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geostatistics-interpolation — Claude Code skill: point interpolation

A skill that turns sparse point measurements into a continuous surface and ships an uncertainty map alongside it. Handy when values between stations, wells or soundings have to be estimated.

Install into Claude Code · Skills CLI (Vercel) All methods and platforms ↓
npx skills add muend/geoai-skills --skill geostatistics-interpolation -a claude-code
Open on GitHub

What geostatistics-interpolation does

The skill takes scattered point measurements and produces a continuous surface, with one condition attached: a prediction raster never travels alone. It picks a method to fit the situation — IDW for a quick look, ordinary kriging as the default working choice, universal or regression kriging when a trend or covariates are present, indicator kriging for categorical targets.

Exploration comes first. Duplicate coordinates get averaged or offset, because kriging matrices go singular otherwise. Skewed variables usually want a log or normal-score transform, and the back-transform has to be done properly. The variogram is treated as a modelling decision rather than an auto-fit: nugget, sill and range are interpreted in words, and directional variograms at 0/45/90/135° catch anisotropy. Distances in degrees give wrong kriging, so work happens in a projected CRS.

Validation is not optional here. Leave-one-out suits small samples; clustered sampling needs spatial block cross-validation as well, and kriging has to beat a plain baseline to justify itself. Deliverables include the prediction surface, the kriging standard deviation, a validation table and a mask over areas the data cannot support. Skip the variogram plot and the CRS check, and you get a convincing raster that misleads.

What it helps with

  • build a surface from sparse station or well samples
  • quantify prediction uncertainty, not just values
  • fit and explain variogram parameters
  • test the model with spatial cross-validation
  • mask extrapolation beyond the data hull

Example prompts for the agent

  • Interpolate the points in stations.csv with ordinary kriging and give me the standard deviation map
  • Estimate a variogram for this data, fit a model and explain nugget, sill and range
  • Compare IDW and kriging on these points with leave-one-out and tell me whether the extra complexity pays off

How to install geostatistics-interpolation

1Skills CLI (Vercel)

npx skills add muend/geoai-skills --skill geostatistics-interpolation -a claude-code

2Manually: put the files in place

~/.claude/skills/geostatistics-interpolation/SKILL.md

Copy the whole skill folder; for one project use .claude/skills/geostatistics-interpolation/

Step by step, with commands for each platform: How to install skills in Claude Code: five ways

Questions about geostatistics-interpolation

How do I install geostatistics-interpolation in Claude Code?

Run npx skills add muend/geoai-skills --skill geostatistics-interpolation -a claude-code, then confirm the file landed at ~/.claude/skills/geostatistics-interpolation/SKILL.md.

What does geostatistics-interpolation do?

It builds a continuous surface from scattered point measurements and pairs it with an uncertainty map. Variogram modelling, ordinary, universal and regression kriging, IDW and spatial cross-validation are all covered.

When is this skill the wrong tool?

Not for point-density heatmaps, zonal aggregation or raster resampling without value interpolation. Counting how many samples fall in a cell is a different job.

Source text

SKILL.md · MIT
---
name: geostatistics-interpolation
description: >-
  Turn scattered point measurements into continuous surfaces with quantified
  uncertainty: variogram modeling, ordinary/universal/regression kriging,
  IDW, and spatially honest cross-validation. Use when unobserved values must
  be estimated from sparse samples such as stations, wells, or soundings.
  Trigger on "interpolate", "kriging", "variogram", or "IDW"; a named
  interpolation method is sufficient even when the requested surface is
  described informally as a heatmap. Do not use for point-density heatmaps,
  zonal aggregation, or raster resampling without value interpolation.
license: MIT
metadata:
  author: Muhammed Enes Duran
---

# Geostatistics & Interpolation

Purpose: interpolation that reports what it doesn't know. The difference
between a professional product and a pretty raster is the uncertainty
surface and an honest cross-validation — both are non-optional here.

## Method selection

| Situation | Method |
|---|---|
| Dense, smooth phenomenon, quick look | IDW (report power parameter; test 1-3) |
| Physical phenomenon with spatial structure, need uncertainty | **Ordinary kriging** (default professional choice) |
| Clear trend (elevation gradient, coastal effect) | Universal kriging or regression kriging on covariates |
| Strong covariates available (DEM, land cover, distances) | Regression kriging / random-forest residual kriging |
| Categorical target | Indicator kriging |
| Honeycomb-free tessellation, no extrapolation wanted | Natural neighbor |

IDW is a reasonable baseline but has no error model and bullseyes around
extremes; say so when delivering IDW-only products.

