NATS 1780 – Energy & Earth’s Atmosphere: Comprehensive Study Notes

The UV Index

  • Introduced in 1992, originating in Canada; internationally recognized 1994, adopted globally 2002
  • Purpose: communicate potential health risk from solar UVR to public
    • RiskαUV IndexαUV Intensity\text{Risk} \alpha \text{UV Index} \alpha \text{UV Intensity}
    • Health Safety1UV Index\text{Health Safety} \propto \frac{1}{\text{UV Index}}
  • Scale (Canada): 0–11+ (higher = more risk)
  • Depends on:
    • Stratospheric ozone thickness (daily variability; anthropogenic + natural)
    • Solar elevation angle (greatest at local solar noon; longer path length when Sun low)
    • Cloud cover (thick clouds attenuate UV)
  • Dose concept
    • UV Dose=UV Index×Time of Exposure\text{UV Dose} = \text{UV Index} \times \text{Time of Exposure}
  • Daily pattern: rises after sunrise → peak at local solar noon → zero at night
  • Seasonal pattern (Toronto example): maximum near Summer Solstice, minimum near Winter Solstice, moderate at Equinoxes
  • Effectiveness: Systematic review (Italia & Rehfuess, 25 studies) – low familiarity & understanding, minimal influence on protective behaviour.
Health Impacts of UV
  • Acute: sunburn, photokeratitis
  • Chronic: cataracts, skin aging, skin cancer, immunosuppression
Types of UV Radiation
  • UVA (315–400 nm): not absorbed by ozone; penetrates deepest; “most concerning”
  • UVB (280–315 nm): partially absorbed; causes sunburn; still concerning
  • UVC (100–280 nm): totally absorbed by ozone & atmosphere; no ground-level exposure
Sunscreen Technology
  • Physical / Mineral (ZnO, TiO2)
    • Reflects & scatters UV; broad spectrum; immediate protection; may leave white cast; good for sensitive skin/children
  • Chemical / Organic (avobenzone, oxybenzone, octinoxate…)
    • Absorbs UV → converts to heat; requires 15–30 min to activate; cosmetically elegant
  • Both can be broad spectrum (UVA + UVB) depending on formula
Environmental Concerns
  • Release pathways: direct wash-off (swimming, boating), wastewater effluent, sludge, landfill leachate, airborne particulates during application
  • UV-filter pollutants: large suite of organics (PABA, benzophenones, cinnamates, salicylates, triazines, camphor derivatives, benzimidazoles, phenols) + inorganics (nano/non-nano TiO2, ZnO)
  • Ecotoxicological impacts along molecular → community levels (Hodge 2025, Marine Pollution Bull.)

Radiation & Energy Transfer

  • Three heat-transfer modes: conduction, convection, radiation
  • Key question: How does solar energy reach Earth? → via radiation (EM waves)
  • Wave properties: wavelength λ\lambda & frequency ff (inverse relation c=λfc = \lambda f)
  • Microwave oven example: uses 2.45 GHz radiation to excite polar water molecules (heating)
Electromagnetic Spectrum
  • Spectrum spans radio (10³ m) → γ-ray (10⁻¹² m)
  • Only certain bands penetrate atmosphere (radio, visible, parts of IR)
  • Wien’s Displacement Law (1893): λmax=bT\lambda_{max} = \frac{b}{T} with b = 2.898\times10^{-3}\;\text{m·K}
    • Sun’s T5,773KT \approx 5{,}773\,\text{K}λmax5.02×107m=502nm\lambda_{max} \approx 5.02\times10^{-7}\,\text{m} = 502\,\text{nm} (blue-green visible)
  • Solar spectrum reaching top-of-atmosphere (ToA): ~48 % visible, 7 % UV, 44 % near-IR
Atmospheric Absorption
  • Gases absorb strongly in UV (O₃) & IR (H₂O, CO₂, CH₄, N₂O) bands; visible largely passes through “atmospheric window”
  • Result: Downwelling long-wave (DWLW) < 50 % of downwelling short-wave (DWSW) measured at surface
Greenhouse Effect
  • Natural GE: water vapour dominant; keeps mean surface 15C\sim 15\,^{\circ}\text{C} vs 18C-18\,^{\circ}\text{C} without atmosphere
  • Anthropogenic GE: added GHGs (CO₂, CH₄, N₂O) enhance IR trapping → warming
  • Correlation vs causation: CO₂ and temperature strongly correlated (HadCRUT/NOAA); causality attributed to radiative forcing physics

