feat(antarctica): ISMIP7 core-experiment pipeline with n=3 rheology and hist-branched CTRL - #4
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hoffmaao wants to merge 74 commits into
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feat(antarctica): ISMIP7 core-experiment pipeline with n=3 rheology and hist-branched CTRL#4hoffmaao wants to merge 74 commits into
hoffmaao wants to merge 74 commits into
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The whole antarctica/mesh/ dir was gitignored to keep the large .msh/.h5 files out of git, but that also hid the 155-byte boundary_ids*.json files that every solver script reads by default (ISMIP7_BNDIDS -> calving/other physical-line ids for the calving-terminus BC). A fresh clone hit a missing default path. Switch the rule to 'antarctica/mesh/*' + a '!boundary_ids*.json' negation (a negation under the dir form is a no-op) and commit the four files. These encode the gmsh $PhysicalNames split: addPhysicalGroup() auto-numbers the alternating Calving_/Other_ segments 1,2,3,... so odd=calving, even=other. Caveat: boundary_ids_buffered.json (55 ids) matches only the 4km/8km buffered meshes; the finer buffered meshes have 35 ids (use boundary_ids.json). The buffered sidecar is not yet per-mesh. Co-Authored-By: Claude Opus 4.8 (1M context) <noreply@anthropic.com>
…s generator - forcing.py: load_racmo_smb_climatology() reprojects RACMO ANT11 SMB to EPSG:3031 (rasterio) and samples to the mesh via icepack.interpolate - control/run.py: use RACMO climatology as the SMB baseline (acabf fallback), report area-weighted mean SMB - simulation.py: VAF/mass diagnostics use SI ice density (RHO_I_SI=917); the imported icepack rho_I is in MPa-m-yr units and was zeroing the output - mesh.py / mesh_antarctica.py: loaders take data_dir so they resolve antarctica/data instead of <project>/data - make_boundary_ids.py: generate boundary_ids.json from mesh $PhysicalNames Co-Authored-By: Claude Opus 4.8 <noreply@anthropic.com>
The boundary-id sidecar only matches the specific mesh it was generated from (its segment count is a deterministic function of the BedMachine input and SIMPLIFY_TOL/SUBSAMPLE). Committing a fixed sidecar silently mismatches any mesh built from different inputs. Instead, make_boundary_ids exposes an importable write_boundary_ids(), and mesh_antarctica.py calls it after writing each mesh so the sidecar always matches the local mesh. Co-Authored-By: Claude Opus 4.8 <noreply@anthropic.com>
…orcing Reconciles our local work with the upstream ocean-melt branch. Conflict resolutions: - simulation.py: keep upstream's ocean_melt mass sink and h_clamp=0; take upstream's _RHO_I_SI/362.5 for the VAF/mass diagnostic (same fix as ours), dropping our redundant RHO_I_SI/GT_PER_MM_SLE duplicates. - control/run.py: RACMO climatology SMB baseline (ours) + per-basin ocean-melt callback (theirs); union imports; construct atm lazily in the acabf fallback. - forcing.py: our load_racmo_smb_climatology alongside their Burgard melt parameterization (auto-merged). boundary_ids policy: sidecars are now generated locally to match the mesh (mesh_antarctica.py emits one), so .gitignore ignores the whole mesh dir and upstream's four committed (35-segment) sidecars are dropped — they matched no mesh reproducible from the repo. Co-Authored-By: Claude Opus 4.8 <noreply@anthropic.com>
Adds make_synthetic_ocean_callback: prescribes TF(draft) = clip(tf_max * |draft|/depth_ref, 0, tf_max) and runs it through the Burgard quadratic_mixed_slope melt with constant salinity and the default scalar K. Needs no ocean/meltMIP data, so it works without the Globus download. Opt-in via ISMIP7_SYNTHETIC_MELT=1 (tunable with ISMIP7_SYNTH_TF_MAX / ISMIP7_SYNTH_DEPTH_REF); the real per-basin K path remains the default and is unchanged. Uncalibrated development stopgap, not protocol forcing. Co-Authored-By: Claude Opus 4.8 <noreply@anthropic.com>
Debugging tooling for the diagnostic solver: - simulation.py: opt-in SNES/KSP convergence monitoring (ISMIP7_SNES_MONITOR), routed to a per-run file via ISMIP7_SNES_LOG (ascii:<file>) or stdout, so concurrent debug runs don't interleave. - control/run.py: --snes-monitor / --snes-log CLI flags that set those, plus a --restart <checkpoint.h5> option to resume a control run. - simulation.py: clamp the loaded thickness to h_clamp on restart, so a run never resumes below the floor (no-op for the default h_clamp=0). Co-Authored-By: Claude Opus 4.8 <noreply@anthropic.com>
- --tag (ISMIP7_RUN_TAG): suffix on experiment_name so concurrent/successive runs write distinct output files instead of overwriting each other. - --checkpoint-interval (ISMIP7_CHECKPOINT_INTERVAL): control how often thickness+velocity checkpoints are saved (e.g. frequent snapshots for debugging). Default 100, so existing behavior is unchanged. Co-Authored-By: Claude Opus 4.8 <noreply@anthropic.com>
Default to antarctica_64000_500_aniso.msh (the mesh behind inversion_icepack2_500.h5) instead of the 1 km aniso mesh, raise the memory gate to 128 GB for the ~7M-DOF MUMPS factorization, and mark the script executable. This is the configuration that produced inversion_icepack2_rc_500.h5.
ISMIP7_FRICTION=regularized_coulomb makes setup_model() drive the prognostic system from the inversion_icepack2_rc_<lc>.h5 MAP: - geometry (thickness/bed/surface) and velocity_obs are taken from the checkpoint itself, so the Weertman anchor C_w0 — and hence the meaning of the inverted theta — is reproduced exactly; a node-ordering check guards the dof copy (also protects the existing Budd path). - the diagnostic solves build_rc_residual on the LIVE prognostic (h, s): grounded gate, Coulomb cap c0*N, and driving stress all track the evolving geometry, so the grounding line migrates with exact-zero shelf drag and no thickness clamp anywhere (h_clamp_init defaults to 0 in RC mode; h_visc_floor=10 m handles the ice-free buffer). - composite alpha defaults to the inversion's 1e-2 in RC mode so the forward diagnostic is consistent with the MAP. - setup_model now reports the initial velocity misfit vs observations (the rc_500 checkpoint predates its final report, so this is where we learn how converged that MAP is). Verified at LC=32000 against the completed RC inversion: the forward reproduces the checkpoint's saved velocity to rel L2 = 3.2e-9, and a short dt=0.1 clamp-free prognostic runs cleanly.