## Exploratory phase (before any interpolation)

- Map the points with values; look for duplicates at identical coordinates
  (average or offset them — kriging matrices go singular otherwise).
- Histogram + skew: strongly skewed variables (rainfall, concentrations)
  usually want a log/normal-score transform; back-transform predictions
  properly (bias correction for lognormal kriging).
- Trend check: regress value on x, y, and candidate covariates; visible
  trend → universal/regression kriging path.
- Declustering if sampling is preferential (dense where values are high).

## Variogram discipline

The variogram is a MODELING decision, not an auto-fit output:

```python
import gstools as gs

bin_center, gamma = gs.vario_estimate((x, y), values, max_dist=dmax)  # dmax ≈ half extent
model = gs.Exponential(dim=2)
model.fit_variogram(bin_center, gamma, nugget=True)
print(model)   # report: nugget, sill, range — plus the fitted plot
```

- Max lag ≈ half the domain diameter; ≥30 pairs per bin.
- Check anisotropy with directional variograms (0/45/90/135°); geological
  and meteorological fields are often anisotropic — fit an anisotropic
  model rather than ignoring it.
- Interpret and report the parameters in words: nugget (measurement error +
  micro-scale variance), range (correlation distance), sill. A nugget near
  the sill means the data barely support interpolation — say that honestly.
- Never interpolate meaningfully beyond the variogram range from the
  nearest sample; mask or flag those cells.

## Kriging execution

```python
from pykrige.ok import OrdinaryKriging

ok = OrdinaryKriging(x, y, values, variogram_model="exponential",
                     variogram_parameters={"sill": s, "range": r, "nugget": n},
                     coordinates_type="euclidean")
z, ss = ok.execute("grid", gridx, gridy)   # ss = kriging VARIANCE — keep it!
```

- Work in a projected CRS (kriging distances in degrees are wrong except
  with explicitly geographic-aware models).
- Deliver TWO rasters: prediction AND kriging standard deviation
  (`np.sqrt(ss)`). The uncertainty map drives where to sample next and
  where not to trust the map.
- Search neighborhood: 16-32 nearest points typical; document it.

## Validation — leave-one-out and beyond

- **LOOCV** for small n: report ME (bias ≈ 0?), RMSE, and standardized
  RMSE (should be ≈ 1 if kriging variances are honest).
- For clustered samples, LOOCV flatters; also run spatial block CV
  (canonical recipe: `ml-experiment-standards` →
  `references/spatial-cv-protocol.md`) and report both.
- Scatter plot observed vs predicted with 1:1 line; map the CV residuals —
  spatially clustered residuals mean missing trend/covariate.
- Compare against the dumb baseline (global mean, IDW): kriging must earn
  its complexity.

## Reporting template

```
## Surface: <variable>
- n = <>, extent, CRS, transform applied: <log/none>
- Variogram: <model>, nugget/sill/range = <...>, anisotropy: <...>
- Method: <OK/UK/RK + covariates>
- LOOCV: ME <>, RMSE <>, RMSE_std <>; block-CV RMSE <>
- Uncertainty: kriging SD raster delivered; area beyond reliable range masked
```

## Pitfalls checklist

- Auto-fitted variogram accepted without looking at the plot.
- Kriging in EPSG:4326 over large extents.
- Prediction raster delivered without its variance/SD companion.
- Log-kriging back-transformed by naive `exp()` (bias!).
- Extrapolation far beyond the data hull presented at equal confidence.
- Duplicated station coordinates crashing or silently distorting the fit.

## Execution contract

- **Workflow:** inspect sampling and transform needs; model spatial dependence; fit candidate surfaces; validate against simple baselines; quantify uncertainty; mask unsupported extrapolation.
- **Decision rules:** choose IDW or trend methods for transparent baselines, kriging when a defensible variogram exists, and regression kriging when covariates improve blocked validation.
- **Verification protocol:** examine variogram diagnostics, LOOCV and spatial block-CV residuals, baseline uplift, uncertainty calibration, and behavior beyond the sample hull.
- **Failure modes:** withhold a confident surface when sampling is too sparse, dependence is absent, duplicates dominate, distance units are invalid, or uncertainty is uncalibrated.
- **Deliverables:** prediction surface, uncertainty surface, variogram and parameters, validation table, sampling-support mask, and method limitations.
- **Source freshness:** consult [the authoritative source registry](references/authoritative-sources.md) before relying on package APIs or defaults and record the checked date.

© Muhammed Enes Duran · MIT · muend/geoai-skills

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