Science Writer
frames the claim for a non-specialist audience.
Year-over-year shift in fire-active centroid latitude in Northern Hemisphere is poleward at rate > 0.3° lat/yr.
Boreal-region catastrophe models revise fire-loss frequency 2-3× by 2030. Reinsurance rate-on-line for subarctic regions widens 40-80 bps. Permafrost-bond and CO₂-storage insurance underwriting factorise tipping-point fire-carbon-release scenarios at 3-5× current baseline. Taiga-to-tundra transition becomes detectable in Landsat/Sentinel-2 NDVI time series at p<0.01 within five years.
The metric is approaching the SUPPORTS threshold. The council judges that the underlying signal is real but not yet decisive. Do not underwrite, price, or cite this hypothesis as supported. The catalogue version is FORMING/CONVERGING; downstream reliance is premature until the SUPPORTS line is crossed and the falsification path remains genuinely reachable under null.
Metric: Population-weighted centroid latitude of active fires in NH boreal zone (>50°N), 12-mo rolling
Now reading: 4.16 · Current weighted-mean fire latitude 4.16° (drift requires archived snapshots)
/api/fires
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/api/forestwatch
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Captain reads 2 Earth API endpoints together (/api/fires + /api/forestwatch). The hypothesis emerges only at their intersection — none of these streams alone reveals the pattern.
Annual centroid (lat-weighted by fire count) for NH boreal NASA FIRMS data. Linear regression on 5-yr window. Statistically significant positive slope confirms.
frames the claim for a non-specialist audience.
designs the formal experiment.
Synthesises 2 angles into the formal hypothesis, sets thresholds, schedules revisits when data lands.
Five independent claude-sonnet-4-6 calls, one per persona — Skeptic, Fact-Checker, Researcher, Compliance-Guard, Falsification-Auditor. Each writes its hardest objection from its own seat, paired with the methodological resolution it would accept. Run on the static catalogue spec Jun 3, 2026; a live council for any topic is at /try.
The northward drift of the fire-active centroid may be an artifact of differential fire suppression effort rather than genuine ecological migration. Canada's CIFFC and Russia's Federal Forestry Agency have systematically concentrated aerial suppression resources in the southern boreal (50–65°N) throughout the FIRMS record period, because proximity to infrastructure and timber values makes suppression cost-effective there. This preferential extinguishment removes fires from the lower-latitude portion of the centroid calculation before they accumulate detectable FIRMS hotspot counts, mechanically pulling the population-weighted mean poleward even if ignition frequency and climate-driven spread are stationary across the full latitudinal band.
Recompute the centroid using only fires in explicitly designated "no-attack" or "monitor-only" management zones, which receive negligible suppression regardless of latitude—these boundaries are published annually by CIFFC (Canadian Fire Management Zones shapefile) and the Russian Federal Forestry Agency (Zone B unmanaged forest polygons). Run a difference-in-differences regression with zone type (managed vs. unmanaged) as the treatment indicator and year as the running variable, using FRP-weighted burned area from the Global Fire Atlas (Andela et al. 2019, 0.25° grid) rather than hotspot count as the outcome. If the poleward centroid slope in unmanaged zones matches or exceeds the full-domain slope (β ≥ +0.3°/yr, p < 0.05), suppression artifact is ruled out; if the slope collapses to near zero in unmanaged zones while persisting only in managed ones, the centroid drift is a suppression-filtering artifact, not ecological signal.
The binding uncertainty is not instrument geolocation precision but the enormous inter-annual variability in boreal fire centroid latitude—driven by which regional complexes dominate a given fire season (Siberia, Northwest Territories, Alaska)—which produces a 1-sigma spread of roughly ±2–4° lat between calendar years. With a 5-year OLS window and that level of natural variability, the standard error on the estimated slope is approximately ±0.5–0.8° lat/yr, placing the 0.3°/yr SUPPORTS threshold squarely inside the 1-sigma noise band and indistinguishable from zero drift at any standard confidence level. Compounding this, MOD
The dominant uncontrolled confounder is systematic agricultural-waste burning at the southern margin of the study domain (50–60°N), concentrated in Russia, Kazakhstan, and Eastern Europe. Agricultural field-burning generates large numbers of NASA FIRMS detections at lower boreal latitudes, and any secular reduction in that activity — driven by Russia's 2015 open-burning regulatory amendments, post-Soviet land-use shifts, or drought-related harvest failures rather than by climate — mechanically pulls the fire-count-weighted centroid poleward. Because the methodology aggregates all active-fire detections without separating land-cover class, this land-management signal is aliased directly into the regression slope, biasing the estimated poleward drift upward and potentially generating a spuriously "significant" result even if natural forest fire centroids are stationary.
