GenesisAeon
P105 · v1.0.1 · 2026-08-31
Black Carbon Albedo
black-carbon-albedo-utac
Black carbon / light-absorbing-particle albedo feedback on glaciers: Kang et al. 2020's mechanism review, Li et al. 2017's Central Tibetan Plateau melt-enhancement case, and Yang, Kang, Chen et al. 2025's plateau-wide solid-water-storage decline study. A new atmospheric-deposition lens on the P99-P104 series, contrasting aerosol-masking-utac's global cooling effect. Deliberately no UTAC/CREP/AFET bridge. GenesisAeon P105.
Live von GitHub, Stand 11.09.2026, 20:52
Laienverständliche Fassung (Deutsch)
Paket-DOI
Keine eigene Paket-DOI in CITATION.cff oder .zenodo.json.
Quellen-DOIs
Literatur je Paket
A review of black carbon in snow and ice and its impact on the cryosphere
Earth-Science Reviews, 2020
10.1016/j.earscirev.2020.103346Light-absorbing impurities accelerate glacier melt in the Central Tibetan Plateau
Science of the Total Environment, 2017
10.1016/j.scitotenv.2017.02.169Reduced solid water storage over the Tibetan Plateau caused by black carbon
Communications Earth & Environment, 2025
10.1038/s43247-025-02335-9
Schlagworte
Disclaimer
DISCLAIMER — Real Science, No Framework Bridge
Why no UTAC/CREP/AFET bridge: not only because the cited literature
already provides the necessary quantitative structure -- a deliberate
choice. This project's highly speculative AFET/UTAC experiments must
never stand in the way of climate/ecology topics being accessible and
usable to people who don't work inside that construct and aren't
looking for renormalization groups. Real, checkable science, without
the burden of an unproven framework. See PACKAGE_REGISTRY.md's "Why
no UTAC/CREP/AFET bridge in the climate/ecology series" (2026-08-31) in
the GenesisAeon workspace root for the full canonical note.Status: Real, independently verified science. NO UTAC/CREP/AFET bridge.
What this is
Every figure in this package was checked directly against the paper (DOI lookup or publisher abstract) on 2026-08-15.
- Kang, Zhang, Qian & Wang (2020), Earth-Science Reviews 210,
- 103346, DOI: 10.1016/j.earscirev.2020.103346 — the foundational,
- widely-cited synthesis review of black carbon's impact on the
- cryosphere, real mechanism, real ablation-zone-enrichment pattern.
- Li, Kang, He et al. (2017), Science of the Total Environment
- 587-588, 482-490, DOI: 10.1016/j.scitotenv.2017.02.169 — a real,
- measured single-glacier case (Xiao Dongkemadi Glacier, central
- Tibetan Plateau, 2014-2015): light-absorbing impurities enhanced
- summer melt by ~15%.
- Yang, Kang, Chen et al. (2025), *Communications Earth &
- Environment* 6, 430, DOI: 10.1038/s43247-025-02335-9 — a real,
- decade-long (2007-2016), plateau-wide study: BC's direct
- (albedo-reduction) effect increased melt by 7.5%, BC's indirect
- (precipitation-suppression) effect added a further 6.1% mass loss,
- against a total ob
…
README
Technische Dokumentation (Englisch)
black-carbon-albedo-utac
GenesisAeon Package 105 — black carbon / light-absorbing-particle albedo feedback on glaciers. A new lens on the P99–P104 series: atmospheric deposition physics, not water balance, geophysics, or governance. Deliberately has no UTAC/CREP/AFET bridge — see DISCLAIMER.md.
For a plain-language explanation of the same topic (German, no jargon, written for general audiences), see WHITEPAPER.md.
The core idea
Soot and other light-absorbing particles deposited on snow/ice reduce albedo, increase absorbed solar radiation, and directly accelerate melt — a mechanism independent of, and additional to, greenhouse-gas warming. It's also a positive feedback: as darkened ice melts, the black carbon within it concentrates at the surface exactly where melt is already happening, further darkening it.
A deliberate, honest contrast to this ecosystem's aerosol-masking-utac: there, aerosols mask warming globally (a cooling effect, from reduced shipping-fuel sulfate). Here, aerosols deposited on the cryosphere accelerate melt locally (a warming effect, from black carbon). Same broad class of atmospheric particles, opposite climate role depending on where they end up.
