VOL III — 07 — CYANOTYPE

Climate Science.

A planet wrapped in a thin atmosphere, swallowing sunlight and radiating it back. The accounting is well understood; the consequences are accelerating.

P. 01 / 16 — Energy budget

Earth's energy ledger.

The Sun delivers ~340 W/m² to the top of Earth's atmosphere, on average. About 30 % is reflected (clouds, ice, deserts) — the planetary albedo. The remainder, ~240 W/m², is absorbed and re-radiated as longwave infrared.

Greenhouse gases — H₂O, CO₂, CH₄, N₂O, O₃ — absorb a fraction of that outgoing radiation and re-emit it in all directions, including downward. Net effect: surface stays ~33 K warmer than it would otherwise.

S0(1 − α) / 4 = σ T4eff

Stefan–Boltzmann balance with no atmosphere: Teff = 254 K = −19 °C. With greenhouse: 288 K = 15 °C.

SURFACE TROPOPAUSE 340 incoming 100 reflected 240 absorbed 340 LW up 340 LW back
P. 02 / 16 — Greenhouse Gases

The warming gases.

+1.36 °Cglobal warming, 2024 vs preindustrial
426.9 ppmCO₂ — Mauna Loa monthly mean, May 2024
+3.7 W/m²forcing per CO₂ doubling
2.5 – 4 °Cequilibrium climate sensitivity
P. 03 / 16 — Paleoclimate

The last 800,000 years.

Air bubbles in Antarctic ice (Vostok, EPICA, Dome C cores) preserve a direct sample of past atmospheres. CO₂ in the Pleistocene oscillated between 180 ppm (glacials) and 280 ppm (interglacials), driven by orbital pacing and amplified by ocean–carbon and ice-albedo feedbacks.

The Milankovitch cycles — eccentricity (100 kyr), obliquity (41 kyr), precession (23 kyr) — set the rhythm. The amplitude is the climate system responding.

We blew through the natural ceiling around 1950. CO₂ has not been this high in at least 3 million years (mid-Pliocene), when sea level was 15–25 m higher than today.

ppm CO₂ 450 300 180 years before present (×1000) May 2024 · 426.9 ppm
P. 04 / 16 — Attribution

It's us.

Three independent fingerprints converge on anthropogenic CO₂ as the main driver:

  1. Isotopes. Fossil fuels are ¹⁴C-dead and ¹³C-depleted. Atmospheric δ¹³C is falling, exactly as expected.
  2. O₂ depletion. Combustion consumes O₂; atmospheric O₂/N₂ is falling consistently with the carbon source.
  3. Spectral. Outgoing longwave radiation has decreased in CO₂ absorption bands, while downwelling at the surface has increased.

IPCC AR6 (2021): "It is unequivocal that human influence has warmed the atmosphere, ocean and land."

Forcing decomposition (W/m²)

CO₂+2.16 CH₄+0.54 N₂O+0.21 aero−1.1 solar+0.06

IPCC AR6 effective radiative forcings, 1750–2019.

P. 05 / 16 — Ocean

The great heat sink.

The ocean has absorbed ~91 % of the excess heat trapped by greenhouse gases since 1970, and ~26 % of anthropogenic CO₂. It is the planet's thermal flywheel.

Consequences: thermal expansion (~⅓ of observed sea-level rise), acidification (pH down ~0.1 unit), oxygen loss in many regions, slowing of the Atlantic Meridional Overturning Circulation, marine heatwaves of unprecedented intensity (e.g. North Atlantic 2023, Mediterranean 2022).

Greenhouse_effect
P. 06 / 16 — Cryosphere

Ice in retreat.

Greenland

Mass loss ~270 Gt/yr, 2002–23 (GRACE/GRACE-FO). 7.4 m of potential SLR locked up.

Antarctica

~150 Gt/yr loss; West Antarctic Ice Sheet contains 4.3 m SLR; Thwaites & Pine Island glaciers vulnerable.

Arctic Sea Ice

September minimum: −13 % per decade. First ice-free summer plausible 2030s–40s.

Mountain Glaciers

~270 Gt/yr; ~half of Hindu Kush Himalaya glaciers gone by 2100 in current path.

Permafrost

~1,500 GtC stored. Thawing → CO₂ & CH₄ feedback. Yedoma especially carbon-rich.

Snow cover

Northern-hemisphere June extent down ~20 % since 1970. Cascading water-supply effects.

Glacier edge

PLATE I

Glacial calving front. The cyanotype's natural subject — water in three states.

P. 08 / 16 — Models

The model hierarchy.

0-D EBMs

Single-layer energy balance. T = ((1−α) S₀ / 4σε)^(1/4). On a postcard.

1-D / 2-D

Latitudinal or vertical column models. Manabe–Wetherald (1967): radiative-convective with H₂O feedback.

GCMs

3-D atmosphere/ocean general circulation models. ~25-100 km horizontal grid; primitive equations.