Restrict FIRMS detections to pixels classified as boreal needleleaf or mixed forest using the annual MCD12
The downstream predictions explicitly quantify reinsurance rate-on-line adjustments (40–80 bps) and catastrophe model revisions (2–3× fire-loss frequency), meaning premature citation of this hypothesis as confirmed could trigger violations of Actuarial Standard of Practice No. 38 (catastrophe modeling credibility) and NAIC's Catastrophe Model Governance guidance, both of which require that models underpinning insurance pricing reflect scientifically validated, peer-reviewed inputs rather than provisional regression findings. If the unvalidated centroid-drift metric were embedded in an Insurance-Linked Securities prospectus or catastrophe-bond term sheet, SEC Rule 10b-5 would apply to any materially misleading statement about the scientific basis for loss frequency assumptions; simultaneously, IFRS S2 and the EU CSRD double-materiality framework would expose corporate filers who cite the finding in climate-risk disclosures to restatement and enforcement risk if the hypothesis later fails to sustain the +0.3°/yr threshold.
No actuarial, underwriting, or securities-disclosure use of this finding is permissible until the centroid drift exceeds +0.3° lat/yr for a full 24-consecutive-month window, the linear regression on the 5-year NASA FIRMS window yields a statistically significant positive slope (p < 0.05) independently reproduced against a second active-fire dataset (e.g., MODIS Collection 6 cross-validated against VIIRS S-NPP), and the methodology is published in a peer-reviewed journal or formally adopted by an IPCC Working Group I or analogous authoritative body. All interim outputs from /api/fires and /api/forestwatch must carry an explicit disclaimer stating: "This metric has not crossed the pre-registered SUPPORTS threshold; it must not be cited as established science in actuarial filings, ILS prospectuses, IFRS S2 disclosures, or CSRD materiality assessments."
The interannual standard deviation of NH boreal fire centroid latitude, driven by ENSO, PDO, and blocking-pattern variability, is empirically on the order of ±1–3° per year — roughly 3–10× larger than the stated +0.3°/yr SUPPORTS threshold. Over the proposed 5-year regression window with annual data points, the standard error of the slope is approximately 0.6–1.4°/yr (σ/√Σ(xᵢ−x̄)²), meaning a well-calibrated null system routinely produces observed slopes of ±1°/yr or more by chance alone. Critically, the FALSIFIES condition is stated only as "stable or drifting equatorward" — no lower numerical bound is given — so any marginally positive slope generated purely by interannual noise escapes falsification entirely, making the hypothesis structurally one-sided and effectively unfalsifiable under realistic data variance.
Execute a 10,000-iteration Monte Carlo null model by block-bootstrap-resampling annual fire centroid latitudes from the full NASA FIRMS archive (2001–present) under a zero-trend assumption, and derive the empirical 2.5th–97.5th percentile slope distribution; set the SUPPORTS threshold at the 97.5th percentile of that null distribution (likely ≥ +0.8°/yr) and define a symmetric, quantitative FALSIFIES band as any sustained slope below the 2.5th percentile (likely ≤ −0.8°/yr). Additionally, residualize the centroid time series against ENSO (MEI) and PDO indices using a sensitivity sweep across ERA5, NCEP-CFSR, and MERRA-2 reanalysis fire-weather ensembles; if climate-mode variance explains more than 60% of the observed slope, the SUPPORTS and FALSIFIES bands must be recomputed on the residual series to prevent large-scale oscillations from masquerading as a structural poleward regime shift.
Unlike the static stress tests above (synthesised against the frozen catalogue spec), this is what a 3-voice council found in the most recent biweekly review. Refreshed on the 1st and 15th of each month at 09:00 UTC. Each voice runs one bounded web search via Anthropic's web_search_20260209 tool, cites what it finds, and recommends a verdict.
The verdict diverges from the curated catalogue status (converging) — the synthesis below explains why.
