recompute replayed the Kalman over stored rows at their own spacing while q stays tuned for the live 2 s cadence. Q scales with dt^3, so at the 30 s persist interval the process noise was 3375x too large and the filter tracked noise instead of smoothing: it wrote indoor temperature rates of +/-20 C/h into the history. This is the exact trap DESIGN.md section 2 documents for simulate.py, which does scale q, and I walked into it anyway. Now rescaled per step, because tiering means the stored cadence is not constant. Mean |rate| on the real board dropped to 2.73 C/h; what remains above 10 is the filter's warm-up transient in the first four samples, which is honest. Readout scene puts the actual numbers between the animations: temperature, humidity, sea-level pressure and the signed three hour forecast, each in its channel colour, scrolling. Text is drawn whole-pixel on purpose. Everything else here is sub-pixel and that is what makes it look good, but splitting a 3 px glyph across two columns halves its peak and smears it illegible. Crisp beats smooth when the thing has to be read. site.environment and site.enclosure record where the sensor lives and what has changed around it, with POST /api/environment to change them at runtime. This is not cosmetic: closing a door changes how strongly the sensor couples to outside, which is a regime change in the process the heads are fitting, and at lambda 0.9985 they carry about 55 hours of memory. Left alone they keep predicting the old room for two days. Page-Hinkley would notice eventually but needs matured forecasts to do it, which at the long horizons is the same two days. So the endpoint marks a discontinuity and queues a retrain.
Ashvale Station
An online machine learning suite for a Raspberry Pi Zero 2 W with a Sense HAT v2. It turns the original telemetry dashboard into a forecasting instrument: multi-horizon predictions with calibrated uncertainty, a verification scorecard that scores the model against persistence, drift detection that triggers its own retraining, and a human-in-the-loop labelling path.
Everything runs on the Pi. No cloud, no GPU, no PyTorch, no scikit-learn, no pandas. The learners are pure numpy and the whole process sits comfortably under 150 MB RSS.
python scripts/simulate.py --days 14 --wipe # seed synthetic history
python scripts/evaluate.py # walk-forward backtest
python run.py # serve on :8000
Why the design looks like this
A single point sensor on a windowsill is not a weather service, and pretending otherwise is the fastest way to build something that looks impressive and is useless. The honest inventory of what your hardware can actually observe:
| Signal | What it tells you | Useful range |
|---|---|---|
| Pressure and its tendency | Synoptic systems, and it passes through walls | Genuinely hours ahead |
| Temperature, humidity | The local micro-environment | Hours, strongly diurnal |
| Ambient light and colour | Cloudiness, occupancy, time of day | Now |
| IMU | Whether someone knocked the desk | Now |
So the suite is built around that reality. Short horizons lean on state estimation and learned dynamics. Long horizons lean on climatology plus a decaying anomaly, and are labelled an outlook rather than a forecast. Every claim gets scored against the "nothing changes" baseline, in public, on the dashboard.
The stack
sensors.py hardware + a physics-based simulator fallback
|
estimation.py self-heating compensation -> Kalman bank -> level + rate
|
storage.py SQLite, WAL, tiered downsampling (raw -> 5 min -> hourly)
|
features.py 33 features on a 5-minute grid, physics computed not learned
|
models/
rls.py recursive least squares + adaptive conformal intervals
nowcast.py 18 direct heads (3 targets x 6 horizons), Hedge-blended
climatology.py harmonic regression for the 7-day outlook
precip.py Zambretti prior + online logistic residual learner
anomaly.py Mahalanobis EWMA + Page-Hinkley drift + sensor health
|
station.py four async loops: sample / persist / train / verify
api.py, led.py, dashboard.py
Six decisions worth defending
1. Self-heating is a grey-box parameter, not a magic constant.
The HTS221 and LPS25HB sit millimetres above a SoC running 20 to 25 °C hotter than the
room. The usual fix is T = T_sensor - (T_cpu - T_sensor) / 1.5. That 1.5 depends on
your case, your orientation, your airflow, and your CPU load. Here it is a single RLS
parameter that you update from the dashboard by typing in a thermometer reading. In
testing it recovers a known coefficient of 0.62 from a prior of 0.30 in one sample,
and holds post-calibration bias to 0.012 °C.
2. Rates come from a Kalman filter, never a finite difference.
Pressure tendency is the single most informative variable you have, and the LPS25HB
noise floor makes a naive (p[t] - p[t-1])/dt pure noise. A constant-velocity Kalman
filter estimates level and rate jointly, in Joseph form so the covariance stays positive
semi-definite over months of continuous operation. The filtered dp/dt is what feeds
both Zambretti and the learned heads.
3. Direct multi-horizon heads, not one model iterated forward. Iterating a one-step model 288 times to reach 24 hours compounds its own bias into a beautifully smooth lie. Eighteen small direct heads cost about 150 kB total and each one is honest about its own horizon.