The acabf-anomaly files are referenced to the ESM's 1960-1989 climatology, and no historical scenario exists in the local data tree — so the projection driver's anomaly-only SMB was missing the entire climatological accumulation, while the CTRL driver's climatology lookup silently fell back to zero SMB. Fix both sides consistently: - ssp585 driver: force with the full acabf(t) field (smb_anomaly=False, new make_forcing_callback knob). Against a CTRL held at the 2015-2029 acabf mean, projection minus control is the forced signal relative to the 2015-centered climate with no anomaly re-referencing. - control driver: compute the reference climatology from full acabf pooled over historical + projection scenarios in an env-configurable window (default 2015-2029, the locally available years); raise instead of silently running a zero-SMB control. - both drivers pick up the calibrated per-basin K npz (falling back to the 2500 m calibration — 16 basin scalars remapped via the IMBIE2 8 km grid, mesh-independent); ssp585 default dt is now 0.1 per the May dt sweep. - launch_rc_ctrl_when_ready.sh: resource-gated launcher for the 500 m regularized-Coulomb CTRL2015 verification run (dt=0.1, 2015-2025, 24 ranks), logging under antarctica/results/logs/ so run logs survive reboots. End-to-end tested at LC=32000 through control/run.py with ISMIP7_FRICTION=regularized_coulomb.
Bring Dan's fixes into the antarctica branch: RACMO2.4p1 SMB climatology baseline (load_racmo_smb_climatology), SNES/KSP convergence monitoring with per-run log routing, restart/argparse tooling in the control driver, the synthetic depth-dependent melt stopgap (ISMIP7_SYNTHETIC_MELT=1), and the boundary-ids generator (make_boundary_ids.py; the static boundary_ids*.json leave tracking). control/run.py resolution composes both sides: RACMO stays the primary CTRL baseline (area-weighted mean report), the fallback is the pooled historical+projection full-acabf climatology (anomaly means are wrt 1960-1989 and are not a baseline), and a missing climatology is a hard error instead of a silent zero-SMB control (ISMIP7_ALLOW_ZERO_SMB=1 to override). The OI-climatology + per-basin calibrated K path remains the default ocean forcing.
SMB(t) = RACMO_clim + [aSMB(t) - mean(aSMB over the reference window)]: the acabf-anomaly is referenced to the ESM's 1960-1989 climatology, so re-referencing over the CTRL window (2015-2029 of it exists locally) removes that mismatch, and the RACMO baseline keeps projection and control on the same absolute SMB. Falls back to full acabf(t) when RACMO is absent. make_forcing_callback grows an smb_baseline parameter (per-node array added to the anomaly each step). Also: run_simulation nsteps now rounds instead of truncating (a 285-yr dt=0.1 run silently lost its final step), and the RC CTRL launcher verifies boundary_ids.json exists (untracked on this branch) and pins ISMIP7_BNDIDS for the run.
front, and an observation mask for the inversion Investigating the mass gain Dan saw. A new per-step mass audit in run_simulation attributes dM to SMB - melt - boundary outflux - calving and exposes any created mass; at 32 km it immediately caught two real leaks in the pre-existing scheme: - the -h*div(u*phi) volume term is non-conservative for DG0 (spurious h*div(u) mass at thickness jumps; +4700 Gt/yr at the test front). For piecewise constants the facet upwind terms alone are the finite-volume scheme, so the volume term is now dropped by default. - the L2 DG0->CG1 projection undershoots negative at steep fronts and the h floor then injects mass (+7600 Gt/yr step-1 at 32 km). Replaced by a lumped-mass projection (convex combination of adjacent cell values: bounded, no floor injection, integral-preserving). With both fixes the audited budget closes to machine precision (resid = 0.00, clamp = 0.0-0.2 Gt/yr). ISMIP7_LEGACY_TRANSPORT=1 restores the old scheme for comparison. ISMIP7_FIXED_FRONT=1 (now set by the RC CTRL launcher) removes ice that flows past the initially ice-free cells and tallies it as calving flux - without it a buffered mesh has no calving sink (~1300 Gt/yr in reality) and must gain mass. Only meaningful with a true-geometry initial state (RC mode). The inversion misfit now excludes nodes without velocity observations (MEaSUREs ERR > 0 defines coverage; icepack zero-fills NODATA, which read as "observed stationary" and prescribed friction where there is no constraint). Coverage gaps are small - 0.7% of grounded, 0.5% of floating area - so this is rigor, not the mass-gain culprit. obs_mask is saved in inversion checkpoints; ISMIP7_OBS_MASK=0 reverts.
get_thermal_forcing/get_salinity now load one (variable, year) slice out of its decadal chunk file into an in-memory nearest-neighbour RegularGridInterpolator over (z, y, x), cached across steps. The previous pointwise xarray .interp over the open_mfdataset dask graph cost ~10 minutes per step even at 5k mesh nodes; the new path reads a year in ~2 s and answers in ~1 ms, and is verified bit-identical to an xarray nearest-neighbour reference over 2000 random points and drafts. Nearest-neighbour also matches the OI-climatology CTRL path and the per-basin K calibration. A 32 km SSP5-8.5 step now costs the same as a CTRL step (~10 s after warm start, was ~675 s). ISMIP7_K_SCALE multiplies the melt K in both the projection callback and the CTRL driver (the calibrated per-basin K integrates 689 vs 865 Gt/yr observed on the 2500 m mesh; 1.26 matches the observed total).
The front mask was derived from the run's starting h, so a restarted run (the CTRL -> projection chain) would re-mask cells that legitimately retreated mid-run inside the observed extent and forbid them from re-advancing. setup_model now exposes the t=0 BedMachine/inversion thickness as ctx["H_init"] (restart_from does not overwrite it) and run_simulation builds the mask from that. Cold-start behavior is unchanged (verified identical at 32 km).
Local working-notes patterns belong in each clone's .git/info/exclude rather than the shared .gitignore, and the README's writeup pointer now names only the tracked document.
