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jHBV

PyPI version License

Dual-backend (JAX + NumPy) implementation of the HBV-96 rainfall–runoff model — usable standalone or as a SYMFLUENCE plugin.

Part of the SYMFLUENCE JAX-native model family — self-contained packages that run standalone (NumPy fallback, no JAX required) and register automatically with SYMFLUENCE when installed alongside it.

Features

  • Differentiable: automatic differentiation through the full simulation (JAX)
  • Fast: JIT compilation via lax.scan; vmap for ensembles; GPU-capable
  • Dependency-light: pure-NumPy fallback when JAX is not installed
  • Plugin architecture: auto-registers with SYMFLUENCE via entry points

Installation

pip install jhbv          # NumPy backend
pip install 'jhbv[jax]'    # with JAX (differentiable, JIT)

Quickstart

import numpy as np
from jhbv import simulate

# daily forcing: precipitation (mm/d), temperature (degC), PET (mm/d)
runoff, state = simulate(precip, temp, pet)           # default parameters

params = {"FC": 250.0, "BETA": 2.0, "K1": 0.1}        # override any subset
runoff, state = simulate(precip, temp, pet, params=params)

# hourly simulation (parameters stay in daily units)
runoff_h, _ = simulate(precip_h, temp_h, pet_h, timestep_hours=1)

Gradient-based calibration

The JAX backend makes the full simulation differentiable end-to-end, so model parameters can be calibrated with gradient descent:

import jax
from jhbv import kge_loss, get_kge_gradient_fn

grad_fn = get_kge_gradient_fn(precip, temp, pet, observed)
value, grads = grad_fn(params)          # dKGE/dparam for every parameter

nse_loss / kge_loss and their gradient factories are JIT-compatible and work with any optax optimizer. Within SYMFLUENCE the same interface powers the ADAM and L-BFGS calibration options.

Use with SYMFLUENCE

jhbv registers with SYMFLUENCE through the symfluence.plugins entry point — installation is the integration:

pip install symfluence jhbv
# config.yaml (excerpt)
model:
  hydrological_model: HBV

SYMFLUENCE then handles forcing preparation, calibration, evaluation, and benchmarking for the model with no further wiring.

Model structure

HBV-96 (Lindström et al., 1997) consists of four routines, all implemented with smooth, differentiable formulations:

  1. Snow — degree-day accumulation and melt with refreezing
  2. Soil moisture — beta-function recharge and evapotranspiration reduction
  3. Response — two-box (upper/lower zone) storage with percolation
  4. Routing — triangular transfer-function convolution

15 calibration parameters (jhbv.PARAM_BOUNDS), with defaults in jhbv.DEFAULT_PARAMS. Daily and sub-daily timesteps are supported; parameters are specified in daily units and scaled internally (timestep_hours argument).

Testing

pip install -e '.[dev]'
pytest

How to cite

If you use jHBV in your research, please cite the SYMFLUENCE companion papers, which describe the design of the JAX-native model family (registry integration, differentiability, and the calibration experiments they enable):

Eythorsson, D., et al. (2026). The registry as social contract: Architectural patterns for community hydrological modeling. Water Resources Research (submitted).

Eythorsson, D., et al. (2026). From configuration to prediction: Multi-model, multi-basin experiments with SYMFLUENCE. Water Resources Research (submitted).

Citation metadata for this package is provided in CITATION.cff; a version-specific DOI is minted via Zenodo for each GitHub release.

References

  • Lindström, G., Johansson, B., Persson, M., Gardelin, M., & Bergström, S. (1997). Development and test of the distributed HBV-96 hydrological model. Journal of Hydrology, 201(1–4), 272–288. https://doi.org/10.1016/S0022-1694(97)00041-3
  • Bergström, S. (1995). The HBV model. In V. P. Singh (Ed.), Computer Models of Watershed Hydrology (pp. 443–476). Water Resources Publications.

License

Apache-2.0. See LICENSE.

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