4. RLS with directional forgetting, not SGD.
A station produces 288 grid rows a day. Sample efficiency is not a nicety. RLS is the
exact minimiser of the exponentially weighted squared error at every step and converges
in far fewer samples. The covariance P gives free parameter uncertainty. The forgetting
factor (0.9985, about 11 hours of effective memory) handles seasonal adaptation without
any retraining schedule at all. Plain forgetting inflates P exponentially during quiet
nights when the regressor barely moves, so the trace is capped: this is the single most
common way a field RLS deployment detonates.
5. Adaptive conformal intervals, not Gaussian error bars. Split conformal assumes exchangeability. Weather is not exchangeable: a front arrives and yesterday's residual quantile becomes fiction. Adaptive conformal inference feeds realised coverage back into the working alpha, so the band widens after each miss and narrows after each hit. Measured coverage in the backtest below sits at 89 to 91% against a 90% target, across every target and horizon.
6. The ensemble is allowed to conclude that the model is useless. Each head blends persistence, climatology and the learned model with Hedge weights. At 15-minute pressure the weights land on 96% persistence, which is the correct answer, and the scorecard says so out loud. A forecasting system that cannot tell you when to switch it off is a marketing asset, not an instrument.
Measured performance
Walk-forward backtest, 14 days of synthetic history, 60/40 split, strictly no target
visible before its validity time. skill = 1 - MAE/MAE_persistence.
target lead MAE persist clim skill cover
temperature 15m 0.439 0.463 0.449 5.0% 90%
temperature 1h 0.707 0.981 0.840 28.0% 89%
temperature 3h 0.824 1.961 1.302 58.0% 91%
temperature 6h 0.770 3.094 1.619 75.1% 90%
temperature 12h 0.816 3.922 1.969 79.2% 90%
temperature 1d 0.834 1.630 1.683 48.9% 91%
humidity 3h 1.526 2.790 2.826 45.3% 90%
humidity 1d 2.370 14.506 14.523 83.7% 90%
pressure 15m 0.949 0.950 0.950 0.1% 90% <- persistence wins
pressure 3h 2.606 3.531 3.631 26.2% 89%
pressure 1d 3.389 8.638 8.650 60.8% 90%
These are numbers against a simulator, so read them as a check that the machinery is
sound rather than as a promise about your windowsill. Run scripts/evaluate.py again
after a fortnight of real data and believe those instead.
Install on the Pi
sudo apt update && sudo apt install -y python3-venv sense-hat
git clone <your-repo> ~/ashvale-ml && cd ~/ashvale-ml
python3 -m venv --system-site-packages .venv
source .venv/bin/activate
pip install -r requirements.txt
pip install sense-hat smbus2
cp systemd/ashvale.service /etc/systemd/system/ # edit User/paths first
sudo systemctl enable --now ashvale
--system-site-packages matters: sense-hat pulls in RTIMULib, which is installed
via apt and is a genuine ordeal to build inside a clean venv.
Without the hardware libraries the suite falls back to a simulated board automatically, so you can develop the whole thing on a laptop and deploy the same code unchanged.
Set your altitude in config.yaml. Sea-level pressure reduction is the one setting
people skip and then wonder why every rule-of-thumb forecast reads pessimistic. At 100 m
an uncorrected station pressure shifts the Zambretti number by roughly two categories,
permanently.
The dashboard
Five tabs, one viewport, no scrolling on desktop. Below 1024 px the constraint is released, because pinning five panels into a phone viewport produces unreadable eight-pixel type.
| Tab | Answers |
|---|---|
| Live | The week ahead, current readings, the forecast with its band, and conditions |
| History | What did it do, over any timeframe you ask for |
| Models and Calibration | Has the model earned its confidence, and the calibration inputs |
| Stats for Nerds | Every internal the estimator and the 18 learners are carrying |
| Methods | How the whole thing is wired, and how each stage fails |
Live carries the current readings, the observed-and-forecast chart with its 90% conformal band, and the precipitation panel together, so the question "what is it doing and what happens next" is answered without changing tab.
History
Presets from 6 hours to a year, plus an explicit from/to range picker. Aggregation happens in SQLite, not numpy: pulling 90 days of rows into Python to average them would cost more memory than the board has. The bucket auto-selects from the span and snaps to round durations, so 6 hours gives one-minute buckets and a year gives daily ones. Min and max travel alongside the mean and render as a shaded band, so an hourly view still shows that the hour spanned four degrees rather than implying a flat line.
Alongside: per-day minima and maxima in local time, all-time records with the timestamp each was set, and CSV export of any range (streamed as a generator, so a year of history never has to exist in memory at once).
Methods
Generated from methods.py and rendered against your live config, so it describes the
station you are running rather than the one shipped. Ten stages, each with what it
consumes, what it produces, why it is built that way, and how it fails. The failure mode
is the field that usually goes undocumented and the one you need at 2 a.m.
- Fan chart with the 90% conformal band drawn behind the observed line. As the model earns confidence the band visibly narrows, so model quality becomes a shape you can read from the doorway.