ESMs

Earth System Models: GCM + carbon cycle, dynamic vegetation, ice sheets, atmospheric chemistry.

CMIP6 (2019–) coordinates ~50 modeling groups. Hindcasts since 1850 reproduce the warming pattern only when anthropogenic forcing is included. Forecasts range from SSP1-1.9 (best case, ~1.5 °C peak) to SSP5-8.5 (~4.5 °C by 2100).

FIG. 2
Keeling Curve.
The Keeling Curve — Mauna Loa CO2 measurements show steady annual rise from ~315 ppm (1958) to ~420+ ppm (2024).
P. 09 / 16 — Scenarios

Five futures.

ΔT °C +3 +1.5 2000 2050 2100 SSP1-1.9 SSP2-4.5 SSP5-8.5
P. 10 / 16 — Key Figures

Climate's discoverers.

Joseph Fourier

1768–1830. First to argue, 1824, that Earth's atmosphere acts as an insulator.

Eunice Foote

1856. Showed CO₂ absorbs heat — predating Tyndall by 3 years.

John Tyndall

1859. Quantified IR absorption of H₂O, CO₂, CH₄.

Svante Arrhenius

1896. First quantitative climate sensitivity calc — ~5 °C per doubling.

Roger Revelle

1957. "Geophysical experiment"; ocean uptake limits on CO₂.

Charles Keeling

1958–. The Mauna Loa CO₂ curve.

Syukuro Manabe

1967, 2021 Nobel. First reliable CO₂-doubling GCM.

James Hansen

1988 testimony to U.S. Senate; raised public alarm.

P. 11 / 16 — Timeline

Two centuries of warning.

1824

Fourier proposes the greenhouse mechanism.

1856

Foote: "An atmosphere of [CO₂] would give to our earth a high temperature."

1896

Arrhenius computes ΔT for ×2 CO₂.

1938

Guy Callendar links CO₂ rise to observed warming.

1958

Keeling begins continuous CO₂ measurement at Mauna Loa.

1979

Charney Report: ECS = 1.5–4.5 °C.

1988

IPCC founded; Hansen testifies.

1992

UN Framework Convention on Climate Change (Rio).

1997 / 2005

Kyoto Protocol signed / enters force.

2015

Paris Agreement: hold < 2 °C, pursue 1.5 °C.

2021

IPCC AR6 WG1: human role unequivocal.

2024

First calendar year > 1.5 °C above preindustrial.

Sea_level_rise
P. 12 / 16 — Pull Quote

"It is unequivocal that human influence has warmed the atmosphere, ocean and land."— IPCC AR6 WG1, Summary for Policymakers, 2021

P. 13 / 16 — Impacts

What changes.

Heatwaves

Frequency & intensity rise faster than the mean. Pacific NW 2021: +5σ event, attributed virtually impossible without warming.

Tropical cyclones

Frequency uncertain; intensity (Cat 4–5) and rainfall up. Slower translation = more flooding.

Drought & flood

Wet regions wetter, dry drier; extremes amplified. Western US "megadrought" 2000–22 worst in 1,200 yr.

Wildfire

VPD ↑, fire season ↑. 2023 Canadian fires emitted ~1,300 Tg CO₂ — > many countries.

Food & water

Crop yield projections −5 to −30 % by mid-century in tropics; adaptation partial.

Health

~37 % heat-related deaths attributable to climate change (Lancet Countdown 2024).

P. 14 / 16 — Mitigation

The solution wedges.

Solar PV

Cost down 90 % since 2010. ~3 TW installed globally. Adds ~600 GW/yr.

Wind

Onshore + offshore. ~1 TW installed. LCOE competitive with gas.

Nuclear

~10 % of global electricity. SMRs in development. Lifetime extensions.

Storage

Li-ion, sodium-ion, flow batteries, pumped hydro. Cost trajectory matches PV.

Electrification

Heat pumps, EVs. Doubles end-use efficiency typically.

CDR

Direct air capture, BECCS, biochar, ocean alkalinization. Needed at GtC scale by 2050.

Land use

Reforestation, soil carbon, regenerative agriculture, halt deforestation.

Methane

Leak detection (MethaneSAT 2024), agricultural feed additives, livestock improvements.

P. 15 / 16 — Open Questions

What we still don't know.

P. 16 / 16 — Go Deeper

Watch & read.

MinutePhysics & Kurzgesagt — Climate Series

Plus PBS Terra "Weathered" for extreme-weather attribution stories.

Watch ↗

References

  • IPCCAR6 reports (WG1 2021, WG2 2022, WG3 2022)
  • PierrehumbertPrinciples of Planetary Climate (2010)
  • Wallace & HobbsAtmospheric Science
  • Hansen et al.numerous, on equilibrium sensitivity
  • Carbon Briefcarbonbrief.org — daily updates
  • Project Drawdowntechnology-by-technology mitigation atlas