All ESM-forced core experiments (historical 1/2, SSP projections 3-8) are the same run with different (esm, scenario, period), so the nine drivers are now thin shims over experiment.run_core_experiment. That puts every fix from this week's work in force for the whole matrix at once: RACMO baseline + aSMB re-referenced over one shared pool (historical + ISMIP7_CLIM_SCENARIO, 2000-2029) so all cores and the CTRL share a single baseline and the 2014/2015 historical->projection handoff is seamless; calibrated per-basin K with the 2500 m fallback; dt=0.1; hard fast-failure (seconds, before the expensive model setup) when the forcing tree for an (ESM, scenario) is not downloaded, instead of silently running anomaly-only/zero-SMB. OCX (core 11) is rebuilt as a genuinely observation-forced run: RACMO actual-year SMB (1979-2023) + constant OI-climatology ocean with per-basin K — runnable entirely from local data. The OI-climatology ocean callback moves from control/run.py into icepack2_tools.forcing (shared by CTRL and OCX). Verified at 32 km: the ssp585 shim reproduces the standalone driver's results exactly; OCX runs with a closed mass budget; missing-data drivers (historical, ssp370) fail in ~7 s with the download hint. Co-authored work retained from prior drivers; fracture masks are loaded when present but still not applied to the thickness update (open protocol item).
Gate log, run log, and lockfile move from /tmp (wiped on reboot — the Jun 20 rc_500 inversion log was lost that way) to the repo results tree, tagged by resolution so a 2500 m and a 500 m gate can coexist.
The AIS_ocean/share_with_modellers tree is gone; data now lives under CMIP6_test_protocol/AIS mirroring the runtime layout, so downloads land directly in ISMIP7/AIS/ (no rename step, closing the README caveat). Auth is now headless-first: the script's own refresh-token cache, then the globus CLI token store (~/.globus/cli/storage.db keeps a long-lived transfer refresh token + the per-user confidential client), then an interactive login that now requests refresh tokens so it is one-time. The destination endpoint defaults to the Globus Connect Personal id registered on the machine. Transfers verify checksums. Manifest updated to what the share actually carries today: the SDBN1 1960-1989 long-term means (the exact reference climatology of the acabf-anomaly files), ocean ct/sa climatology+bias, the newer 06_nov OI climatology (1972-2024), the ISMIP7 obs kit, IMBIE v3, grid, and topography. NOT yet published upstream: historical yearly forcing, processed ssp126/ssp370, all of MRI-ESM2-0 — and the processed ssp585 tree we hold locally is no longer on the share (treat it as irreplaceable). Co-existing raw CMIP output lives in ../CMIPraw for when processing becomes necessary.
- build_oi_climatology_interpolators grows ISMIP7_OI_VERSION (default 30_sep, matching the per-basin K calibration; 06_nov selects the reorganized share's 1972-2024 re-release). The 06_nov so/thetao files currently ship the tf field by mistake (upstream packaging bug, reported) - the reader refuses them with an explanatory error instead of silently melting with TF-as-salinity. - load_K_per_basin falls back to the IMBIE v3 basin file when the calibration-era v2 is absent (verified identical basinNumber field, so the calibrated per-basin K remains valid with either). - scripts/preflight.py: five-second per-core readiness table checking every input each experiment needs (mesh, MAP, boundary ids, K, RACMO, OI climatology, atmosphere/ocean coverage over the run period), honoring the same env knobs as the runs. Current verdict: cores 7, 9, 11 READY (core 10 = core 9 while RACMO is the baseline); 1-6, 8 blocked on unpublished upstream forcing.
Re-walked the whole GHub tree to diagnose what climate forcing is pullable. The collection is mid-reorganization: CMIPraw is now gone entirely, AIS/MRI-ESM2-0 does not exist, and AIS/CESM2-WACCM holds only climatologies + bias ingredients (no scenario dirs, no per-year forcing). Everything still pullable is already mirrored locally, so the downloader is a no-op. The processed CESM2-WACCM/ssp585 forcing we run from (133 GB) is no longer on the share — flag the local copy as irreplaceable.
The 500 m RC CTRL crashed in setup_model's initial n=1->4 continuation (DIVERGED_MAX_IT): a fine mesh + a rough mid-optimization MAP outruns Newton across the 5-step ramp, and unlike the timestep loop the initial solve had no retry. Now it restores the initial guess and re-ramps with 2x then 4x steps on divergence (ISMIP7_CONTINUATION_STEPS, default 8), and reports the step count that worked. 32 km reproduces the identical initial misfit and VAF/mass through the new path (no regression).
On the 500 m mesh each diagnostic solve is costly, so seed the adaptive continuation finer (16) rather than failing at 8 and re-ramping.
Diagnosis of the 500 m CTRL divergence: the rc_500 MAP (a 20-iter mid-optimization checkpoint) carries ~700 theta/phi nodes with |.| up to 23, i.e. exp() coefficients ~1e10 that are local singularities the SNES cannot solve through — not a step-size issue. A converged MAP is O(1) everywhere (rc_32000 maxes at 1.64). setup_model now clips theta/phi to |.|<=ISMIP7_MAP_CLIP (default 6) and logs the count, removing the pathology (0.1% of nodes) without touching real structure. No-op for converged MAPs. Pairs with the adaptive continuation to unblock the 500 m cold start pending a proper re-inversion.
Adds a minimum-yield shelf-drag knob to the RC forward and records the multi-step instability diagnosis. The RC diagnostic velocity blows up ~2x/step in prognostic use (global, hypersensitive to sub-percent geometry change) — confirmed independent of transport scheme (legacy and conservative both blow up), independent of the fixed calving front (on/off identical), and NOT curable by shelf drag (tested up to 50 kPa, already enough to defeat RC's purpose). Budd ran stably for 10-20 steps in May, so this is RC-specific: exact-zero shelf drag + composite viscosity leaves the mixed diagnostic system near-singular as h evolves. The knob and MAP clip / adaptive continuation stay as robustness options; the forward prognostic needs Budd (proven stable) or a monolithic implicit coupling.
Following the pivot away from the prognostically-unstable RC forward: a resource-gated 2500 m Budd CTRL2015 validation run with the full conservation pipeline (RACMO SMB, OI ocean + per-basin K, conservative transport, fixed front, h_clamp_init=0, dt=0.1). Also confirms the Budd + fixed-front + h_clamp_init=0 config (new since May, which used h_clamp_init=10); a non-converging run self-terminates in ~10 steps so gating is safe. The rc_ctrl launcher is superseded for forward use.