Daily & Seasonal Energy Balance

  • Insolation (visible) passes atmosphere, absorbed by land/ocean (≈47 % of incoming)
  • Absorbed energy re-emitted as IR; troposphere heated from ground up
  • Diurnal cycle: solar noon → maximum insolation, but TmaxT_{\text{max}} occurs later due to thermal inertia (radiative transfer time-lag)
    • Cloud cover modulates DWSW (EMOS May 26 2025 example shows DWSW deficit during cloud passage; TmaxT_{\text{max}} ~2.5 h earlier than DWSW = UWLW)
  • Night-time radiational cooling: continued IR emission without solar input
  • Seasonal cycle driven by axial tilt → latitude-dependent insolation (CHELSA global map, winter vs summer solstice patterns)
Planetary Energy Budget (Trenberth 2009)
  • Incoming SW: 341W m2341\,\text{W m}^{-2}
    • Reflected (albedo): 101.9W m2101.9\,\text{W m}^{-2} (clouds + surface)
    • Absorbed by surface: 161W m2161\,\text{W m}^{-2}
    • Absorbed by atmosphere: 79W m279\,\text{W m}^{-2}
  • Surface emits 396W m2396\,\text{W m}^{-2} IR; atmosphere back-radiates 333W m2333\,\text{W m}^{-2} downward
  • Net imbalance ~ 0.9W m20.9\,\text{W m}^{-2} (positive) → warming

Energy Balance Climate Model (EBCM)

  • Pedagogical spreadsheet model built for NATS 1780 based on process-flow diagrams (Ahrens Fig 2.15, 2.16)
  • Balances energy at each node; useful for “what-if” scenarios (ice age, geoengineering, altered solar constant, pandemic emissions drop)
  • Example scenario – COP-21 Paris Agreement
    • Δ[CO2]=146ppm\Delta[CO_2] = 146\,\text{ppm} (≈2.2 ppm yr⁻¹ reaching 2081)
    • +3 % increase in atmosphere → IR re-emission back to surface
    • Predicts ΔT2C\Delta T \approx 2^{\circ}\text{C} warming
  • Limitations: “toy” level – lacks full physics, chemistry, equations, spatial resolution

Preliminary & Key Takeaways

  • UVA & UVB constitute primary health risks; UVC fully filtered by ozone
  • UV Index communicates risk but behaviour change remains limited
  • Visible light (44 %) is the dominant energy input driving atmospheric circulation; UV only 7 % of solar flux
  • Earth’s surface absorbs visible → emits IR; greenhouse gases trap part of this IR, warming troposphere
  • Tropospheric heating is bottom-up
  • Rising GHG concentrations ⇒ ΔT[GHG]\Delta T \propto [\text{GHG}] → global warming
  • Energy balance frameworks (daily, seasonal, planetary) enable quantitative climate reasoning; simple models (EBCM) illustrate scenario impacts
  • Only anthropogenic enhancement of GE is problematic; natural GE is essential
  • Water vapour, though strongest GHG, is controlled by temperature-dependent feedbacks (question deferred)

Frequently Tested Concepts / Sample MCQ Answers

  • Daily UV pattern: C (Increases from sunrise, peaks at local solar noon, disappears at sunset)
  • Incorrect energy-budget statement slide 40: C (Insolation is converted into IR via radiative transfer) – actually correct → so the intended incorrect one is D? (Check original; teacher flags heating from ground up as correct)
  • EBCM incorrect statement slide 74: E (EBCM can be applied to real-world examples such as Paris Agreement) – considered illustrative only

Key Equations

  • UV Dose=UV Index×t\text{UV Dose} = \text{UV Index} \times t
  • λmax=bT\lambda_{max} = \dfrac{b}{T} with b = 2.898\times10^{-3}\,\text{m·K}
  • ΔT[GHG]\Delta T \propto [\text{GHG}] (qualitative alpha-statement)

Ethical / Practical Implications

  • Sunscreen chemicals pose emerging marine pollution threat – calls for greener formulations & policy
  • Public-health messaging (UV Index) must improve to translate awareness into behaviour change
  • Mitigating climate change requires curbing anthropogenic GHGs; models (even simple) inform policy (Paris Agreement, geoengineering debates)