The council collectively finds the hypothesis directionally plausible but quantitatively unsupported: Allen et al. 2024 (Science Advances) and PNAS 2025 show NH boreal area-burned trends are statistically nonsignificant or regionally decreasing, directly undermining the >0.3°/yr centroid-drift threshold, while a newly documented VIIRS nighttime low-confidence suppression bias (2025-10) and NOAA-21 calibration step-change further compromise the reliability of the centroid metric itself. The hypothesis requires downward revision of its quantitative threshold and must account for regional heterogeneity, aerosol forcing, and instrument artefacts before it can be meaningfully evaluated.
Two peer-reviewed papers (Allen et al. 2024, Science Advances; PNAS 2025) directly challenge the hypothesis's core metric: area-burned trends in the NH boreal zone (>60°N) as a whole are statistically nonsignificant, and sub-regional trends are decreasing in boreal Asia and North America — making a sustained >0.3°/yr poleward centroid drift factually unsupported at the aggregate NH level. Additionally, aerosol mitigation and nonlinear BBE-climate feedbacks are identified as confounding drivers, suggesting the hypothesis as stated is too simple and requires revision to account for regional heterogeneity and non-GHG forcing pathways.
This Science Advances paper (Allen et al., 2024) reports that for the NH boreal regions as a whole (poleward of 60°N), the area-burned trend is statistically nonsignificant (~2.5%/yr), and that boreal North America and boreal Asia show decreasing area-burned trends — directly contesting the picture of a coherent, sustained poleward migration of the fire-active centroid. It also introduces aerosol mitigation as a dominant driver of future boreal fire increase, rivalling or exceeding GHG-driven warming as an alternative mechanism, meaning centroid shifts may reflect pollution-policy geography rather than a monotonic poleward climate signal.
This June 2025 PNAS study (CESM2 analysis, 1997–2023 GFED data) shows that observed zonal trends in black-carbon biomass burning emissions are highly variable across 15° latitudinal bands and driven by nonlinear aerosol–cloud feedbacks; boreal BBE increases have a net cooling effect on the Arctic. This complicates the hypothesis by showing that fire-centroid dynamics are modulated by aerosol-climate feedbacks that can suppress high-latitude fire activity in some periods, making a sustained >0.3°/yr poleward drift implausible as a simple linear trend.
This December 2024 PNAS paper finds that boreal forests are transitioning toward an open-canopy state (30–50% tree cover) driven primarily by warming-induced tree-cover loss, not fire-centroid migration. It offers an alternative structural explanation for observed high-latitude ecosystem change — time-lagged vegetation state transitions — that could produce the same poleward fire-signal pattern without requiring a consistent >0.3°/yr centroid drift rate.
Two independent instrument-level issues weaken confidence in the 0.3°/yr SUPPORTS threshold: (1) the newly documented VIIRS nighttime low-confidence suppression bias disproportionately affects high-latitude, low-FRP detections and could artificially shift the fire centroid poleward; and (2) the mid-record addition of NOAA-21 in January 2024 introduces a calibration step-change in detection density whose effect on population-weighted centroid latitude has not been formally assessed. Together these mean the instrument uncertainty budget is not well-characterised relative to the claimed threshold, and the 24-month SUPPORTS criterion cannot be evaluated with confidence until the VIIRS filtering anomaly is corrected and a sensor-homogenised time series is produced.
An undocumented algorithmic filtering step in the VIIRS active fire confidence classification suppresses all low-confidence nighttime detections globally, across all latitude bands and both Suomi-NPP and NOAA-20 satellites. This asymmetric suppression (~696,908 expected missing low-confidence nighttime detections per year) introduces a systematic, latitude-correlated bias into fire centroid computations: high-latitude boreal fires, which are disproportionately detected at oblique scan angles and low radiative power, may be selectively under-counted at night, potentially inflating any apparent poleward centroid drift. The SUPPORTS threshold of >+0.3°/yr could be partially artefactual until this filtering anomaly is characterised and corrected in the standard product.
Using 375 m VIIRS detections 2012–2023, this study maps circumpolar Arctic–boreal fires into seven pyroregions with distinct climate sensitivities. Boreal North America, eastern Siberia and northern tundra show the highest climate-driven fire sensitivity, which is consistent with a poleward migration signal; however, the study underscores that anthropogenic factors and regional heterogeneity strongly modulate fire number and size, meaning a single NH centroid latitude metric may aggregate structurally different pyroregions, reducing the precision of a 0.3°/yr threshold claim.
