Systems Thinking, Climate Psychology, Radiation Physics, and Carbon Cycle Vocabulary

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A vocabulary list defining critical terms across systems dynamics, climate psychology, radiation laws, emissions accounting, and carbon cycle mechanics.

Last updated 12:45 PM on 9/26/26
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20 Terms

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Systems Thinking

Habits and practices used to analyze complex issues at a dynamic structural level.

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Stock

A reservoir or pool in system dynamics that stores mass, energy, or information, possesses inertia or memory, and persists if time is hypothetically frozen.

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Flow

The rate of movement of material, energy, or information between stocks per unit of time.

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Information Deficit Model

The assumption that providing more scientific information or increasing public literacy automatically drives action or closes climate belief gaps.

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Dual-Process Theory

A psychological framework describing the conflict between rational/analytic processing (logical, abstract) and emotional/affective processing (intuitive, vivid), where affective processing typically dominates decision-making.

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Pluralistic Ignorance

A perceptual bias occurring when individuals privately support climate action or hold concern but falsely assume that the majority of others do not share their view.

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False Consensus Effect

A perceptual bias wherein individuals overestimate how widely shared their own personal beliefs or opinions are.

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Agency Frame (A-Frame)

A mitigation framework that reconciles individual (i-frame\text{i-frame}) and structural (s-frame\text{s-frame}) approaches by targeting role-based agency across five key spheres: citizens, professionals, investors, consumers, and role models.

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Blackbody

An idealized physical surface that absorbs and emits 100%100\% of incident radiation strictly as a function of absolute temperature TT in Kelvin.

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Wien's Displacement Law

A radiation law stating that peak emission wavelength λmax\lambda_{\text{max}} is inversely proportional to absolute temperature TT, defined as λmax=2897T μm\lambda_{\text{max}} = \frac{2897}{T}\,\mu\text{m}.

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Stefan-Boltzmann Law

A physical law stating that total radiative energy flux EE emitted per unit area scales with the fourth power of absolute temperature, E=σ⋅A⋅T4E = \sigma \cdot A \cdot T^4, where σ=5.67×10−8 W/m2K4\sigma = 5.67 \times 10^{-8}\,\text{W/m}^2\text{K}^4.

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Albedo

The fraction of incoming solar radiation reflected back into space by a surface or planet, measured as approximately 0.300.30\text{--}0.310.31 for Earth.

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Territorial Emissions

A greenhouse gas accounting framework that measures emissions produced strictly within a country's geographical borders.

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Consumption-Based Emissions

An emissions accounting framework calculated by subtracting embodied carbon in exported goods from territorial emissions and adding embodied carbon in imported goods.

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Airborne Fraction

The proportion of total annual anthropogenic CO2\text{CO}_2 emissions that remains accumulated in the atmosphere, currently approximately 45%45\%.

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Ecological Overshoot

A state in which human resource consumption and waste generation exceed the regenerative and absorptive capacity of Earth's ecosystems.

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Clausius-Clapeyron Relation

A thermodynamic relation dictating that atmospheric moisture-holding capacity increases by approximately 7%7\% for every 1∘C1^\circ\text{C} increase in temperature.

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Silicate Weathering

A natural long-term geological sink process where atmospheric CO2\text{CO}_2 reacts with silicate rocks according to CaSiO3+2CO2+H2O→CaCO3+SiO2+CO2+H2O\text{CaSiO}_3 + 2\text{CO}_2 + \text{H}_2\text{O} \rightarrow \text{CaCO}_3 + \text{SiO}_2 + \text{CO}_2 + \text{H}_2\text{O}.

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Transient Climate Response to Cumulative Carbon Emissions (TCRE)

The near-linear relationship between cumulative total anthropogenic CO2\text{CO}_2 emissions and global mean surface temperature increase.

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Kaya Identity

An identity expressing total CO2\text{CO}_2 emissions as the product of Population, GDP per capita, Energy Intensity of GDP, and Carbon Intensity of Energy.