over the next decade could significantly influence the trajectory of the Earth System for tens to hundreds of thousands of years and potentially lead to conditions that would be inhospitable to humans and to many other species.

Main point: Earth is tracking a hothouse pathway



Earth System Sensitivity


How the climate system will respond to increasing CO2 levels depends on time-scale and which feedbacks we consider. Taking into account fast feedbacks such as clouds, water vapour, snow cover change, and aerosols we get a climate sensitivity of about 2-4.5°C to a doubling of CO2. But this does not include slow longer-term feedbacks such as ice sheet disintegration, changes in carbon cycle (e.g. permafrost thaw), vegetation cover changes, or changes in oceans ability to store carbon. If we include all feedbacks, both fast and slow, we get a Earth System Sensitivity of 3-6°C.  

Estimated temperature changes from fast and slow feedbacks. Source: Schmidt, 2016



Studies of past climates in Earth's history show that long-term feedbacks play an important role in Earth's overall climate. For example, during the mid-Pliocene some 3-4 million years ago, when global mean temperatures were about 3-4°C warmer than preindustrial and sea levels 10-25 meter higher than today, CO2 levels peaked at 450 ppm. Our current concentration levels stand at 410 ppm CO2, but temperatures have only risen about + 1,2°C, so Earth is likely to warm up at least to similar levels eventually. And we would over millenia have sea-level rise of up to at least 10 m.

The reason why most people don't talk about ESS is due to the fact that its presumed to take centuries or millennia for these slow feedbacks to kick in. But the issue now is that the rate of change is many times faster than any natural rate in Earth's history. Only comparable with catastrophic rare events such as the meteorite strike that took out the dinosaurs some 66 million years ago. This means that longer-term “slow” feedbacks such as melting of ice sheets and changes in permafrost carbon stores are starting to occur now, much quicker than expected, and will likely impact humanity during this century.

Which means that on top of some more warming from rapid feedbacks that has yet to be realised due to thermal inertia we also face the consequences of slow feedbacks already coming into play. These biogeophysical forces are incredibly strong and could become dominant in driving the system. Thus limiting the range of potential future trajectories.


Main point: Earth's climate is more sensitive to forcings than standard scenarios of future warming assumes


Biogeophysical Feedbacks


Some of the key negative (dampening) feedbacks such as carbon uptake by land and oceans and reflectivity by ice and snow that have maintained the Earth system in favourable conditions are weakening. We are now witnessing ever more systems close to or passing a threshold, tipping point, causing abrupt change. The challenge with tipping points is that they're often easiest to identify in retrospect.


For example, Arctic sea ice crossed a tipping point in 2007 and is now in terminal decline and could be gone during the summer by 2040 or earlier. Due to the loss of reflective ice the dark oceans are now absorbing more energy, in turn accelerating regional warming, further melting ice and snow. It also influences jet stream patterns causing more extreme weather events in northern latitudes. The loss of Arctic sea ice has also flipped the Barents Sea from acting as a buffer between the warmer Atlantic and colder Arctic ocean to now being essentially an extension of the Atlantic.

A warmer Arctic also leads to thawing of permafrost in the region. Before believed to be a rather gradual process, new studies show abrupt (decades) thaw in Alaska and Siberia due to the formation of thermokarst lakes. Releasing CO2 and CH4 to the atmosphere and accelerating warming. 

The Greenland ice sheet is now melting rapidly, the ice caps melting irreversibly. Accelerated surface melt has doubled Greenland's contribution to global sea level rise to 0.74 mm per year since 1992–2011. The interior ice sheet could cross a tipping point slightly under 2C warming. Global sea level rise has accelerated to 4.8 mm/yr

The Amundsen Sea sector of the West Antarctic Ice Sheet has already crossed a tipping point and is melting irreversibly. This will likely trigger a collapse of the rest of the West Antarctic Ice Sheet on decadal time scales. Leading to at least 1 meter sea level rise this century. Partial deglaciation of the East Antarctic ice sheet is likely for the current level of atmospheric carbon dioxide, contributing to about 5 metres of sea level rise in the first 200 years.

Melting freshwater pouring into the Atlantic has slowed down the Atlantic Meridional Overturning Circulation (AMOC) that transports heat from the Gulf of Mexico to Northern Europe. Slightly cooling northwest Europe and piling up heat along the southeast waters of the US. This in turn increases temperature differentials between tropical and sub-polar waters that can drive stronger storms. 