NASA FIRMS confirms that VIIRS NOAA-21 data only became available from 17 January 2024 onward, meaning the three-sensor VIIRS ensemble (Suomi-NPP, NOAA-20, NOAA-21) used for centroid calculations has a step-change in spatial coverage and detection density at that date; positional errors during spacecraft maneuvers or space-weather events can reach several kilometres, which at high latitudes translates to a non-trivial fraction of the 0.3°/yr threshold (~33 km/yr), raising uncertainty about whether sub-threshold centroid drifts are real or instrumental.
Recent literature strongly corroborates poleward biome migration as the structural driver (0.43° median shift over 35 years ≈ 0.012°/yr for tree cover, far below the hypothesis's 0.3°/yr fire-centroid threshold), and confirms intensifying Arctic fire feedbacks; however, the specific metric — a fire-active centroid drifting >0.3°/yr sustained over 24 months — lacks direct empirical validation in the retrieved papers, and the NH boreal fire trend at >60°N remains non-significant, suggesting the quantitative threshold in the hypothesis may need downward revision while the directional claim remains well-supported.
Using 36 years of calibrated satellite data (1985–2020), this study confirms a biome-wide poleward shift in boreal tree cover of 0.29° mean / 0.43° median latitude, with gains concentrated at 64–68°N and exceeding southern-margin losses — directly corroborating the structural precondition for poleward fire-regime migration.
Projects future NH boreal fire activity (>60°N) showing a non-significant increasing trend of ~2.5% yr⁻¹ poleward of 60°N, while finding aerosol mitigation amplifies fire increases more than GHG warming alone — partially supporting poleward intensification but complicating a simple centroid-drift signal.
Models a future with prescribed increases in boreal biomass burning events finding significant Arctic feedbacks (sea ice recovery peaking ~3M km² difference by 2030s), reinforcing the hypothesis that expanding high-latitude fire regimes have Earth-system-scale consequences consistent with the hypothesis's permafrost/carbon-release predictions.
Agent draft incorporating the 9 cited findings from the live council above. Not auto-merged — surfaces here for human review. To accept, open a PR editing site/src/_data/hypotheses.json with the revised fields below. To reject, ignore and the proposal will refresh on the next council run.
Allen et al. 2024 (Science Advances) and the PNAS 2025 CESM2/GFED study collectively show that aggregate NH boreal area-burned trends poleward of 60°N are statistically nonsignificant and regionally heterogeneous (decreasing in boreal Asia and North America), directly falsifying a coherent >0.3°/yr NH-wide centroid drift; the domain voice corroborates this, noting that satellite-confirmed biome-level poleward tree-cover migration proceeds at only ~0.012°/yr over 35 years. Simultaneously, the arXiv 2025-10 VIIRS low-confidence nighttime suppression finding and the NASA FIRMS NOAA-21 step-change (January 2024) reveal that the current metric's instrument uncertainty budget is uncharacterised relative to the 0.3°/yr threshold, and the Nature Geoscience 2024-09 pyroregion study shows that a single NH centroid aggregates structurally distinct fire regimes, masking the real signal. Together these findings require: (1) downward revision of the centroid-drift threshold to a level consistent with the literature's observed sub-0.1°/yr signals; (2) restriction of the metric to sensor-homogenised daytime-only VIIRS detections to eliminate the nighttime suppression artefact; (3) disaggregation into climate-sensitive pyroregions rather than a single NH aggregate; and (4) explicit acknowledgement that aerosol-forcing geography and nonlinear BBE feedbacks are co-drivers alongside GHG warming.
SUPPORTS threshold lowered from >0.3°/yr to >0.05°/yr and window extended from 24 to 36 months; metric restructured from a single NH population-weighted fire-count centroid to an FRP-weighted daytime-only centroid disaggregated across 3 climate-sensitive pyroregions with explicit NOAA-21 intercalibration requirement; FALSIFIES threshold made numerically specific (±0.02°/yr instrument-uncertainty band); claim geographic scope tightened from >50°N NH aggregate to the three pyroregions identified in Nature Geoscience 2024-09; predicts magnitudes moderated (reinsurance widening 25–55 bps vs. 40–80 bps; carbon-insurance multiplier 2–3× vs. 3–5×; NDVI detectability extended from 5 to 7 years) to reflect regional rather than NH-wide signal and aerosol co-forcing pathway.
Year-over-year shift in fire-active centroid latitude in Northern Hemisphere is poleward at rate > 0.3° lat/yr.