The 1873 hard eras are front-cell-emptying EVENTS in sequence: the rescue ladder alone fails them at dt=0.1, but a dt=0.025 approach from the 1870 checkpoint crossed the 1873.3 event with four consecutive trust-region+limiter recoveries (then walled at the next event) - small geometry increments let Newton track the branch through each event. run_simulation's step is now transport-first (advance with the velocity solved AT the current geometry, then solve at the new geometry - the same (G, u) sequence as before, with the bonus that checkpoints store a mutually consistent (h, u) pair). A step whose post-advance solve exhausts the rescue ladder rewinds ITS OWN advance (h_dg/z entry buffers) and retries it as dt/4 then dt/16 subcycles with full rescue solves between substeps (ISMIP7_SUBCYCLES, default 1,4,16). Budget tallies (outflux/calving/clamp/limit) accumulate over substeps into the step's row, so the audit residual still closes exactly. Validated: the 2-yr balanced CTRL is unchanged (flat VAF, resid 0.0, ON TRACK, no rescue fires). Historical cores rerun next; their reports record how the 1873+ era sequence resolves.
First core experiment of the matrix run end-to-end: full 1850-2014 window from the balanced init, 13 front-cell-emptying events crossed by the dt-subcycle rescue ladder. Century-scale behavior is sound: SMB 2520, shelf melt 1371, front discharge 1050 Gt/yr means; dM/dt -314 Gt/yr; dVAF/dt -0.5 mm SLE/yr; budget residual <= 0.1 Gt/yr over 1640 steps. The single audit FAIL is the runaway detector's absolute-peak clause on an isolated one-step discharge spike during an emptying event (tallied, budget closed - a different signature from the sustained exponential growth the clause was built for; left as-is pending a ruling on refining the detector). Final state (t_yr=2014.0) is the restart base for the CESM2-WACCM projections (cores 3/5/7).
Second core of the matrix, on the newly mirrored MRI forcing. Completed in two legs: cold to 1876.9, then a warm resume whose x64 subcycle rung crossed the 1877 Amery front-emptying event (a single 553 s step) and cruised to 2014. Inter-ESM contrast established at 32 km: MRI gains ~+88 mm VAF over the window (stronger SMB) where CESM loses ~-87 mm. Budget residual closed throughout; same isolated-spike audit caveat as core 1. Final state (t_yr=2014.0) is the restart base for the MRI projections (cores 4/6/8).
First projection of the matrix to run its full window: 2015-2100 from the core-2 historical final, zero rescue events end to end (the MRI forcing never produces a front-emptying era at 32 km within this window). Budget residual closed throughout; audit table in-report. Ensemble overlay lands with the CTRL pair (cores 9/10).
Full window in two legs: cold to the 2069.7 front-emptying wall, then a warm resume that crossed it and ran out the window (17 rescued events total). By 2100 the CESM ssp370 forcing has driven the system into a surface-loss regime (net SMB -1987 Gt/yr, melt 5064 Gt/yr); VAF -265 mm vs 2015. Budget residual closed throughout.
108+ years of ssp585 from the historical final - the configuration that died at year 9 before the balanced-init/rescue work. 19 rescued events; a warm resume in the deep-collapse era (net SMB -6659, melt 13,818 Gt/yr, VAF -584 mm vs 2015) buys only +1.3 yr: front-emptying eras are continuous there and the split scheme saturates. Honest stop state saved; the monolithic coupling port owns the 2124->2300 stretch.
Three more full 2015-2300 projections: - Core 5 (ssp126 CESM): two legs across the 2056.4 wall. - Core 6 (ssp126 MRI): one clean leg, no rescues. - Core 8 (ssp585 MRI): 114 clean years to the 2129.0 wall, then a warm resume through the deep era to 2300 - where the CESM ssp585 twin (core 7) saturates at 2124.5, MRI's milder ocean lets the split scheme finish the window. Budget residual closed on all three; per-core reports carry audits and CTRL-differenced ensemble overlays.
- Core 9 (CTRL CESM): COMPLETE 2015-2300, the balanced control the projections difference against. - Core 10 (CTRL MRI): PARTIAL to 2040.5 (split-scheme-edge wall its physical twin core 9 crossed; RACMO baseline makes them near-identical, so CTRL behavior is demonstrated by core 9). - Core 11 (OCX): COMPLETE 1990-2025 obs-constrained; the real OCX forcing product (now on the share) is a follow-up swap.
Parallel line to antarctica running the composite viscous rheology at standard Glen n=3 instead of n=4 Goldsby-Kohlstedt. n=3 is the ISMIP6/ISMIP7 default and the more directly comparable configuration; the n=4 branch is left untouched. The n=4 assumption lived entirely in two env-var defaults, so this is a small, self-documenting change: - N_FLOW_DEFAULT 4.0 -> 3.0, A4_FACTOR_DEFAULT 10.0 -> 1.0 as module constants in simulation.py and inversion_icepack2.py. A0 = rate_factor(260 K) is already the n=3 fluidity, so the composite main term is plain Glen with no prefactor rescale (a4_factor=1); at n=4 the factor lifts A_3 to A_4 so A_4 tau_c^4 ~ A_3 tau_c^3 at tau_c. - map_n_tag() gives n=3 MAPs an _n3 filename tag (inversion_icepack2_budd_n3_<lc>.h5) so they coexist on disk with the untagged n=4 MAPs; empty at n=4 (backward compatible). The forward and its inversion must use the same ISMIP7_N_FLOW / ISMIP7_A4_FACTOR. - Launcher log/lock names n-tagged so n=3 and n=4 inversions don't collide on one machine. - COMPOSITE_RHEOLOGY.md + antarctica/N3_FRAMEWORK.md document the branch. Verified: syntax on all three scripts; map_n_tag() returns _n3 at the n=3 default, '' at n=4; launcher dry-run emits budd_inv_n3 names.
… stale n=4 comments
Adopt the mismip_time-dependent-da (Recinos/fenics_ice) inversion method to fix the n=3 theta/phi blow-up. The old n=3 MAP was ill-conditioned (theta/phi to +-36 in observed ice; forward gave misfit 3.5e5 vs the MAP's 1798, not forward-consistent) because the fluidity control phi=log(A/A0) sat on a CONSTANT baseline, so phi had to carry all the spatial fluidity structure and, without the n=4 a4x10 boost, exploded. The fix regularizes the DEVIATION from a physical prior mean, not the amplitude: - icepack2_tools/thermo_model.py: depth-averaged enthalpy (Stefan) model ported from the mismip thermo_model, adapted for Antarctica with a spatially-varying surface-temperature BC + an under-relaxed fixed-u Picard driver (compute_fluidity_prior). - icepack2_tools/prior.py: fenics_ice Whittle-Matern prior gamma*(theta^2 + L^2|grad theta|^2) - the theta^2 mass term (absent from the old gradient-only reg) removes the null space that let smooth large controls through. - forcing.load_mean_annual_surface_temperature: ISMIP7 tas climatology. - inversion: control phi=log(A/A_prior) on the thermomechanical prior mean (A4_base=A_prior, a Function; theta stays log(C/C_w0) on the balance anchor); WM reg at a physical gamma=1e4; A_prior saved in the MAP. - forward (simulation.py): loads A_prior from the MAP and reconstructs A=A_prior*exp(phi); restart checkpoints carry it. - antarctica/scripts/thermo_prior.py: standalone A_prior driver + figure. Validated at 32 km (30-iter inversion): thermo prior converges (T 221-272 K, A 1-884), controls drop to theta [-2.7, 5.7], phi [-6.1, 0.64] (was +-36), misfit descends 7.6e3->5.7e3, and the forward reproduces (setup_model initial misfit 6.7e3 vs the old 3.5e5; MAP clip now touches 2 nodes, was ~600). Full-convergence inversion next.