Main point: Abrupt changes are already occurring in the climate system, passing 2°C would likely prove catastrophic



Human feedbacks on the system


As I have explained above, the climate system is much more sensitive to even small perturbations than most people think. Another way of showing this fact is to look at human impacts on the climate before industrialisation. 

Since the rise of agriculture, human activities on Earth have played a role in shaping ecological and climatic conditions. There is good evidence to suggest that the rise of agriculture actually had a positive (amplifying) feedback on early climate, hindering a new ice age to occur. 

Atmospheric CO2 and CH4 increases during the last few millennia are anomalous compared to preceding interglacial periods. The same time period when agriculture spread across the continents and emitted greenhouse gases by clearing forests for crops and pastures, domesticating livestock and burning crop residues. Suggesting that emissions were large enough to warm climate and prolong the natural interglacial warmth.



Ruddiman et al. (2016) show evidence for what seems to be a trend brake in naturally falling CO2 and CH4 concentrations some 6000-5000 years ago, towards increasing concentrations most likely driven by anthropogenic forcing.


We know that agriculture spread across the world during this time period. Agrarian civilisations started to flourish along the Nile, Tigris, Euphrates, Indus and Yellow River some 7000-5000 years ago. Cultivation was dependent on flow and ebb cycles that in turn relied on seasonal rains and melting snows packs in the mountains. These formed the conditions for production of surplus food (energy) which allowed societies to expand and grow more complex.



Ruddiman and colleagues show how the development of irrigated rice paddies in Asia and widespread livestock domestication some 5000 years ago coincides with increases in methane emissions. Just like today, forests were cut down, vegetation slashed and burned to make way for agriculture all across Eurasia, Africa and the Americas. This generated CO2 emissions which in turn impacted climate. 

Archeological data records a shift from forest cover to more open vegetation in northern and central Europe that began som 6000-5000 years ago and was complete by the start of the industrial era. Similarly, early deforestation was likely caused around the Mediterranean by extensive land use by Greek and Roman civilisations. In Britain and France, forests had already been reduced to near-modern levels by 2500-2200 years ago.

East central China had widespread forest cover until 8000 years ago, followed by a persistent decrease especially after 6000 years ago. Archaeological sites, proxy for population density, in central China increased thirtyfold between 8000–7000 and 5000–4000 years ago. By 4000 years ago, coal had come into use as a fuel source in the Yellow River Valley because of lack of wood. Deforestation of southern China during the spread of rice agriculture after 5000 years ago added to the ongoing CO2 increase.

In India, sedentary farming and clearance emerged between 5000 and 3500 years ago, with especially rapid settlement expansion on the Deccan Plateau and in the Ganges plains. 

All this evidence provides support for the idea that large-scale deforestation led to a rise in CO2 during the middle and late Holocene. Many models have missed this because they assume low population numbers and small forest clearance per person and thus show low emissions. But this doesn't fit with historical evidence of larger per capita forest clearing 2500-1000 years ago than during industrial times. Probably because land use was inefficient and required large amounts of land but became more intensive over time as agricultural methods changed.



The simulation above indicates much greater deforestation during the millenia preceding the industrial era in agreement with pollen evidence. In contrast, standard reconstructions that assume small constant per capita clearance during preindustrial times show 40-80% of forest cover still persisting in Europe by the year 1800. Meaning massive deforestation must have taken place within the last 200 years to explain current low forest cover. But this doesn't fit with historical evidence of pervasive reforestation in western and central Europe since 1800, not deforestation. 

Main point: The Holocene climate was partly a consequence of human feedbacks on the climate system


Climate Change Adaptation


Changes in temperature and precipitation have always impacted people by affecting what they could and couldn't grow to harvest food (energy) for survival. 

The climate stabilised about 7,000-5,000 years ago coinciding with the flourishing of agrarian civilisations along the Nile, Tigris, Euphrates, Indus and Yellow River. Cultivation was dependent on flow and ebb cycles that in turn relied on seasonal rains and melting snows packs in the mountains. These formed the conditions for production of surplus food (energy) which allowed societies to grow more complex.

But agrarian societies have always been vulnerable to climatic changes. Sudden cooling events or extended droughts caused widespread famines and sometimes collapsed entire communities. Especially vulnerable were those who relied on single crops or undermined the ecological base for survival for example through intense deforestation. 

