Fast univariate time series models that run in Pyodide
Project description
skaters
Fast univariate online time series models — in Python and JavaScript. Zero dependencies. Runs natively in the browser or in Pyodide.
Python and JavaScript, verified identical. The full library is ported to zero-dependency JavaScript and checked against the Python reference to 1e-6. Use it natively in the browser or via Pyodide — see the live demos.
Install
pip install skaters
Quick start
from skaters import skater
f = skater(k=3)
state = None
for y in observations:
dists, state = f(y, state)
dists[0].mean # point forecast
dists[0].std # uncertainty
dists[0].quantile(0.975) # 95th percentile
dists[0].logpdf(y) # log-likelihood
dists[0].cdf(y) # CDF at y
Every skater returns list[Dist] — a weighted Gaussian mixture for each horizon $h = 1, \ldots, k$. Point forecasts, uncertainty, density evaluation, and quantiles are all aspects of the same object.
Named search policies
Every named function builds a Bayesian ensemble over the same full candidate population. The names represent different search strategies — different priors, learning rates, and complexity penalties — not different models.
from skaters import holt, hosking, laplace, samuelson, wald, dantzig, kahneman, dirac, doob
f = holt(k=1) # expect trends (Holt 1957)
f = hosking(k=1) # expect long memory (Hosking 1981)
f = laplace(k=1) # no opinion — let the data decide
f = samuelson(k=1) # there's a drift, find it carefully (Samuelson 1965)
f = wald(k=1) # minimax caution (Wald)
f = dantzig(k=1) # optimize under compute constraints (Dantzig 1947)
f = kahneman(k=1) # think fast and slow (after timemachines, Cotton)
f = dirac(k=1) # bet on repetition — atoms on the lattice it revisits (after Paul Dirac)
f = doob(k=1) # martingale + learned volatility clock; feed levels (after Joseph Doob)
They are nmenomics in some instances.
| Policy | After | Prior | $\eta$ | $\lambda$ | Best for |
|---|---|---|---|---|---|
holt |
Holt 1957 | Differencing + Holt linear | 0.50 | 0.02 | Trending data |
hosking |
Hosking 1981 | Fractional differencing | 0.50 | 0.01 | Long memory |
laplace |
Laplace | Uniform | 0.80 | 0.005 | General purpose (recommended default) |
samuelson |
Samuelson 1965 | Drift + Holt | 0.40 | 0.01 | Persistent drift (GDP, prices) |
wald |
Wald | Depth 0 | 0.15 | 0.08 | Adversarial, non-stationary |
dantzig |
Dantzig 1947 | Adaptive search | 0.30 | 0.01 | Adaptive (grows pool online) |
kahneman |
timemachines | Fast tracker + slow residual scale | 0.50 | 0.01 | Fast signal, persistent noise |
dirac |
Paul Dirac | Lattice projection over skater |
— | — | Repeating / grid-quoted series (policy rates, posted prices) |
doob |
Joseph Doob | Martingale mean + learned volatility clock | — | — | Near-martingale levels (prices, indices) |
For example kahneman is a nod to thinking_fast_and_slow in
timemachines and puts a strong
prior on candidates with a fast process tracker outside and a slowly-varying
residual scale inside. Tune the bet with kahneman(k=1, strength=8); see examples/benchmark_kahneman.py.
dirac wraps skater in a lattice projection: it keeps a recency-weighted
frequency table of the exact values the series takes and adds near-Dirac atoms on
the ones it revisits (each carrying that value's frequency as probability),
mean-preserving so the atoms add mass without moving the ensemble's mean.
It's still a plain Dist. On continuous data nothing is revisited, no atom
fires, and it vanishes; unlike a simple last-value spike it also captures values
that recur often but never twice in a row. Judged by log-likelihood — the
package's metric — it dominates on administrative, grid-quoted series that sit on
a small set of values (policy rates, posted prices), where a continuous
predictive cannot place mass on an exact value.
Every policy also draws on a Yeo-Johnson coordinate candidate group (a coarse grid of the signed Box-Cox family), so the ensemble can learn the coordinate a series is simple in — log/multiplicative, sqrt, or linear — online, rather than committing to one up front.
doob is the one committed policy (after Joseph Doob): it pins the mean to a
martingale (the last value — no drift, no mean reversion) and only learns how
the volatility breathes, Bayesian-averaging several martingale predictives
that differ in their volatility clock (constant, GARCH, slowly-varying, heavy
tailed). By Dambis–Dubins–Schwarz any continuous martingale is a time-changed
Brownian motion, so the bet is exactly "BM on a stochastic clock". Feed it the
level series (prices, indices, rates), not pre-differenced changes: when the
martingale prior holds it beats the diffuse laplace ensemble by committing the
mean and spending its capacity on the clock; on genuinely mean-reverting series
(e.g. the VIX) the prior is wrong and it gives ground — a deliberately sharp tool.