… MAP) At -n 16 on the tiny 32km mesh (~90 vertices/rank) MUMPS got fragile on the stiff thermomechanical A_prior and the FIRST adjoint solve failed. The adjoint/forward guards returned a large objective with a ZERO gradient, which L-BFGS-B read as convergence at iteration 0 - it quit and overwrote the good MAP with theta=phi=0 (misfit 1e11). Now a failure on the first evaluation (iteration_count==0, no successful gradient yet) raises a clear RuntimeError naming the likely cause (too many ranks for a small mesh) instead of silently producing garbage. Mid-run failures still backtrack as before. Fix: run small-mesh inversions at fewer ranks.
The full 32km n=3 Budd inversion with the thermomechanical fluidity prior + Whittle-Matern regularization converged (iter 534, misfit 4815, n=4-comparable). Controls are physical - theta p99abs 2.93 (max 7.8), phi p99abs 3.78 (max 5.9), vs the old p99 14-17 / max +-36 - and the forward REPRODUCES the inversion (setup_model initial misfit 6191 vs the old broken 3.5e5). Document the physical-prior method + run recipe in N3_FRAMEWORK.md (few ranks for small meshes; ISMIP7_MAP_CLIP=10 at n=3).
…rnings; dedupe anchor
The physical-prior inversion changed the fluidity baseline from the constant a4_factor*A0 to the thermomechanical A_prior stored in the MAP: - COMPOSITE_RHEOLOGY.md: composite spec now defines A = A_prior*exp(phi) with the legacy constant fallback noted, pointing to N3_FRAMEWORK.md (the owner of the prior method) instead of duplicating it. - antarctica/README.md \S4: the default inversion now also needs the \S2 ISMIP7 tas climatology (plus \S1 RACMO) for the thermo prior solve. - inversion_icepack2.py header: note the physical-prior controls and Whittle-Matern regularization with a pointer to N3_FRAMEWORK.md. - N3_FRAMEWORK.md: add ISMIP7_L_REG to the env list. Lint (no linter configured; py_compile + AST unused-import scan on the changed files): remove imports the change orphaned (grad, ds, dS in the inversion after the regularization moved to icepack2_tools/prior.py) plus pre-existing unused ones in the changed files.
experiment.py::run_core_experiment and projections/ocx.py now suffix the experiment name with ISMIP7_RUN_TAG (matching control/run.py's --tag), and the hist->projection restart lookup uses the tagged historical. This lets a parallel method line (e.g. the n=3 matrix, ISMIP7_RUN_TAG=n3) write distinct output files (hist_<esm>_n3_<lc>_final.h5, ssp585_<esm>_n3_..., ocx_n3_...) that coexist with the n=4 results instead of clobbering them, with the restart chain staying within one line.
The ISMIP6-ensemble comparison (compare_ismip6.py) now auto-selects the emission-scenario pool from the projection filename (ssp126->rcp26; ssp370/ssp585->SSP5-8.5+RCP8.5, best-effort from Seroussi 2020, --exps to override) and, when our trajectory is outside the envelope, prints the deviation direction plus a parametrization hint. Running it on the n=4 matrix exposed a methodology bug: the scenarios sat ABOVE the ISMIP6 envelope and were compressed (ssp126 +134 mm SLE at 2100 vs ensemble [-14,+50]; nearly as high as ssp585), a scenario-independent bias. Root cause: the CTRL cold-started from the 2015 inversion, so its frozen apparent-MB correction (a_ref) balanced to that geometry (net -95 Gt/yr), while the projections warm-start from the drifted historical endpoint and inherit its a_ref (-777 Gt/yr). a_ref is a constant per-step sink, so the -681 Gt/yr mismatch never cancels in proj-CTRL: it is a spurious -160 mm SLE trend over 2015-2100, larger than the whole +132 mm ssp126 signal. Fix: control/run.py branches the CTRL from hist_<esm>_<lc>_final.h5 (same t0 state -> identical frozen a_ref as the projections, respecting ISMIP7_RUN_TAG), cold-starting with a loud warning only when the historical endpoint is absent. Verified at 32 km: the hist-branched CTRL loads amb=-777 Gt/yr from the checkpoint, matching the projections exactly, so proj-CTRL now cancels the apparent-MB baseline and isolates the forced signal. Claude-Session: https://claude.ai/code/session_01UrjGwCeaeZv566CpbVhE15
…ef artifact The hist-branch CTRL change is kept (it is the protocol-correct same-state differencing: the control and projections must branch from the same historical endpoint so their shared relaxation drift cancels in proj-CTRL). But the justification in the previous commit was wrong. An isolation test at fixed n=4 rheology (same ssp126 projection, only the control baseline changed) shows: - cold-start CTRL (dVAF +8 mm over 2015-2100) -> proj-CTRL = +132 mm SLE - hist-branch CTRL (dVAF +37 mm) -> proj-CTRL = +161 mm SLE So the correct control makes the signal LARGER, not smaller: the projection's historical-endpoint relaxation only cancels when the control shares it. a_ref is a t=0 balancing correction (it zeroes the initial tendency), NOT a constant net sink, so the earlier "681 Gt/yr x 85 yr = -160 mm spurious trend, remove it and we fall into the ISMIP6 range" claim was invalid arithmetic and is retracted. The ISMIP6 overshoot is a real forced-response bias (melt/dynamics parametrization), not a differencing artifact; n=3 rheology roughly halves it (ssp126 +85 mm, still above the tight [-14,+50] envelope). Comment and the operator warning are corrected accordingly. Claude-Session: https://claude.ai/code/session_01UrjGwCeaeZv566CpbVhE15
…st-branch rationale
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Moving staging to the fork (hoffmaao/ismip7) while this work matures; will reopen or file a fresh PR when it is ready for upstream review. |
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Intent
Correct the rationale for the hist-branch CTRL change (comment + operator-warning text only; no behavior change). Context: an earlier commit (01696a7, already on PR #4) justified branching the CTRL from the historical endpoint by claiming the CTRL/projection apparent-MB (a_ref) mismatch of -95 vs -777 Gt/yr was a constant net sink that leaked a spurious ~160 mm SLE trend into proj-CTRL, and that removing it dropped us into the ISMIP6 envelope. That reasoning was WRONG: a_ref is a t=0 balancing correction that zeroes the initial thickness tendency, not a free net sink, so multiplying 681 Gt/yr by 85 years estimates nothing physical. An isolation test at fixed n=4 rheology (same ssp126 projection, only the control baseline swapped) shows the cold-start CTRL (its own drift +8 mm) gives proj-CTRL=+132 mm while the hist-branch CTRL (drift +37 mm) gives +161 mm - i.e. the CORRECT same-state control makes the signal LARGER, because the projection's historical-endpoint relaxation only cancels when the control shares it. The hist-branch change is KEPT (it is the protocol-correct same-state differencing the ISMIP6 ctrl_proj convention requires), but the ISMIP6 overshoot is now understood to be a real forced-response bias (melt/dynamics), not a differencing artifact; n=3 rheology roughly halves it (ssp126 +85 mm, still above the [-14,+50] envelope). This commit only rewrites the code comment and the cold-start warning message to state the correct rationale. This lands on antarctica-n3 / PR #4, which stays OPEN (Shapero merges to main later).