For example, a sudden cooling that happened around 3,700 to 3,000 years ago greatly influenced populations in Asia. The most dramatic changes were seen in high latitude and high-altitude areas in Mongolia and the Tibetan Plateau. Crops started to fail and widespread famine took hold. This forced people to migrate, shift to more cold resistant crops, or turn to pastoralism. Cooling temperatures also affected Northern China between AD 291-360, a time when the Chinese capital was relocated from Xian to what is now Nanjing, in the south. Again, people would have had to adapt by migrating, changing crops, herding cattle or trading. It was not an easy process and lots of conflicts arose.

The difference now is of course that the rate of change is much more rapid and that its becoming hotter, not colder, which humans have had less of an experience adapting to. Furthermore, there are no virgin lands left to move to when one region becomes uninhabitable, the world is full and most ecosystems severely degraded. Using migration as a tool for adaptation doesn't work that well anymore. We have also become heavily reliant on just a few crops and undermined diversity by eradicating species. This makes our current civilisation very vulnerable to a changing climate.

Main point: Humans can adapt to a changing climate but this time the rate of change is much more rapid and migration is not a good option


Fragile systems under abrupt climate change



We know from our, humanity's, ancient history on this planet that rapid climatic changes ruin agrarian societies. Especially vulnerable are societies that mismanage their resource base and/or live on the margins, for example, in extremely arid regions that are wholly dependent on predictable precipitation patterns. But even societies that manage to survive periods of, say, extreme drought may suffer as they become increasingly fragile to any perturbations to the system.

A changing climate is not bound by any borders and often occur within whole regions or on a global scale. When highly populated areas undergo climatic fluctuations it often cause people to migrate in search of better lands. Which can collapse other, already fragile, societies as the extra pressure from the inflow of people pushes the system over the edge.

This is demonstrated in the German documentary How Climate Made History (2017), above. I highly recommend it and other videos about climate on the youtube channel Hazards and catastrophes. More informative than American or British counterparts.

What can we learn from history? 

Well, first of, Homo Sapiens hunter-gatherers, a generalist species, could adapt easier to extreme environmental conditions than neanderthals which were restricted to specific food sources, methods of hunting, or climates. This ability may have been the result of humans cooperative nature. It had nothing to do with brain size or intelligence.

Second, a relatively stable mild climate and fertile land, with ample and reliable sources of freshwater, plant and animal life, where instrumental to rise of agriculture. People settled and surpluses (food energy) from agriculture could be stored, freeing up time from simply collecting food, and giving rise to specialist occupations. It also gave rise to hierarchies, inequality, as some had more of a surplus than others. Humans also started worshipping the sun (source of energy).

Third, thriving agricultural civilisations were more vulnerable to changes in climatic conditions than nomadic peoples. When the climate changed rapidly and rainfall became unpredictable or rivers dried out people were forced to move in search of new lands to survive. Especially if they managed their lands unsustainably, degraded the land, and were more vulnerable to shocks.

Fourth, in highly populated regions such drastic changes in climatic conditions impacted civilisations both directly and indirectly. High pressure on the land from a large population made societies more susceptible to shocks. As people migrated from poorer lands into other richer areas they tended to destabilise societies that could have survived longer if not for the extra pressure. It also led to unrest and conflict over remaining resources.

Fifth, when civilisations collapsed people spread out to look for resources and knowledge was lost. What we call a dark age occurred.

Implications for modern society

Climate change is occurring rapidly and it is uncertain to what degree we will manage to adapt. We still live in agrarian type societies and are dependent on predictable rainfall, some regions more than others of course. Desertification and water scarcity is a major problem in many parts of the world already. Many societies are extremely fragile to shocks due to overexploitation and land degradation. Crop yields are falling. Seas are rising. Taking for granted that fossil fuels will save us is not a good idea for several reasons. Some societies may succeed better than others in managing their resources but will be vulnerable in other ways, e.g. to climatic changes, financial shocks, trade shocks and/or migration flows. Today there are no new/empty regions to populate once other areas fail. Resources are limited on a global scale.  Tensions over scarcity are rising. Some societies, like Syria, have already collapsed. While others, where most of the remaining resources are located, are having issues with immigration. It will be a very difficult journey for humankind. But as history shows, even if civilisations collapse, humanity survives. We are a tenacious species.

Blowing past 2°C, headed for 4-5°C?



Wishful thinking is today so prevalent that it even has infected the brain of people who are trained not to be biased, scientists. I mean sure, economists have always been blissfully ignorant and wrong in their predictions but what I’m talking about is more widespread. It's a deep denial among the people researching our most critical issues: climate change and energy limitations. 

