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Ecology and sustainability · Sustainability and global change

Climate change

Picture a record-breaking January cold snap in Chicago, and someone saying, "So much for global warming!" Is that right? By the end of this page you'll be able to answer. First, a surprising fact: without the greenhouse effect, the Earth's average temperature would be about $-18\ \text{°C}$ ($0\ \text{°F}$), a frozen planet uninhabitable for life as we know it. The problem is not that the greenhouse effect exists, but that human activities are intensifying it much faster than ecosystems can keep up with.

The natural greenhouse effect

The Moon is about the same distance from the Sun as Earth but has no atmosphere, so its average temperature is about $-18\ \text{°C}$ (and swings wildly between day and night), whereas that of our planet is around $+15\ \text{°C}$ (59 °F): what atmospheric mechanism retains heat and stops the Earth's surface from being a frozen desert?

Diagram of the natural greenhouse effect: visible solar radiation reaches the Earth's surface, the surface emits infrared towards space, and the greenhouse gases in the atmosphere send part of that heat back to the surface. Sun atmosphere (with GHGs) Earth's surface 1. visible solar radiation 2. infrared emitted 3. part returns to the surface

Greenhouse gases (GHGs)

Not all gases trap heat equally. Three key ones: carbon dioxide ($\text{CO}_2$), methane ($\text{CH}_4$) and nitrous oxide ($\text{N}_2\text{O}$). Water vapor and CFCs also trap heat.

Gas Main human source
$\text{CO}_2$ burning fossil fuels, deforestation
$\text{CH}_4$ livestock, rice paddies, landfills, natural gas leaks
$\text{N}_2\text{O}$ nitrogen fertilizer on farm fields
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Look at the greenhouse effect diagram. Explain what each numbered arrow (1, 2, and 3) represents, why the natural greenhouse effect is essential for life on Earth, and…

Look at the greenhouse effect diagram. Explain what each numbered arrow (1, 2, and 3) represents, why the natural greenhouse effect is essential for life on Earth, and what the human-caused alteration of it consists of.

atmosphere (with GHGs) Earth's surface 1 2 3
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Name three greenhouse gases, state the main source of each, and indicate which contributes most to current warming and why.

Name three greenhouse gases, state the main source of each, and indicate which contributes most to current warming and why.

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Weather, climate and the evidence for warming

Comparative graph showing short-term fluctuations in weather superimposed on a continuous upward trend line that represents the long-term warming of the climate. climate trend daily data fluctuate a lot; the long-term trend rises
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Distinguish between weather and climate, and explain why a week of intense cold in winter does not contradict the global warming trend, drawing on the difference between…

Distinguish between weather and climate, and explain why a week of intense cold in winter does not contradict the global warming trend, drawing on the difference between an isolated data point and a long-term average.

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Name two pieces of evidence of climate change observed in Spain (the retreat of the Pyrenean glaciers, earlier flowering, more frequent heat waves, rising sea level on…

Name two pieces of evidence of climate change observed in Spain (the retreat of the Pyrenean glaciers, earlier flowering, more frequent heat waves, rising sea level on the coast) and explain what each one consists of.

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Describe two consequences of climate change already observable in the ecosystems of the Iberian Peninsula and explain the physical or biological mechanism that produces…

Describe two consequences of climate change already observable in the ecosystems of the Iberian Peninsula and explain the physical or biological mechanism that produces them.

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The rise in CO2 and its human cause

Graph of atmospheric CO₂ concentration: it rises from 280 ppm in pre-industrial times (around 1750) to 420 ppm today, with an increasingly rapid rise. Time CO₂ (ppm) 280 ppm (pre-industrial) 420 ppm (today) ≈ 1750 Today +140 ppm ≈ +50 %

The carbon cycle connection

Carbon moves between reservoirs: atmosphere, oceans, plants and soils, and fossil fuels. Photosynthesis removes $\text{CO}_2$ from the air; respiration and decomposition return it. Fossil fuels are carbon stored for millions of years. Two human processes added the extra $\text{CO}_2$: burning fossil fuels (coal, oil, natural gas) moves carbon from underground to the air in decades, and deforestation removes trees that would absorb $\text{CO}_2$ (and burning them releases it).

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Relate the carbon cycle to the increase in atmospheric $\text{CO}2$ since the Industrial Revolution, naming the two human processes that contribute most to this increase.

Relate the carbon cycle to the increase in atmospheric $\text{CO}_2$ since the Industrial Revolution, naming the two human processes that contribute most to this increase.

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The concentration of atmospheric $\text{CO}2$ has gone from around $280\ \text{ppm}$ in pre-industrial times to around $420\ \text{ppm}$ today. Calculate the percentage…

The concentration of atmospheric $\text{CO}_2$ has gone from around $280\ \text{ppm}$ in pre-industrial times to around $420\ \text{ppm}$ today. Calculate the percentage increase and discuss what would have happened to ecosystems if this increase had occurred over centuries instead of less than two.