What Changed
icepack2_toolsgains forcing readers (ISMIP7 atmosphere/ocean, RACMO baseline), regridding, dual friction, and a thermal model;antarctica/scriptsadds the shared experiment runner, control/projection drivers for all core experiments (historical, ssp126/370/585 x 2 ESMs, CTRL, OCX), conservative thickness transport with mass-budget audits, rank-robust warm restarts, a solver rescue ladder with per-step dt-subcycling, and gated when-ready launchers with preflight checks.MATRIX_STATUS.md, an ISMIP6 ensemble comparison script with scenario-aware pool selection, an ISMIP6-track audit script, per-basin melt calibration, and a reworked Globus forcing mirror for the reorganized GHub share. The no-mistakes review pass surfaced 30 findings; the two documentation ones (stale hist-branch rationale in README/MATRIX_STATUS and the cores 9/10 cold-start CTRL provenance note) were fixed on-branch, and the remaining code-level findings are tracked as open items.Risk Assessment
✅ Low: The new delta is a four-line docs-only addition to MATRIX_STATUS.md that implements the approved provenance-note fix verbatim in spirit - factual, no retracted claim reintroduced, no code or behavior change - leaving nothing new to flag.
Testing
Proved the change is behavior-neutral via normalized-AST comparison of run.py before/after, then exercised the real CTRL driver in the Firedrake environment through both branch paths to capture the actual operator-facing messages, confirming the corrected same-state-differencing rationale replaces the retracted a_ref-sink claim in code, warning text, and docs; all checks passed and the worktree was left clean.
Evidence: CTRL operator messages (live transcript, both branch paths)
CASE A: no historical endpoint present -> cold-start WARNING path WARNING: no historical endpoint hist_cesm2_waccm_evharness_2500_final.h5; cold-starting from the inversion. The CTRL will start from a DIFFERENT geometry than the hist-branched projections, so projection-minus-CTRL will not cleanly isolate the forced response. Run the historical first, or pass --restart. CASE B: historical endpoint present -> hist-branch message path Branching CTRL from the historical endpoint (same initial state as the projections; shared drift cancels in proj-CTRL): hist_cesm2_waccm_evharness_2500_final.h5Evidence: Harness used to drive run.py:main() through the branch decision
Pipeline
Updates from git push no-mistakes
✅ **intent** - passed
✅ No issues found.
⏭️ **Rebase** - skipped
antarctica/scripts/control/run.py- merge conflict rebasing onto origin/mainantarctica/scripts/simulation.py- merge conflict rebasing onto origin/main🔧 **Review** - 30 issues found → auto-fixed (2) ✅
icepack2_tools/forcing.py:755- Flotation mask density mismatch: both melt callbacks compute haf = s - (b + (_RHO_WATER/_RHO_ICE)max(-b,0)) with freshwater _RHO_WATER=1000 while the model surface s is built with seawater flotation (rho_water=1024 per icepack2.constants and simulation.py), so genuinely floating ice with h between ~0.866depth and ~1.117*depth is classified grounded and receives zero ocean melt - exactly the near-grounding-line band where melt matters most. Same expression at forcing.py:755 (CTRL climatology callback) and forcing.py:824-826 (projection callback). Ask-user because fixing it changes scientific results and the per-basin K calibration may have partially compensated.antarctica/scripts/run_control.py:303- run_control.py's VAF and total-mass diagnostics multiply by rho_I imported from icepack2.constants (ice_density in icepack2's MPa-m-yr unit system, not 917 kg/m^3), so the reported mm SLE and Gt values are off by many orders of magnitude; simulation.py fixed the identical diagnostics with _RHO_I_SI=917.0 (lines 1299-1300) but this script was not updated.antarctica/scripts/simulation.py:357- u_c is set from a rank-LOCAL mean of observed speed (Function(Q).interpolate(...).dat.data_ro.mean() with no comm reduction, unlike the mesh.comm.allreduce used elsewhere in the file), so under mpiexec each rank builds a different sliding scale in K_base (line 391) and K_linear (line 406) and the assembled momentum operator is partition-dependent - results silently change with rank count, defeating the file's own rank-count-robust restart design. run_control.py:139 has the same rank-local mean.antarctica/scripts/inversion_icepack2.py:549- The inversion's solve-failure sentinel returns last_good_obj[0]*10, but last_good_obj stores the misfit-only J_val (line 556) while successful evaluations return total = J_val + reg_theta + reg_phi; with GAMMA defaults of 1e4 the regularization terms can dominate late in optimization, so a mid-run forward/adjoint failure can return an 'objective' lower than the current total with a zero gradient, which L-BFGS-B accepts and then terminates on projected-gradient 0, silently writing the MAP from the failed control point; the sentinel should store the last good TOTAL (both the forward guard at ~549 and the adjoint guard at ~574).icepack2_tools/forcing.py:37- smb_kgm2s_to_myr multiplies by a spurious _RHO_WATER/_RHO_ICE factor (kg/m^2/s * sec/yr / rho_ice already IS m/yr ice equivalent), inflating every ISMIP7 acabf SMB anomaly by ~9%, inconsistent with the RACMO loader which divides only by rho_ice; already tracked as open item 1 in MATRIX_STATUS.md as 'a real pending decision', so it needs the author's call.antarctica/scripts/run_control.py:1- run_control.py is a stale duplicate of the simulation.py pipeline that is scientifically inconsistent with the branch: it loads the untagged (legacy n=4) MAP but applies n=3 Glen, uses the non-conservative legacy transport with mass-injecting h_clamp=10 L2 projection, truncates nsteps with int(), and writes non-restartable checkpoints without t_yr; it is superseded by control/run.py and should be deleted or reduced to a shim before someone runs it as 'the control'.antarctica/scripts/simulation.py:1004- Checkpoints record friction and lc attrs (and restarts hard-fail on friction/a_ref mismatch) but not n_flow/a4_factor/m_slide, so resuming a checkpoint under a different ISMIP7_N_FLOW or ISMIP7_A4_FACTOR (e.g. resuming an n=4 antarctica-branch run on this n=3 branch, whose defaults differ) runs cleanly with silently wrong rheology - the same failure class the friction guard at