You see it in the media when scientists discuss oxymorons like “green growth”, or proclaim that we can “decarbonize our entire economy within 20 years”, or that “agriculture will save biodiversity”, or that “lab grown meat will solve our food problems” and so on. It's nothings but grasping at straws in a world that is on fire. Such delusional statements are more about belief systems and identities reflecting values than science. It's also because climate scientists have been told by behavioural psychologists not to scare people as it may hamper action. But isn't it odd that the profession that claims to be devoted to curiosity and truth seeking wants to restrict exploration of future possibilities and censor people due to how it might come across to others?

Our climate reality is harsh. Most scientists tend to underestimate our predicament because they are too conservative, not the other way around. But now it's becoming clear, predictions made by oversimplified climate models have underestimated the changes we're already witnessing due to climate change. Earth, the biosphere, ecosystems and human systems such as the economy are dynamic complex systems and their behaviour is nonlinear. A model that does not include critical feedbacks in the system will not be able to accurately predict results in the real world. This has now become obvious as real world observations about the sad state of our climate is pouring in. Climate change is accelerating.

Sea ice in the Arctic is melting at an alarming rate and looks to be completely gone summertime some time in the coming years (2022?), accelerating global warming further. Ice and snow reflect about 80 percent of the Sun’s energy back into space while the darker ocean and land will absorb 90 percent of that heat. The albedo effect due to vanishing sea ice is already responsible for about 25 percent of global warming (Pistone et al. 2014). Greenland shed about 280 gigatons of ice per year between 2002-2016 and the island’s lower-elevation and coastal areas experienced up to 4 meters of ice mass loss (expressed in equivalent-water-height) over a 14-year period (NASA, 2018). Accelerating rates of ice loss also implies accelerated rates of sea level rise. Certain cities will have to be abandoned. In ten years prior to 2016 the Atlantic Ocean soaked up 50 percent more carbon dioxide than it did the previous decade, speeding up the acidification of the ocean (Woosley et al. 2016). And the list goes on and on with increasingly worrisome observations.

With an increase of carbon emissions of 2% in 2017 (Carbon Brief, 2017), the so called “decoupling” of economic activity from emissions is not yet making a net dent in global emissions. Even if we start reducing emissions now it's not going to be enough to prevent dangerous climate change since there is about a decade lag between emissions and resulting warming (Ricke & Caldeira, 2014). We have already (95% probability) gone past the 2°C warming point/UN target (Raftery et al. 2017), and are  likely headed towards 4-5°C (Steffen et al. 2018). That's because the Earth system is dynamic and is more likely to continue warming until it stabilises at another point, which in the Earth's past occurred at about 4-5°C warmer than pre-industrial levels. By the way, it is generally accepted that a 5 degree rise in temperature is not compatible with human civilisation as we know it. At the same time, perhaps a complete collapse of civilisation could prevent the worst climate change outcomes (Garrett, 2012). But no one is going to promote or talk about that in public. Even if diminishing returns on resources, especially oil, likely will shrink our civilisation in the near future, whether we like it or not (Turner, 2014). 

No one likes either outcomes of this predicament and that's why most experts are basically just arguing over different options of removing carbon from the atmosphere through geoengineering. Using machines to suck out carbon, however, is not feasible both in terms of cost and scale and could cause more harm than good. Current technology would have to be scaled by a factor of 2 million times within 2 years. That's just not going to happen. Biological approaches to carbon capture such as planting trees, restoring soils, holistic grazing, and growing seagrass and kelp appear far more promising. 

Anyway, the real issue for ordinary people is how to adapt to a world that is increasingly hostile while using less energy? Not wasting time listening to myths about "green tech" or believing in fantasies like "colonising Mars" or "geoengineering the entire planet"

Collapsing systems

Credit: Devfactory, CC-BY-SA 2.0

Another great systems theory based book on why nations fail is out. This time its academic, journalist and writer Nafeez Ahmed, who long wrote for the Guardian but now has his own crowdsourced news site (Insurge-intelligence), who has delivered the goods. 

In his book, "Failing states, Collapsing systems: Biophysical Triggers of Political Violence", Nafeez presents the essential data on resource depletion, net energy decline, economic stagnation (debt bubble) and ties it nicely together with the acceleration of civil unrest around the globe. It's a big picture analysis of how the triple crises of energy, climate and food production impact societies around the world. A current example, according to Ahmed, of how these multiple stressors interact and can lead to systemic failure is war torn Syria. 