Or tune directly:
from skaters import skater
f = skater(k=3, aggressiveness=0.9) # fast adapter
f = skater(k=3, aggressiveness=0.1) # conservative
Architecture
Everything is transforms all the way down, with a distributional leaf at the bottom:
$$y ;\xrightarrow{T_1}; y' ;\xrightarrow{T_2}; y'' ;\xrightarrow{\cdots}; \text{leaf} ;\rightarrow; \hat{D}$$
The leaf estimates $\hat{D} = \mathcal{N}(0, \hat\sigma^2)$ from residuals via Welford's algorithm. The prediction in the original space is obtained by inverting the transform chain:
$$\hat{D}_{\text{original}} = T_1^{-1}\bigl(T_2^{-1}\bigl(\cdots\bigl(\hat{D}\bigr)\bigr)\bigr)$$
Every node returns list[Dist]. There is no separate "point forecast" vs "uncertainty" — both are aspects of the same $\hat{D}$.
The key insight
Every "model" is really a transform. An EMA doesn't "predict" — it subtracts a running level $\ell_t$, leaving simpler residuals $\varepsilon_t = y_t - \ell_t$. The prediction comes from inverting the transform chain applied to the leaf's distributional estimate.
The Dist type
A weighted mixture of Gaussians $\sum_{i} w_i ,\mathcal{N}(\mu_i, \sigma_i^2)$. Pure Python (math.erf, math.exp).
from skaters import Dist
d = Dist.gaussian(5.0, 2.0)
d.mean # 5.0
d.std # 2.0
d.pdf(5.0) # density at x
d.cdf(3.0) # P(X <= 3)
d.logpdf(5.0) # log-likelihood
d.quantile(0.975) # inverse CDF
# Exact mixture combination (for ensembles)
mix = Dist.combine([d1, d2, d3], weights=[0.5, 0.3, 0.2])
# Propagate through transform inverses
d.shift(10.0) # translate: mu -> mu + 10
d.scale(2.0) # scale: mu -> 2*mu, sigma -> 2*sigma
d.affine(2.0, 3.0) # x -> 2x + 3
# Bound component growth
d.prune(max_components=10)
Transforms
Online bijective maps. Each has a forward (scalar in, scalar out) and an inverse_k that propagates $\text{Dist}$ objects back through the inverse.
| Transform | Forward | Inverse | Use case |
|---|---|---|---|
ema_transform($\alpha$) |
$y'_t = y_t - \ell_t$ | $D \mapsto D + \ell_t$ | Remove level |
difference() |
$y't = y_t - y{t-1}$ | Cumsum with $\text{Var}$ growing as $\sum \sigma_h^2$ | Random walk |
drift($\alpha, \lambda$) |
$y'_t = \Delta y_t - \hat\mu_t$ | $y_t + h\hat\mu + \sum\varepsilon$ | Random walk + drift |
holt_linear($\alpha, \beta$) |
$y'_t = y_t - (\ell_t + b_t)$ | $\ell_t + h \cdot b_t + \varepsilon$ | Level + trend (Holt 1957) |
ar($p$) |
$y't = y_t - \sum \hat\phi_j y{t-j}$ | AR reconstruction with variance propagation | Autoregression (online RLS) |
grouped_ar($L$) |
Same, grouped coefficients | Same | Long-lag AR with $O(\log L)$ params |
fractional_difference($d$) |
$y'_t = (1-B)^d , y_t$ | $(1-B)^{-d}$ | Long memory |
standardize($\alpha$) |
$y'_t = (y_t - \hat\mu_t) / \hat\sigma_t$ | $D \mapsto \hat\sigma_t \cdot D + \hat\mu_t$ | Remove scale |
garch($\omega, \alpha, \beta$) |
$y'_t = y_t / \hat\sigma_t$ | $D \mapsto \hat\sigma_t \cdot D$ | Volatility clustering |
seasonal_difference($s$) |
$y't = y_t - y{t-s}$ | Shift by lagged value | Periodicity |
power_transform($p$) |
$y'_t = \text{sign}(y_t)|y_t|^p$ | Delta method | Tail compression |
Conjugation
Transforms compose via conjugation. Given a transform $T$ and a skater $f$:
$$f_{\text{conjugated}}(y) = T^{-1}!\bigl(f\bigl(T(y)\bigr)\bigr)$$
The pipe | notation reads left-to-right (outermost transform first):
from skaters import conjugate, ema, difference, standardize
# diff removes trend, EMA predicts the differenced series
f = conjugate(ema(alpha=0.1, k=3), difference(), k=3)
# Chain: standardize, then difference, then EMA
f = conjugate(
conjugate(ema(alpha=0.1, k=3), difference(), k=3),
standardize(),
k=3,
)
# canonical name: std|diff|ema_t|leaf
Ensembles
Precision-weighted (MSE)
Weights by $w_i \propto 1/\text{MSE}_i$ where $\text{MSE} = \text{bias}^2 + \text{variance}$.