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Consequences: sea level, albedo and feedbacks

Comparison of albedo: over sea ice most of the sunlight is reflected, whereas the open ocean reflects little light and absorbs more energy, which warms it. solar radiation reflected light Ice: high albedo reflects a lot of light solar radiation little reflection heat Ocean: low albedo absorbs more heat

Thermal expansion, ocean changes, heat waves, mountain snow and methane

Ocean warming and acidification: the oceans absorb more than 90% of the extra heat trapped by greenhouse gases, so surface waters warm, hold less dissolved oxygen, and stress marine life. The oceans also absorb about a quarter of human $\text{CO}_2$. It reacts with water: $\text{CO}_2 + \text{H}_2\text{O} \rightarrow \text{H}_2\text{CO}_3$ (carbonic acid), which lowers ocean pH (ocean acidification) and makes it harder for corals, oysters and other shell-builders to form calcium carbonate shells. Warm water also causes coral bleaching: stressed corals expel their symbiotic algae and can starve, as in the Florida Keys and Hawai'i reefs.

Thermal expansion: water expands slightly as it warms, so a warmer ocean takes up more volume. Together with melting glaciers and ice sheets, this is the second main cause of sea level rise.

A heat wave is a period of abnormally hot weather, often defined as several days (usually 2 or more) above a high local temperature threshold. If the average shifts up by 1-2 °C, the whole range of temperatures shifts, so extreme hot days that were rare become common, last longer and get hotter.

Mountain snow: in the Rockies and Sierra Nevada, warmer winters mean more precipitation falls as rain and snow melts earlier. Rivers such as the Colorado carry more water in winter and spring and less in summer, when cities and farms need it most.

Permafrost: as frozen soil thaws, trapped organic matter decomposes. In waterlogged, oxygen-poor conditions (thermokarst lakes, peatlands), microbes release methane ($\text{CH}_4$); with oxygen, they release $\text{CO}_2$. This is another positive feedback.

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Explain what the albedo of a surface is, which surfaces on Earth have a high albedo and which have a low one, and why the melting of Arctic sea ice reduces the planet's…

Explain what the albedo of a surface is, which surfaces on Earth have a high albedo and which have a low one, and why the melting of Arctic sea ice reduces the planet's average albedo.

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What is a heat wave and how is it defined meteorologically? Explain why, in a warmer climate, heat waves are expected to become more frequent, longer, and more intense…

What is a heat wave and how is it defined meteorologically? Explain why, in a warmer climate, heat waves are expected to become more frequent, longer, and more intense even if the average temperature only rises by one or two degrees.

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Sea level rises for two main reasons: the thermal expansion of water as it warms and the input of water from glaciers and continental ice sheets. Explain both mechanisms…

Sea level rises for two main reasons: the thermal expansion of water as it warms and the input of water from glaciers and continental ice sheets. Explain both mechanisms and discuss, using Archimedes' principle, why the melting of floating sea ice barely contributes to the rise.

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The average temperature of the Iberian Peninsula has already risen by more than $1.5\ \text{°C}$ since pre-industrial times. Explain what consequences this warming has…

The average temperature of the Iberian Peninsula has already risen by more than $1.5\ \text{°C}$ since pre-industrial times. Explain what consequences this warming has for the snow cover of Spanish mountains and how it changes the flow regime of the rivers that rise in them (more water in winter, less in summer).

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Imagine that global warming exceeds the $+1.5\ \text{°C}$ threshold, triggering accelerated processes in high northern latitudes.\na) Model the interaction between the…

Imagine that global warming exceeds the $+1.5\ \text{°C}$ threshold, triggering accelerated processes in high northern latitudes.\na) Model the interaction between the summer melting of Arctic sea ice and the oceanic radiative balance using a cause-and-effect flow chart. Predict the impact of this loop on heat absorption by the water and on ice formation in subsequent winters.\nb) Thermokarst lakes form in peatlands and thawing permafrost soils. Reason under what biogeochemical conditions the decomposition of organic matter will predominantly release $\text{CH}_4$ instead of $\text{CO}_2$, and justify, based on the relative radiative forcing capacity of both gases, why this worsens short-term forcing.\nc) Based on both mechanisms, justify what a "tipping point" is and argue why, once crossed, the total cessation of anthropogenic emissions might not be sufficient to stop warming.

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Mitigation and adaptation

Internationally, the Kyoto Protocol and the Paris Climate Accord commit countries to limiting greenhouse gas emissions; the Paris Accord aims to keep warming well below 2 °C. Faced with the advance of the climate crisis, a city like Houston can choose to run fleets of electric buses to cut emissions, or to plant shade trees and build flood barriers after hurricanes such as Harvey: why does managing climate change require distinguishing between tackling the origin of the warming and preparing for its unavoidable consequences?

Illustration with two panels: mitigation acts on the cause (a chimney emitting CO₂, a tree absorbing it and an electric bus) and adaptation acts on the effect (a shade tree against heat and a flood barrier against rising seas). mitigation tackle the cause adaptation deal with the effect CO₂ electric bus shade flood barrier

Sinks, scenarios, net zero and fairness

Carbon sequestration is the long-term storage of carbon out of the atmosphere. Natural sinks: forests (carbon in wood, for decades to centuries), soils (organic matter, decades to millennia) and oceans (dissolved $\text{CO}_2$ and shells, centuries or more).