What's real here
- Kang, Zhang, Qian & Wang (2020, Earth-Science Reviews)* — the
- foundational synthesis review of the mechanism: BC concentrations in
- glacier ablation-zone aged snow/ice are commonly 1–3 orders of
- magnitude higher than in accumulation-zone fresh snow, as the
- darkening/melt/re-concentration cycle self-reinforces.
- Li et al. (2017, Science of the Total Environment)* — a real,
- measured case: light-absorbing impurities enhanced summer melt on
- the Xiao Dongkemadi Glacier, central Tibetan Plateau, by ~15%
- (2014–2015 field seasons).
- Yang, Kang, Chen et al. (2025, Communications Earth &
- Environment)* — a real, decade-long (2007–2016), plateau-wide
- study separating BC's direct effect (albedo → melt, +7.5%) from
- its indirect effect (BC-suppressed precipitation → +6.1%
- additional mass loss), against a total observed solid-water-storage
- decline of 33.7% — explicitly not the same number as BC's
- own combined contribution (13.6 percentage points, about 40% of the
- total decline). See
bc_attributable_fraction_of_total_decline().
Quickstart
bash pip install black-carbon-albedo-utac
```python from black_carbon_albedo_utac import ( is_positive_feedback, ablation_zone_enrichment_range, XIAO_DONGKEMADI_2017, TIBETAN_PLATEAU_2025, bc_total_effect_pct, bc_attributable_fraction_of_total_decline, )
print(is_positive_feedback()) # True print(ablation_zone_enrichment_ran
…
Verwandte Pakete
Gletscher & Kryosphäre
Die explizit im Ökosystem selbst so benannte 'P99-P103-Serie' (glacier-buffer -> glacier-buffer-replacement, 'companion to P99' -> distributed-buffer-resilience, 'companion to P99 and P100'), mit mountain-governance-adaptation-utac (P104) als selbstbezeichnetem 'governance/institutional closing chapter of the P99-P103 series'. black-carbon-albedo-utac (P105) ist explizit 'a new atmospheric-deposition lens on the P99-P104 series'. freshwater-ecosystem-stressors-utac (P106) ist explizit 'the ecological bridge between the P99-P102 physical series and the P103-P104 resilience/governance series'. landscape-restoration-hydrology-utac (P107) 'extends the P99/P103 distributed-buffer series'; urban-green-infrastructure-utac (P108) ist explizit 'companion to landscape-restoration-hydrology-utac (P107)'. glacier-legacy-contaminants-utac (P109) 'bridges glacier-buffer-utac (P99), black-carbon-albedo-utac (P105), and freshwater-ecosystem-stressors-utac (P106)'. snowpack-elevation-warming-utac (P110) 'quantifies distributed-buffer-resilience-utac's (P103) unquantified snow buffer category and extends glacier-buffer-utac's (P99) peak-water framing'. tropical-glacier-ecosystem-rle-utac (P123) erweitert den Puffer-Verlust-Mechanismus in Richtung IUCN-RLE-Kollaps-Diagnostik. glacier-microbiome-succession-utac (P129) benennt sich selbst als verwandt zu, aber unterschieden von, P99/P106/P123 (siehe sein eigenes relative_change_honesty_check-Modul) -- dokumentiert die Physikochemie und das Mikrobiom des Gletscherbachs selbst, nicht Abflussmenge, Ökosystem-Stress oder RLE-Status. Alle Zitate stammen wörtlich aus den jeweiligen Paket-Abstracts.
- P99Glacier Bufferglacier-buffer-utac
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- P101Glacial Seismicityglacial-seismicity-utac
- P102Paraglacial Hazardparaglacial-hazard-utac
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- P104Mountain Governance Adaptationmountain-governance-adaptation-utac
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- P107Landscape Restoration Hydrologylandscape-restoration-hydrology-utac
- P108Urban Green Infrastructureurban-green-infrastructure-utac
- P109Glacier Legacy Contaminantsglacier-legacy-contaminants-utac
- P110Snowpack Elevation Warmingsnowpack-elevation-warming-utac
- P123Tropical Glacier Ecosystem Rletropical-glacier-ecosystem-rle-utac
- P129Glacier Microbiome Successionglacier-microbiome-succession-utac