from skaters import precision_weighted_ensemble, ema
f = precision_weighted_ensemble([
ema(alpha=0.05, k=1),
ema(alpha=0.2, k=1),
], k=1)
Bayesian (log-likelihood, XGBoost-inspired regularization)
Each model $i$ accumulates a log-weight updated at every observation:
$$\log w_i ;\mathrel{+}=; \eta \cdot \log p_i(y_t) ;-; \lambda \cdot d_i$$
where $\eta$ is the learning rate (shrinkage), $\lambda$ is the complexity penalty, and $d_i$ is the model's depth. Predictions are combined via $\text{Dist.combine}$ with softmax weights.
from skaters import bayesian_ensemble, ema
f = bayesian_ensemble(
[ema(alpha=0.05, k=1), ema(alpha=0.2, k=1)],
k=1,
learning_rate=0.5, # eta: prevents over-concentrating
complexity_penalty=0.02, # lambda: penalizes deeper chains
depths=[1, 1],
)
Adaptive search (beam search over transform grammar)
Grows the candidate population online: expand top performers with new transforms, replay recent history to warm-start, prune losers.
from skaters import search
f = search(
k=1,
expand_interval=100, # expand top performers every 100 obs
max_depth=3, # maximum transform chain depth
replay_buffer=500, # warm-start new candidates on recent history
max_pool=30, # cap active candidates
)
Heavy tails: the scale-mixture leaf
Everything here is judged by predictive log-likelihood. A plain Gaussian leaf gets the location and scale right but the shape wrong on heavy-tailed residuals (returns, macro data), and — crucially — Bayesian model averaging preserves the mean and variance but washes the kurtosis out, so adding heavy leaves to the candidate pool doesn't help.
The fix is the scale-mixture leaf: a fixed dictionary of zero-mean Gaussians
N(0, aᵢ·σ) with weights learned online (a Student-t is a Gaussian scale
mixture, so this approximates it). It's a plain Dist; the weights are the
"discrepancy from N(0,1)" — all on a=1 is Gaussian, mass on larger a is fat
tails. It matches the Gaussian leaf on Gaussian data and beats it as tails fatten.
from skaters import scale_mixture_leaf, terminal_leaf_ensemble, leaf
Because mixing washes out shape, the named policies use a terminal-leaf
ensemble: the candidates are combined for the mean, then one terminal
scale-mixture leaf models the combined residual — so the leaf's shape reaches the
output undiluted. On Student-t₃ this takes laplace from a logpdf of ≈ −2.07
(Gaussian-collapsed) to ≈ −1.93, with no cost on Gaussian data.
Dist.crps(y) (closed-form CRPS) is also available as a proper score for
benchmarking.
Spec system
Serialize and rebuild any pipeline:
from skaters import (
build, spec_name, to_json, from_json,
ema_spec, conjugate_spec, ensemble_spec, diff_spec,
)
spec = ensemble_spec(
conjugate_spec(ema_spec(0.1, k=1), diff_spec()),
ema_spec(0.3, k=1),
k=1,
)
spec_name(spec) # "ensemble(diff|ema(0.1),ema(0.3))"
j = to_json(spec) # JSON string
f = build(from_json(j)) # live skater
Writing a custom transform
Any $(T, T^{-1})$ pair where forward is scalar and inverse_k maps list[Dist]:
def my_transform():
def forward(y, state):
if state is None:
return 0.0, {"anchor": y}
transformed = y - state["anchor"]
return transformed, {"anchor": y}
def inverse_k(dists, state):
return [d.shift(state["anchor"]) for d in dists]
return forward, inverse_k
JavaScript & the browser
The whole library is also a zero-dependency JavaScript port (docs/js/skaters/) — every
transform, ensemble, and named policy. It is verified against the Python reference by a parity
suite that checks 76,000+ values to 1e-6 (parity/, run in the test suite via
tests/test_js_parity.py).
<script type="module">
import { kahneman } from "https://skaters.microprediction.org/js/skaters/index.mjs";
const f = kahneman(1);
let state = null;
for (const y of observations) {
const [dists, st] = f(y, state); state = st;
dists[0].mean; // point forecast
dists[0].quantile(0.975); // 97.5th percentile
}
</script>
Interactive demos (forecasting playground in native JS, and the real Python package running in Pyodide) live at skaters.microprediction.org/demos.
Design
- Online only — $O(1)$ per observation, no batch recomputation
- Distributional — every prediction is a $\text{Dist}$, not a point estimate
- Composable — transforms chain, ensembles nest, everything returns $\text{Dist}$
- Pure Python — zero dependencies, only
math.erfandmath.exp - Pyodide compatible — works in the browser via WebAssembly
Lineage
This package distills ideas from timemachines, which provided a common skater interface for dozens of time series packages. This is a from-scratch rewrite focused on speed, distributional predictions, and browser compatibility.
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