feat(simulation): district moisture spatial gradient (T-1080)

moisture_q was a single body constant (derive_moisture_q took only &BodyParams →
80 for every one of 2048 ocean-world districts), so vegetation/terrain/ecotones
were uniform — "nothing to fuzz" (the T-1080 believability bug).

- district_profile.rs: derive_moisture_q is now a body ceiling (hydrosphere+atmosphere)
  × per-district gradient — latitude (equator wet → pole dry), elevation (orographic/
  rain-shadow), continentality (100 − ocean_fraction_q). Integer/D-010, no new plumbing
  (elev_q/ocean_fraction_q/latitude_deg already reach build_district_profile). Mirrors
  D-240's temperature model. Coefficients in ClimateConstants + climate_constants.toml
  [moisture_gradient] (provisional; Q-123 calibrates). Tuned so a wet body stays mostly
  green with drier patches and a frozen body clamps mostly barren. + gradient unit test.
- region_profile.rs: region-tier moisture gets the region-latitude gradient (elevation/
  continentality are district-scale).
- Propagates to precipitation_class / vegetation_class / morphology_zone (all read
  moisture_q). D-239 §2 amended. Believability golden regenerated.

Probe (Arbour @ yolo): moisture_q distinct 1 → 49 (spread 0 → 48); 5/7 → 6/7 criteria.
Edict (frozen): moisture 0..20 ×21 — gradient within its low ceiling. Remaining fail
(vegetation-present) is the metric dividing by all-sampled incl. water on a 2/3-ocean
world — a Q-123 calibration concern, not a climate defect.

clippy --all-targets -D warnings clean; 1580 lib tests + harnesses pass.

Co-Authored-By: Claude Opus 4.8 (1M context) <noreply@anthropic.com>

governance/decisions/architecture.md

@@ -1777,6 +1777,7 @@ Technical foundation decisions that constrain implementation: engine, client-ser
 - **Implementation note (T-1024, 2026-06-07):** §1 per-body `RIVER_THRESHOLD` is now a derived field (`derive_river_threshold`) on `RegionProfile`. §2 district temperature is a nullable `f32` on `RegionProfile` sampled from a per-region climate derivation (`derive_temperature_c`); moisture is a separate integer primitive (`derive_moisture_q`, 0–100). Both populate the `RegionProfile` carrier during the L4 cascade run. Climate inputs use a **hybrid strategy**: stellar luminosity and spectral class are sourced from the import pipeline (`bodies.axial_tilt_deg`, `star_systems.spectral_class`); greenhouse offsets and diurnal amplitudes are tunable at runtime via `server/data/climate_constants.toml` (source-canonical TOML, not hardcoded).
 - **Implementation note (T-1025/T-1027, 2026-06-08):** §6's frozen 17-zone `MorphologyZone` enum is realised in `server/src/simulation/generator.rs` (`repr(u8)`, discriminant-pinned). The §5 8-family gated classifier + §7 compatibility-matrix invariants live in `derive_morphology_zone` (`region_profile.rs`). **16 of the 17 zones are reachable at RegionProfile scale; `BraidedPlain` is the exception** — distinguishing it from `Delta` needs a lithology signal (§8 Gravel→braided) that `RegionProfile` does not carry, so `BraidedPlain` is **deferred to ChunkContext** sub-classification. The §7 compatibility invariant is enforced as a **classifier-gate-ordering** property (a build-time test that a single region cannot yield a forbidden pair), per §7's "build-time test" language; genuine cross-region sharp seams (cliff↔fjord, lithology faults) remain permitted. §2 climate-derived fields (`precipitation_class`, `glaciation_grade`, `vegetation_class`) all derive from the temperature(+moisture) primitive (T-1025).
 - **Amendment (T-1082, 2026-06-28):** §5's family set grows from **8 to 9** — a `WaterBody` generator family is added for the water zones **OpenOcean / Lake / TidalFlat**, which previously fell through to the dry-land `AlluvialPlain` fallback (the D-245 believability bug: oceans rendered as dry forested land — `water=Dry` + `Forest` on the sea). `WaterBody` lays `Water::Deep`/`Shallow` (a Shallow shoal band on the district-anchored coast line `coast_anchor_m`, Deep beyond; TidalFlat is all-Shallow), a seabed `TerrainMaterial` (`Rock` on steep districts / `Sand` on gentle / `Wetland` for tidal mud), `Vegetation::Barren`, the water surface at `elevation_m = 0` (the §8 mouths-at-sea-level convention), and seasonal `Ice` via `derive_cover` (frozen seas). This **refines §6**: open ocean / lake / tidal flat are still derived zone *labels*, but their *generator* is now `WaterBody`, not `AlluvialPlain` — so §6's "tidal flat … not [a] distinct generator famil[y]" is superseded for the dispatch of those three zones. `Wetland` stays a land zone on `AlluvialPlain` (a marsh — saturated ground, not open water). Lives in `server/src/atlas/voxel.rs` (`MorphologyFamily::WaterBody` + `generate_water_body`, dispatched by `zone_to_family`); verified by the T-1083 believability harness (water-renders-wet flips PASS for Arbour + Edict). The §5 8-family decision-tree classifier (`derive_morphology_zone`) is unchanged — this is a voxel-tier *generator* family, selected by zone, not a new RegionProfile classifier branch.
+- **Amendment (T-1080, 2026-06-28):** §2's **moisture** primitive is now a **body ceiling × per-district spatial gradient**, not a single body constant. The hydrosphere+atmosphere value (`derive_moisture_q`) is the *wettest* a district on the body can be; per-district **latitude** (equator wet → pole dry), **elevation** (orographic / rain-shadow), and **continentality** (`100 − ocean_fraction_q`, coast wet → interior dry) subtract from it. Integer (D-010); coefficients in `ClimateConstants` / `climate_constants.toml` `[moisture_gradient]` (provisional, Q-123 calibrates). This mirrors D-240's latitude-graded *temperature* model and fixes the T-1080 believability bug (`moisture_q = 80` for all 2 048 districts → uniform vegetation/terrain — "nothing to fuzz"). It **propagates**: `precipitation_class`, `vegetation_class`, and the `morphology_zone` Wetland gate all read `moisture_q`, so those diversify for free. Lives in `district_profile.rs::derive_moisture_q`; verified by the T-1083 believability harness (moisture-gradient flips PASS, `distinct` 1 → ~49 on Arbour). The body-scale ceiling keeps each world's character; the gradient varies it within.
 - **Cross-reference:** [D-227](#d-227) (derive-don't-store voxel model), [D-228](#d-228) (composite tile axes / cohesion / seasonal state), [D-210](#d-210) (temperature proxy — formalised), [D-203](#d-203) (BodyWorldState cache), [D-206](#d-206) (background analysis pass), [D-208](#d-208) (drainage / D8), [D-010](#d-010) (determinism), [D-234](#d-234) (street/footprint geometry — consumes morphology), [D-142](content.md#d-142) (zone types), [D-217](#d-217) (tile condition), [Q-102](../questions/architecture.md#q-102) (cohesion = the warp), [Q-103](../questions/architecture.md#q-103) (mutator schema — open), [Q-105](../questions/architecture.md#q-105) (seasonal/clock state — temperature/ElevationDelta forward contract)
 
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