GenesisAeon
P99 · v1.0.1 · 2026-08-31
Glacier Buffer
glacier-buffer-utac
Real glacial hydrological buffer (peak water) and downstream buffer-loss cascade science -- deliberately no UTAC/CREP/AFET bridge. GenesisAeon P99.
Live von GitHub, Stand 11.09.2026, 20:50
Laienverständliche Fassung (Deutsch)
Paket-DOI
Keine eigene Paket-DOI in CITATION.cff oder .zenodo.json.
Quellen-DOIs
In der CITATION.cff dieses Pakets sind keine Paper-DOIs hinterlegt.
Literatur je Paket
Global-scale hydrological response to future glacier mass loss
Nature Climate Change, 2018
Glacier shrinkage driving global changes in downstream systems
PNAS, 2017
Ecological responses to experimental glacier-runoff reduction in alpine rivers
Nature Communications, 2016
Loss of meltwater from glaciers and snowpack may increase synchrony of river habitats and resources in mountain watersheds
Ecology, 2025
Spatial Patterns of Glacier-Wetland Hydrological Connectivity in the Rapidly Deglaciating Peruvian Andes
Earth's Future, 2026
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, verified science + NO UTAC/CREP/AFET bridge
What this is
- Peak water (Huss & Hock 2018, Nature Climate Change): a real,
- quantitatively modeled phenomenon in glacier hydrology. As glaciers
- lose mass, basin-scale glacier runoff first rises, then reaches a
- maximum, then declines. The decline phase is what removes the
- hydrological buffer that dampened summer/drought low-water periods —
- exactly the mechanism described in the GenesisAeon-Diskurs dialogue
- this package is built from.
- A real, quantified downstream ecological response (Cauvy-Fraunie
- et al. 2016, Nature Communications): an experimental 31% flow
- reduction produced a 6.5x (±1.8) increase in benthic fauna density
- within two weeks, and a 33-site field survey found an abrupt shift in
- algal/herbivore biomass below 11% catchment glacier cover. Recovery to
- pre-perturbation community composition took 14–16 months.
- A real synthesis review (Milner et al. 2017, PNAS) of how
- glacier shrinkage propagates into downstream hydrology, sediment
- transport, biogeochemistry and biota.
- **A
…
README
Technische Dokumentation (Englisch)
glacier-buffer-utac
GenesisAeon Package 99 — real glacial hydrological buffer ("peak water") and downstream buffer-loss cascade science. 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.
What's real here
- Huss & Hock (2018, Nature Climate Change): "peak water" — glacier
- runoff rises, peaks, then declines as ice mass shrinks; the decline
- removes a real hydrological buffer against summer/drought low water.
- Cauvy-Fraunie et al. (2016, Nature Communications): experimental
- 31% flow reduction → 6.5x (±1.8) benthic fauna density increase within
- 2 weeks; 14–16 months to recover; an 11% glacier-cover threshold for
- abrupt algal/herbivore biomass shifts (33-site field survey).
- Milner et al. (2017, PNAS): synthesis review of glacier shrinkage
- propagating into downstream hydrology, sediment and biogeochemistry.
- Dunkle et al. (2025, Ecology): loss of meltwater desynchronizes
- previously asynchronous glacier-/snow-/rain-fed stream resource
- dynamics.
- Xuan et al. (2026, Earth's Future): wetland glacier-meltwater
- dependence is spatially heterogeneous — strong near the glacier
- margin, fading with distance.
- The full glacier → wetland → vegetation → fauna cascade is honestly
- represented as a literature-supported hypothesis network, not a
- single measured causal chain — see DISCLAIMER.md.
Quickstart
bash pip install glacier-buffer-utac
```python from glacier_buffer_utac import ( ALL_CASCADE_STAGES, is_below_glacier_cover_threshold, buffer_sensitivity_multiplier, recovery_time_months_range, )
for stage in ALL_CASCADE_STAGES: print(stage.name, "--", stage.mechanism)
print(is_below_glacier_cover_threshold(8.0)) # True print(buffer_sensitivity_multiplier(0.3)) # 3.33... -- more sensitive as ice shrinks print(recovery_time_months_range()) # (14, 16) ```
Development
bash pip install -e ".[dev]" pre-commit install ruff check src tests mypy src pytest
Citation
See CITATION.cff and .zenodo.json.
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.
- P100Glacier Buffer Replacementglacier-buffer-replacement-utac
- P101Glacial Seismicityglacial-seismicity-utac
- P102Paraglacial Hazardparaglacial-hazard-utac
- P103Distributed Buffer Resiliencedistributed-buffer-resilience-utac
- P104Mountain Governance Adaptationmountain-governance-adaptation-utac
- P105Black Carbon Albedoblack-carbon-albedo-utac
- P106Freshwater Ecosystem Stressorsfreshwater-ecosystem-stressors-utac
- 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