Syrian oil production peaked in 1996 while population, and thus consumption, kept increasing. By 2008 the government, who relied on petrol money for maintaining the state budget, had to slash fuel subsidies which tripled the price of petrol and food almost overnight. A huge deal to anyone already spending almost half of their income on food. At the same time as an ongoing drought in the eastern part of Syria devastated harvests and drove people from the countryside into the cities. Yemen experienced a similar fate of depleting resources, peak oil, and the resulting high vulnerability to shocks. Based on these two cases it takes about 15 years for a country that experiences its peak in oil production before additional pressures, such as climate change, contribute to systemic failure. 

It's not only the Middle East. Many other countries, for example Mexico,  are well on their way of having little to no extra oil to export for keeping their budget in balance or pay for subsidies that people depend on. And the counties who are still able to import some oil or have some mix of energy sources to depend on will be a target of immigrants looking to flee bankrupt and failing nations. Which in turn will fuel the nationalist sentiments and a grab for what's left, military interventions. Something we are already witnessing in Europe and the US.

Decentralisation trend in Europe - Collapse of civilisations?

Source: Armstrong Economics
People in Europe are getting fed up with the elite. Rising resource costs, austerity, bank bail-outs, tax rate hikes and massive corruption of governments has led to a shattering European Union. Of course there are many different reasons for the increasing decentralisation trend in Europe, but my perspective is that the low ranked members of society has started coalitions to demand that the high ranked members of society share a larger part of their natural resources with the rest. As we all know, economic inequality is at an all time high with half of the worlds total capital in the hands of the top 1%, according to Oxfam

As we can see in the map above there are several so called "separatist" movements popping up all over Europe. As the global resource pie starts to shrink there will be winners and losers, the weakest suffering first. And this is what we see with the PIIGS (Portugal, Ireland, Italy, Greece, and Spain) countries suffering, all time high youth unemployment, increasing refugee flows and homelessness. The trend towards decentralisation is the same as a break up of nations, or collapse of society, controlled by centralised corrupt or ineffective governments. Politicians have not understood or accepted that the Earth is finite and that debts have only postponed the harsh reality of resource depletion and economic down turn. Instead they have promoted perpetually borrowing year-after-year (for the last 30 years) despite that science tells us that we can never pay those loans back.

Now when the global economy is turning down, governments are going to attack ordinary people much more aggressively (increasing taxes, cutting benefits, slashing jobs, negative interest rates etc). Unfortunately most governments will think that if they can only increase taxes they will survive another election cycle. They do not understand that massive deflation, and rapidly rising unemployment, is what kills nations. Some politicians will think about starting international war to shift blame, create a diversion for their own population and to steal resources. Just think about what is happening in Syria right now, its a total mess.

So really it is no wonder that people are getting fed up with the political elite, in Europe and elsewhere, and are trying to return to smaller more local types of decision-making and trading of essential resources (food, water, housing etc). It is what one would expect realising that natural resources are scarce, expensive, and becoming more so. Only a steadily increasing supply of energy can maintain a complex society with a wealthy elite, but when the supply of energy starts falling and the elite gets richer on the backs of ordinary people we can expect social unrest and break up into smaller, simpler groups. I think this is whats happening right now.

Abrupt climate changes in the past

Abrupt climate changes to drier conditions impacted the fall of ancient civilisations in the fertile crescent

New research reveals that some of the earliest civilisations in the Middle East and the Fertile Crescent may have been affected by abrupt climate change. Abrupt climate changes occur in the span of years to decades.

A team of international scientists led by researchers from the University of Miami have found that during the first half of the last interglacial period known as the Holocene epoch, which began about 12,000 years ago and continues today, the Middle East most likely experienced wetter conditions in comparison with the last 6,000 years, when the conditions were drier and dustier.

The Fertile Crescent, a region in west Asia that extends from Iran and the Arabian Peninsula to the eastern Mediterranean Sea and northern Egypt is one of the most climatically dynamic regions in the world and is widely considered the birthplace of early human civilisations. The research team found that transitions in several major civilisations across this region, as evidenced by the available historical and archaeological records, coincided with episodes of high atmospheric dust. Higher fluxes of dust are attributed to drier conditions across the region over the last 5,000 years.

Credit: Arash Sharifi
Climate variability during the past 5000 years is shown in the diagram above. The vertical orange bands denote periods of dry and dusty conditions, which correlate to historical records of drought and famine. Transitions between ruling dynasties (grey arrows) in Iran and North Mesopotamia coincides with the episodes of dry and dusty condition in the region.