line 284 was added to prevent.antarctica/scripts/inversion_icepack2.py:658- If the last scipy evaluation ended in a caught ConvergenceError, n_flow/m_slide are left at mid-continuation values (e.g. n=1.5), and the final slvr.solve() can converge at the wrong exponent without raising, so the 'Final misfit (masked)' and the velocity field written into the MAP checkpoint use the wrong rheology; reassign n_flow/m_slide to their target values before the final solve.antarctica/scripts/launch_rc_ctrl_when_ready.sh:99- Presence-vs-value env-var mismatch: launching with ISMIP7_FIXED_FRONT=0 (intending fixed-front OFF) still runs with fixed front because the script only skips its own export while the inherited variable remains set and simulation.py:828 tests presence (is not None); the non-1 branch needs unset ISMIP7_FIXED_FRONT. launch_rc_inversion_when_ready.sh:89 has the same bug with ISMIP7_NO_CALVING_TERMINUS=0 silently dropping the calving-terminus term (inversion_icepack2.py:155 tests presence).antarctica/scripts/experiment.py:121- The pre-run atmosphere check only verifies that SOME acabf years exist, not that they cover [t_start, t_end], and ISMIP7Atmosphere.get_field silently returns zeros for a missing year; in full-field fallback mode (smb_anomaly=False, taken whenever RACMO is absent) any coverage gap silently applies zero total SMB for the missing years, corrupting the mass balance with no warning. Ask-user because a zero-anomaly extension is partly intentional (the tracked 2014-to-2015 handoff gap relies on it), so the right fix is a coverage check against the run window rather than removing the zero fallback.antarctica/scripts/experiment.py:113- Projections have no auto-resume path (ISMIP7_AUTO_RESUME is only wired into control/run.py): rerunning a crashed multi-week projection without a manual ISMIP7_RESTART restarts from hist_*_final.h5 (t=2014), and run_simulation's CSV truncation (simulation.py:1041-1053) then deletes every timeseries row after 2014.5, silently discarding all of the crashed run's progress; wiring latest_checkpoint into experiment.py would mirror the control driver.icepack2_tools/regrid.py:56- ISMIP7Regridder computes its query-point bounding box from rank-local coordinates.dat.data_ro, but Firedrake VertexOnlyMesh defaults to redundant=True (points from rank 0 only), so under MPI the output grid is silently cropped to rank 0's partition bbox and the per-rank _query_shape/crop.reshape mismatches on other ranks - parallel regridded NetCDF output is wrong or crashes.icepack2_tools/forcing.py:288- ISMIP7Atmosphere.get_field silently returns zeros when a year's file is missing (_load_year returns None for any missing or misnamed path), and get_thermal_forcing has the same silent-zero fallback for a missing variable directory, so a renamed file or a run past the last available year quietly zeroes the forcing mid-run instead of failing; at minimum this should warn loudly once per missing year.antarctica/scripts/core_report.py:56- core_report.py always passes its --exps default "exp01..exp05" to compare_ismip6.py, so the scenario-aware auto-pool selection added in commit 01696a7 can never engage via core_report: an ssp126 report is graded against a mostly-RCP8.5 ensemble pool (only exp03 is RCP2.6) and the tracked 'outside envelope' verdicts (core05/06/08 reports) use the wrong comparison set; the default should be None so auto-selection runs, but this changes graded verdicts in tracked reports.antarctica/scripts/core_report.py:87- core_report.py conflates tool failure with a scientific result: any nonzero exit from compare_ismip6.py is written to the tracked report as 'outside envelope', but exit code 2 means usage/data error (missing ~/data/ismip6 archive, no year overlap), and audit rc==2 is similarly recorded as 'OFF TRACK' when the CSV merely lacks budget columns - a broken comparison gets permanently recorded as an out-of-envelope finding.antarctica/scripts/download_forcing.py:313- download_forcing.py skip-if-exists uses only local_path.exists() with no size/checksum comparison, so a file truncated by an interrupted transfer prints '[exists]', is excluded from the TransferData list, and the sync_level="checksum" repair never runs - the corrupt file silently feeds the pipeline indefinitely.antarctica/scripts/download_forcing.py:406- download_forcing.py scenario-group completeness is a bare file-count test (n_local < n_remote), so truncated local files or stale extras make the count match, the group is marked complete and skipped, and the checksum-sync transfer that would repair corruption is never submitted.antarctica/scripts/download_forcing.py:394- download_forcing.py treats a transient Globus auth/network error the same as absent data: list_remote_files returning [] makes _pick_version return None, reported as 'not on the share, skipped', and the run exits 0 - a whole (ESM, scenario) forcing set can be silently omitted from the mirror; a listing failure should be distinguished from an empty listing and exit nonzero.antarctica/README.md:268- Stale rationale: the README still describes the cold-start CTRL warning with the retracted claim ('its apparent-MB baseline will not match hist-branched projections (a spurious trend in proj-CTRL)'), contradicting the corrected rationale in commit 8f873a7 (a_ref is a t=0 balancing correction, not a net sink; the overshoot is a real forced-response bias) and no longer matching the actual warning text in control/run.py:208-214.antarctica/reports/MATRIX_STATUS.md:67- MATRIX_STATUS.md open item 1 (lines 62-67) still asserts the retracted causal claim as fact ('The matrix sitting above the ISMIP6 envelope ... turned out to be the CTRL cold-starting ... with a mismatched frozen apparent-MB baseline' and that cores 9/10 'carry the spurious trend'); per the corrected rationale the overshoot is a real forced-response bias and the hist-branch control makes proj-CTRL larger (+161 vs +132 mm), not smaller, so this status doc now misstates the project's own conclusion.antarctica/scripts/calibrate_melt.py:259- calibrate_melt.py reduces with rank-local numpy sums (node_kgyr[mask].sum(), lumped.sum()) despite the Firedrake/PETSc setup working under MPI, so running it under mpiexec silently produces wrong per-basin K and K* with normal-looking output; an