Year-over-year shift in fire-active centroid latitude in the climate-sensitive NH boreal pyroregions (boreal North America, eastern Siberia, northern tundra; >55°N) is poleward at a rate > 0.05° lat/yr when computed on a sensor-homogenised, daytime-only VIIRS active-fire time series.
Population-weighted centroid latitude of active fires in NH boreal zone (>50°N), 12-mo rolling
Area-weighted centroid latitude of active fires within the three highest-climate-sensitivity NH boreal pyroregions identified in the Nature Geoscience 2024-09 circumpolar study (boreal North America, eastern Siberia, northern tundra zone; bounded 55–75°N), computed from daytime-pass-only VIIRS detections (Suomi-NPP + NOAA-20 pre-January 2024; Suomi-NPP + NOAA-20 + NOAA-21 post-January 2024 with sensor-intercalibration correction applied), on a 12-month rolling basis. Centroid weighted by fire radiative power (FRP, MW) rather than raw fire count to reduce sensitivity to low-FRP detection artefacts. Baseline period: 2012–2023 VIIRS record, with NOAA-21 step-change corrected via retrospective cross-calibration against the two-sensor ensemble before inclusion.
Centroid drift > +0.3° lat/yr sustained 24 months
Centroid drift > +0.05° lat/yr sustained across 36 consecutive months in at least 2 of the 3 target pyroregions, with the linear regression slope statistically significant at p < 0.05 on the FRP-weighted daytime-only series after NOAA-21 intercalibration.
Centroid stable or drifting equatorward
Centroid stable (slope within ±0.02° lat/yr, i.e., within instrument-positional uncertainty of ~2 km/yr for VIIRS at high latitudes) or drifting equatorward across the 36-month window in 2 or more of the 3 target pyroregions, sustained at p > 0.10 under the null of zero trend.
Boreal-region catastrophe models revise fire-loss frequency 2-3× by 2030. Reinsurance rate-on-line for subarctic regions widens 40-80 bps. Permafrost-bond and CO₂-storage insurance underwriting factorise tipping-point fire-carbon-release scenarios at 3-5× current baseline. Taiga-to-tundra transition becomes detectable in Landsat/Sentinel-2 NDVI time series at p<0.01 within five years.
If the SUPPORTS threshold is crossed: (1) pyroregion-specific catastrophe models for boreal North America, eastern Siberia, and northern tundra revise fire-loss return periods by 1.5–2.5× by 2035, consistent with the aerosol-mitigation amplification pathway identified in Allen et al. 2024 rather than a simple GHG-monotonic scenario; (2) reinsurance rate-on-line for subarctic property and infrastructure widens 25–55 bps, reflecting regional rather than NH-wide fire-regime repricing; (3) permafrost-bond and CO₂-storage insurance underwriting incorporates tipping-point fire-carbon-release scenarios at 2–3× current baseline, consistent with Arctic feedback magnitudes modelled in the PNAS 2025 CESM2 study; (4) taiga-to-open-canopy transition (consistent with the PNAS 2024-12 boreal open-state finding) becomes detectable in Landsat/Sentinel-2 NDVI time series at p < 0.05 within seven years in the two most climate-sensitive pyroregions.
This Science Advances paper (Allen et al., 2024) reports that for the NH boreal regions as a whole (poleward of 60°N), the area-burned trend is statistically nonsignificant (~2.5%/yr), and that boreal North America and boreal Asia show decreasing area-burned trends — directly contesting the picture of a coherent, sustained poleward migration of the fire-active centroid. It also introduces aerosol mitigation as a dominant driver of future boreal fire increase, rivalling or exceeding GHG-driven warming as an alternative mechanism, meaning centroid shifts may reflect pollution-policy geography rather than a monotonic poleward climate signal.
This June 2025 PNAS study (CESM2 analysis, 1997–2023 GFED data) shows that observed zonal trends in black-carbon biomass burning emissions are highly variable across 15° latitudinal bands and driven by nonlinear aerosol–cloud feedbacks; boreal BBE increases have a net cooling effect on the Arctic. This complicates the hypothesis by showing that fire-centroid dynamics are modulated by aerosol-climate feedbacks that can suppress high-latitude fire activity in some periods, making a sustained >0.3°/yr poleward drift implausible as a simple linear trend.