- Estimator internals, the signature panel: self-heating coefficient, novelty distance and drift pressure, ticking at 2 Hz. Most weather dashboards show numbers; this one shows the state estimator working.
- Conditions ahead: Zambretti class, rain probability, and the prior/learner/trust split so you can see how much the learned model is actually contributing.
- Two yes/no buttons. "Was it wet in the last hour?" Each press is a strong label worth ten proxy labels. Two seconds of your attention beats a week of heuristics.
- Calibration box. Type a thermometer reading, watch
kupdate. - Scorecard with skill against persistence, and coverage against the 90% target.
- Monitors: novelty, drift pressure, per-sensor health, ensemble weights.
LED matrix
The 8×8 stopped being a scrolling number. It cycles through glyphs readable across a room: a pressure-trend arrow coloured by Zambretti class and brightened by tendency magnitude, a rain-probability column bar, a 3-hour temperature-delta wedge, and a red pulse if a sensor faults or drift fires. Alerts pre-empt everything, because a six-second scroll is a six-second delay on the only frame that matters.
API
| Endpoint | Purpose |
|---|---|
GET /api/telemetry |
Live reading. Superset of the original payload, so existing clients keep working |
GET /api/stream |
SSE. One connection instead of a 2-second poll: 0.4% CPU instead of 4% |
GET /api/history/range?start=&end=&bucket= |
Any window, SQL-aggregated, auto bucket |
GET /api/history/daily?days= |
Per-day min, max and mean in local time |
GET /api/records |
All-time extremes, each with its timestamp |
GET /api/export.csv?start=&end= |
Streamed CSV export |
GET /api/storage |
Rows per resolution tier and database size |
GET /api/methods |
The pipeline description the Methods tab renders |
GET /api/history?hours=&max_points= |
Decimated history (legacy) |
GET /api/forecast?target= |
All horizons with conformal bands and ensemble weights |
GET /api/outlook |
Days 2 to 7, climatology plus decaying anomaly, caveat included |
GET /api/precipitation |
Zambretti class, rain probability, prior/learner split |
GET /api/anomaly |
Novelty, drift, per-sensor health, event log |
GET /api/models |
Per-head diagnostics, coverage, precip coefficients |
GET /api/scorecard |
Verification: MAE, skill, coverage, sample count |
POST /api/train |
Force a retrain |
POST /api/verify |
Force a scoring pass |
POST /api/label |
{"kind":"rain","value":1} strong ground truth |
POST /api/calibrate |
{"reference_c":19.4} or {"reset":true} |
GET /api/status |
Hardware, history span, drift, training log |
Tuning
| Symptom | Knob |
|---|---|
| Temperature reads consistently high | Calibrate from the dashboard, or raise sensor.cpu_heat_k |
| Readings look over-smoothed, lag real changes | Raise sensor.kalman_q_temp |
| Rates look noisy | Lower sensor.kalman_q_*, or raise kalman_r_* |
| Model adapts too slowly to a season change | Lower model.rls_forgetting toward 0.995 |
| Model is jumpy and forgets overnight | Raise it toward 0.9995 |
| Coverage sits well below 90% | Raise model.conformal_gamma so it corrects faster |
| Drift alarms constantly | Raise model.drift_lambda |
| Retrains eat the CPU | Raise model.train_period_s, lower max_pairs in NowcastEnsemble.fit |
A full retrain over 18 heads takes about 10 s on a modern x86 core and closer to 60 to 90 s on a Zero 2 W. It runs in a worker thread, so the sample loop, the API and the LED never stall while it happens.
Honest limitations
- Indoors, this forecasts your room, not the sky. Pressure is the exception: it
passes through walls, which is why the precipitation model runs on pressure and its
tendency rather than on your indoor humidity. Set
site.indoorstruthfully. - Days 2 to 7 are climatology, not a forecast. Labelled as such in the API response and on the dashboard. They will never catch an incoming Atlantic low, because your station physically cannot see one.
- Rain labels are the bottleneck. Without a gauge the proxy label is deliberately
conservative and abstains in the ambiguous middle. The learner earns trust in
proportion to strong labels:
trust = n / (n + 25). Press the buttons. - Annual harmonics stay switched off until 120 days of history exist. Fitting a 365-day sine to three weeks of data produces a magnificent extrapolation straight off the edge of the physical world.
- One uvicorn worker, deliberately. The station owns mutable model state; a second worker would give you two divergent forecasters sharing a socket.
Where to take it next
The obvious extensions, roughly in order of payoff per hour of work:
- A DS18B20 on a one-metre cable outside the window. It removes the indoor caveat entirely, costs about three pounds, and every model in here improves immediately.
- A tipping-bucket rain gauge on a GPIO. Real precipitation labels turn the logistic model from a Zambretti wrapper into something genuinely local.
- Pull METAR from a nearby airfield as a reference channel, and the compensator calibrates itself continuously instead of waiting for you to type a number.
- Swap the RLS head for an ensemble Kalman filter over the parameter vector if you want proper joint state-parameter estimation. You already have the machinery.