nprocs>1 guard would prevent silent misuse.antarctica/scripts/launch_ctrl_when_ready.sh:1- The three when-ready launchers are ~85% line-for-line identical (noclobber lock protocol, traps, resource readers, gate loop, NTAG awk, logging) across ~315 lines and have already drifted (boundary_ids preflight in 2 of 3, MIN_FREE_CORES sanity warning in 1 of 3); consolidating the gate/lock machinery into one sourced library or a single parametrized launcher would make future fixes to the subtle lock/launch logic land in one place.antarctica/scripts/preflight.py:32- The n-tag MAP-filename rule now has at least 6 implementations that must stay bit-identical (inversion_icepack2.py:94, preflight.py:32, simulation.py:65, plus awk one-liners in all three launchers); a divergence silently makes a launcher gate on, or a forward load, a differently-named MAP - at minimum the three Python copies should import one shared helper.antarctica/scripts/launch_rc_inversion_when_ready.sh:72- Unlike both CTRL launchers, the inversion gate never pre-checks boundary_ids.json (required at inversion_icepack2.py:152), so the gate can wait hours for resources, fire, die in seconds on FileNotFoundError, and retain the lock as an 'already launched' marker that masks the failure.antarctica/scripts/simulation.py:790- Because t_restart unconditionally overrides the caller's t_start, hist-branched projections/CTRL integrate 2014->end (not the nominal 2015->end): year 2014 is replayed under the scenario forcing with a typically absent (zero-filled) 2014 anomaly - consistent between CTRL and projections so it cancels in differences, but it shifts absolute timeseries and duplicates a year already simulated in the historical (related to tracked open item 2 in MATRIX_STATUS.md).antarctica/scripts/projections/ocx.py:45- OCX always cold-starts (setup_model() with no restart argument and no --restart/auto-resume handling), so a reboot of the 1990-2025 run at dt=0.1 silently starts over and rewrites the timeseries CSV from scratch even though valid self-contained checkpoints exist on disk.icepack2_tools/coupled.py:139- coupled.py forcing_callback multiplies melt_rate_ice_equivalent() by 31556926 assuming the plume model returns m/s and copies it dof-for-dof into ctx["ocean_melt"] assuming identical dof ordering, but no plume module exists in the repo to verify either assumption - a m/yr-returning plume would be inflated ~3.2e7x and a submesh would scramble the copy.antarctica/scripts/compare_ismip6.py:169- compare_ismip6.py does not re-baseline 'ours' after clipping to the ensemble overlap window, so a run starting well before ~2015 carries its accumulated pre-window signal as a constant offset against ensemble members baselined at their own t0; harmless for the standard 2015-start runs but wrong for earlier-start inputs..gitignore:3- The bare 'data' pattern in .gitignore ignores any file or directory named 'data' at any depth, not just the repo-root data dir; '/data/' would scope it to the root.antarctica/scripts/control/run.py:179- Intent conformance verified: commit 8f873a7 touches only the comment block (control/run.py:179-196) and the two PETSc.Sys.Print operator messages; the hist-branch behavior, cold-start fallback, and restart validation are unchanged, and the corrected rationale (a_ref as t=0 balancing correction, +132 vs +161 mm isolation-test numbers, real forced-response bias, n=3 halving) is stated exactly as the intent requires; the retracted '681 Gt/yr / ~160 mm' arithmetic survives only inside this comment where it is explicitly quoted as retracted.🔧 Fix: Align README and MATRIX_STATUS with corrected hist-branch rationale
2 infos still open:
antarctica/reports/MATRIX_STATUS.md:63- The MATRIX_STATUS rewrite correctly retracts the wrong a_ref attribution, but it also dropped the still-true provenance note that cores 9/10 predate the hist-branch fix (their tracked CTRL records are cold-start controls, i.e. not the protocol-correct hist-branched control under the corrected rationale), and neither core09 nor core10 report records this itself - core09 even states 'This is the CTRL that the projections difference against'. Consider re-adding one sentence noting the archived core09/10 CTRLs are cold-start (mismatched-baseline) controls; ask-user since it is wording in the tracked scientific record.antarctica/reports/MATRIX_STATUS.md:63- Fix conformance verified: commit b6a3ccb changes only antarctica/README.md (cold-start warning description now matches the actual control/run.py:208-214 text - 'DIFFERENT geometry ... will not cleanly isolate the forced response' - and the branching sentence now attributes cancellation to shared relaxation drift plus the identical frozen a_ref) and MATRIX_STATUS.md open item 1 (restated as a real forced-response bias with the +161 vs +132 mm isolation test, a_ref as t=0 balancing correction, explicit retraction of the '~160 mm spurious a_ref trend' claim, and the n=3 halving to +85 mm vs the [-14,+50] envelope); no code or behavior was touched and no other files changed, matching both the user's fix instructions and the stated intent.🔧 Fix: Restore cores 9/10 cold-start CTRL provenance note
✅ Re-checked - no issues remain.
✅ **Test** - passed
✅ No issues found.
AST comparison ofantarctica/scripts/control/run.pyat 8f873a7^ vs 9b0e36b with string literals normalized - identical, proving the change is comments/messages onlygit show --stat b6a3ccb 9b0e36b- confirmed the follow-up commits touch only markdown (README, MATRIX_STATUS)Ranrun.py:main()end-to-end through the CTRL branch decision in the venv-firedrake-2026 environment (setup_model stubbed) for both paths: no historical endpoint (corrected cold-start WARNING printed) and fake historical endpoint present (corrected hist-branch message printed, hist-branch behavior kept)Repo-wide grep for retracted-rationale text (spurious,apparent-MB baseline,681,~160 mm) - only explicit retractions and one unrelated numerics comment remainCross-checked intent numbers (+8/+37 mm drift, +132/+161 mm proj-CTRL, n=3 +85 mm, [-14,+50] envelope) against run.py comment, README, and MATRIX_STATUSgit statusafter harness run - worktree clean, fake endpoint h5 removed✅ **Document** - passed
✅ No issues found.
✅ **Lint** - passed
✅ No issues found.
✅ **Push** - passed
✅ No issues found.