This December 2024 PNAS paper finds that boreal forests are transitioning toward an open-canopy state (30–50% tree cover) driven primarily by warming-induced tree-cover loss, not fire-centroid migration. It offers an alternative structural explanation for observed high-latitude ecosystem change — time-lagged vegetation state transitions — that could produce the same poleward fire-signal pattern without requiring a consistent >0.3°/yr centroid drift rate.
An undocumented algorithmic filtering step in the VIIRS active fire confidence classification suppresses all low-confidence nighttime detections globally, across all latitude bands and both Suomi-NPP and NOAA-20 satellites. This asymmetric suppression (~696,908 expected missing low-confidence nighttime detections per year) introduces a systematic, latitude-correlated bias into fire centroid computations: high-latitude boreal fires, which are disproportionately detected at oblique scan angles and low radiative power, may be selectively under-counted at night, potentially inflating any apparent poleward centroid drift. The SUPPORTS threshold of >+0.3°/yr could be partially artefactual until this filtering anomaly is characterised and corrected in the standard product.
Using 375 m VIIRS detections 2012–2023, this study maps circumpolar Arctic–boreal fires into seven pyroregions with distinct climate sensitivities. Boreal North America, eastern Siberia and northern tundra show the highest climate-driven fire sensitivity, which is consistent with a poleward migration signal; however, the study underscores that anthropogenic factors and regional heterogeneity strongly modulate fire number and size, meaning a single NH centroid latitude metric may aggregate structurally different pyroregions, reducing the precision of a 0.3°/yr threshold claim.
NASA FIRMS confirms that VIIRS NOAA-21 data only became available from 17 January 2024 onward, meaning the three-sensor VIIRS ensemble (Suomi-NPP, NOAA-20, NOAA-21) used for centroid calculations has a step-change in spatial coverage and detection density at that date; positional errors during spacecraft maneuvers or space-weather events can reach several kilometres, which at high latitudes translates to a non-trivial fraction of the 0.3°/yr threshold (~33 km/yr), raising uncertainty about whether sub-threshold centroid drifts are real or instrumental.
Using 36 years of calibrated satellite data (1985–2020), this study confirms a biome-wide poleward shift in boreal tree cover of 0.29° mean / 0.43° median latitude, with gains concentrated at 64–68°N and exceeding southern-margin losses — directly corroborating the structural precondition for poleward fire-regime migration.
Projects future NH boreal fire activity (>60°N) showing a non-significant increasing trend of ~2.5% yr⁻¹ poleward of 60°N, while finding aerosol mitigation amplifies fire increases more than GHG warming alone — partially supporting poleward intensification but complicating a simple centroid-drift signal.
Models a future with prescribed increases in boreal biomass burning events finding significant Arctic feedbacks (sea ice recovery peaking ~3M km² difference by 2030s), reinforcing the hypothesis that expanding high-latitude fire regimes have Earth-system-scale consequences consistent with the hypothesis's permafrost/carbon-release predictions.
This is an original cross-correlation hypothesis. The pattern emerges only when 2 Earth API endpoints are read together; no single dataset or existing publication isolates the claim as stated here. Captain proposes it as a testable scientific question.
Captain Landseed. (May 30, 2026). Boreal fire regime is migrating poleward [Working hypothesis, converging, catalogue v6.3]. Landseed PBC. Retrieved Jun 6, 2026 from https://captain-landseed.pages.dev/h/fire-regime-migration/
@misc{captain_landseed_fire_regime_migration,
author = {Captain Landseed},
title = {Boreal fire regime is migrating poleward},
year = {May 30 2026},
howpublished = {Working hypothesis, status: converging, catalogue v6.3},
publisher = {Landseed PBC},
url = {https://captain-landseed.pages.dev/h/fire-regime-migration/},
note = {Module: biosphere; Originality: NOVEL; Accessed: Jun 6, 2026}
}
TY - GEN AU - Captain Landseed TI - Boreal fire regime is migrating poleward PY - May 30 2026 PB - Landseed PBC UR - https://captain-landseed.pages.dev/h/fire-regime-migration/ N1 - Working hypothesis (status: converging); catalogue v6.3; module: biosphere ER -
JSON snapshot with all hypotheses, archived council deliberations, current live-state, and the build-over-build activity log. SHA-256 manifest included. CC-BY-4.0.
Five personas deliberate in real time. Typically ~$0.08, 40-60 seconds. Three free runs, then bring-your-own Anthropic / OpenAI / Gemini.