Net zero means emissions are balanced by removals: what we still emit is offset by sinks or technology. It does not mean emitting nothing.

A climate scenario is a projection of future climate under assumptions about emissions. Because future energy, economic and population choices are uncertain, scientists give a range of outcomes rather than one temperature.

Maladaptation is an adaptation that increases emissions, harms others or fails later. Snowmaking at a ski resort uses energy and water and only delays the problem.

Fairness: countries differ in historical emissions, current emissions per person and ability to adapt. Small island states emit little but face sea level rise and saltwater in their aquifers.

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Explain what carbon sequestration is and name two natural carbon sinks (forests, soils, oceans, peat bogs), indicating how they store carbon and for how long.

Explain what carbon sequestration is and name two natural carbon sinks (forests, soils, oceans, peat bogs), indicating how they store carbon and for how long.

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Differentiate between mitigation and adaptation strategies for climate change and give two specific examples of each, indicating at what scale (local, national, or…

Differentiate between mitigation and adaptation strategies for climate change and give two specific examples of each, indicating at what scale (local, national, or global) they are applied.

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The IPCC works with emissions scenarios, from the very ambitious to the very high. Explain what a climate scenario is, why science cannot announce a single future…

The IPCC works with emissions scenarios, from the very ambitious to the very high. Explain what a climate scenario is, why science cannot announce a single future temperature, and what role human decisions (energy, economy, demography) play in the range of outcomes.

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Many countries have committed to "carbon neutrality" by 2050. Explain what reaching net zero emissions means, what role removals by sinks play in the balance, and why it…

Many countries have committed to "carbon neutrality" by 2050. Explain what reaching net zero emissions means, what role removals by sinks play in the balance, and why it does not mean stopping emitting altogether.

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Salt marshes and Posidonia seagrass meadows store large amounts of carbon in their sediments ("blue carbon"). Explain why they are especially effective and long-lasting…

Salt marshes and Posidonia seagrass meadows store large amounts of carbon in their sediments ("blue carbon"). Explain why they are especially effective and long-lasting sinks, and discuss what happens to that carbon when a marsh is drained or a meadow is destroyed by anchoring and construction work.

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Design a mitigation plan for your local area: choose three sectors (for example, energy, transportation, and carbon sinks) and justify, for each proposed action, how it…

Design a mitigation plan for your local area: choose three sectors (for example, energy, transportation, and carbon sinks) and justify, for each proposed action, how it reduces emissions or increases removals and what co-benefits it brings.

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A ski resort at an altitude of $1800\ \text{m}$ in the Rocky Mountains has seen its average natural snow season reduced from 120 to 75 days over the last three decades.…

A ski resort at an altitude of $1800\ \text{m}$ in the Rocky Mountains has seen its average natural snow season reduced from 120 to 75 days over the last three decades. To sustain economic activity, the management company plans to build a $200\,000\ \text{m}^3$ water reservoir and install artificial snow guns to cover $80\ \%$ of the skiable area.\na) Justify why this technical solution can be considered an example of "maladaptation", analyzing its energy balance, its carbon footprint, and the impact on water availability for downstream river ecosystems.\nb) If the winter $0\ \text{°C}$ isotherm rises an additional $150\ \text{m}$ over the coming decades, evaluate the thermodynamic limits of technical snowmaking (wet-bulb temperature) and predict the medium-term viability of the resort.\nc) Design an alternative socioeconomic and ecological adaptation proposal for the valley that replaces snow monoculture, justifying how it diversifies employment and protects alpine biodiversity.

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Analyze the following data from two countries ahead of an international climate summit:\n• Country A (developed country): Population: 40 million; cumulative historical…

Analyze the following data from two countries ahead of an international climate summit:\n• Country A (developed country): Population: 40 million; cumulative historical emissions (1850-2020): $18\ \%$ of the global total; current per capita emissions: $12\ \text{t}$ of $\text{CO}_2$/year; GDP per capita: $\$42\,000$.\n• Country B (small island developing state): Population: 1 million; cumulative historical emissions: $<0.05\ \%$; current per capita emissions: $1.2\ \text{t}$ of $\text{CO}_2$/year; GDP per capita: $\$3\,000$; its territory suffers from aquifer salinization and irreversible coastal erosion due to sea level rise.\na) Apply the principle of "common but differentiated responsibilities and respective capabilities" to justify what specific financing and mitigation obligations Country A must assume regarding the Loss and Damage Fund for the benefit of Country B.\nb) Country A proposes setting an identical $40\ \%$ cut in emissions for all countries relative to their current levels by 2035. Evaluate the asymmetric impact of this proposal on Country B using climate justice and socioeconomic development criteria.\nc) Design an equitable criterion for sharing the mitigation effort that weights cumulative historical emissions, per capita emissions, and the Human Development Index, justifying why equity is an indispensable requirement for the effectiveness of climate agreements.

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Summary

Back to the start: a cold snap in Chicago is weather, not climate, so it does not disprove global warming.

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