FluxPrint

FluxPrint is an open-source Python package implementing flux footprint models for eddy covariance data analysis. It provides footprint-model implementations behind a single, consistent interface so researchers can compare spatially resolved fluxes with field measurements, and add new models by following a small convention. It is designed for interoperability with ecosystem flux datasets (e.g. FLUXNET). See Figure 1 for the conceptual scheme.

Figure 1. Conceptual scheme for FluxPrint.

Why FluxPrint?

Most eddy-covariance users already have Kljun's official FFP scripts or EddyPro's built-in footprint estimates. FluxPrint adds, on top of the same science:

• Verified fidelity: the Kljun et al. (2015) implementation is pinned against the original FFP code (vendored in this repository) by regression tests asserting bitwise-identical fields — a dedicated CI job fails if any registered model ever diverges from its reference implementation.
• A batch workflow: one call takes a half-hourly table (FLUXNET/ICOS style), validates and estimates missing micrometeorology per record, and returns a typed FootprintSeries ready for climatologies.
• A typed object API: georeferencing, source-area contours, plots, NetCDF/GeoTIFF/Shapefile export, and provenance metadata on every result.

Features

• Footprint models behind one interface, selected by name (currently Kljun et al., 2015; Hsieh et al., 2000 is an experimental work in progress; Kormann & Meixner, 2001 is planned).
• A typed footprint object (Footprint): a 2-D source-area field on a fixed grid centred on the tower, plus FootprintSeries for time-ordered stacks.
• Two coordinate frames: a local, tower-centred metric grid, and a georeferenced projected grid (georeference()); lon/lat is display-only.
• Source-area contours: contours() for the 50/80% isopleths, plot() for a quick look, to_shapefile() for GIS.
• Serialization: NetCDF is the native format (CF grid mapping included), with GeoTIFF conversion; outputs carry provenance (package/model version, citation, settings).
• Aggregation: collapse a FootprintSeries into a climatology.

Installation

pip install fluxprint

Or from source for development:

pip install git+https://github.com/pedrohenriquecoimbra/fluxprint

import fluxprint is light: the geo/plotting stack (xarray/netcdf4, rasterio, pyproj, fiona/shapely, matplotlib) is imported lazily by the operations that need it. Those libraries are still installed as dependencies today; a future release will move them into the already-declared extras (fluxprint[netcdf], [tiff], [crs], [shapefile]; [viz] adds folium for interactive maps, [all] installs everything).

Quickstart

From a met table to a climatology (the batch path)

import pandas as pd
import fluxprint

data = pd.read_csv("halfhours.csv", na_values=[-9999])  # FLUXNET-style table

climatology = fluxprint.wrapper(
    data=data,
    zm=20.0,       # aerodynamic height: z - d, see note below
    pblh=1500.0,   # boundary-layer height [m] - not in FLUXNET tables, so
                   # supply it (or a PBLH/BLH column, or opt into the crude
                   # 1000 m constant with fill_all=True)
    tower=(4321000.0, 3210000.0),   # tower position, for georeferencing
    tower_crs="EPSG:3035",
    dst="climatology.nc",           # optional: write the result
)

Columns are matched case-insensitively with common aliases (USTAR/u*, WD/wind_direction, WS/wind_speed, OL/L, SIGMA_V/v_sd, ...; H, the sensible heat flux, is matched exactly so FFP's lowercase h — the boundary-layer height — is never mistaken for it). Missing variables are estimated when physically possible — e.g. the Obukhov length from USTAR/H/TA/PA — and every estimated variable is recorded in the result's attrs["estimated_inputs"]. Crude constant fallbacks (including the pblh=1000 constant) require an explicit fill_all=True and warn loudly.

Use fluxprint.calculate_footprint(data, by="timestamp_column", ...) for one footprint per group (a FootprintSeries) instead of a single climatology.

zm is the aerodynamic height. All models define zm = z - d (measurement height above the zero-plane displacement), not the instrument height. Over vegetation the difference is substantial. If you pass measurement_height together with displacement (or canopy_height, using d ≈ 0.67·h), FluxPrint derives zm for you.

Compute a single footprint directly

from fluxprint.model import get_model

kljun = get_model("kljun2015")
fp = kljun(
    zm=2.0,          # measurement height above displacement [m]
    z0=0.01,         # roughness length [m]  (or pass umean instead)
    ustar=0.5,       # friction velocity [m s-1]
    pblh=1000.0,     # boundary-layer height [m]
    mo_length=-50.0, # Obukhov length [m]
    v_sigma=0.5,     # std. dev. of lateral velocity [m s-1]
    wind_dir=180.0,  # wind direction [deg] (orients the grid north-up)
    dx=2.0,          # grid spacing [m]
    tower=(4321000.0, 3210000.0),
    tower_crs="EPSG:3035",
)

fp.total()      # fraction of the flux captured by the grid (also in attrs)
fp.peak_xy()    # (x, y) of the footprint peak, metres from the tower
fp.contours([0.5, 0.8])   # 50%/80% source-area isopleths
fp.plot(rs=[0.5, 0.8])    # quick-look plot (matplotlib)

Inputs may be scalars (one record) or equal-length sequences (composited into a single footprint, fp.n records). Records failing the model's validity checks (including NaN gaps) are rejected per record.

Georeference and export

geo = fp.georeference("EPSG:3035")   # local metres -> projected coords (needs pyproj)
geo.to_netcdf("footprint.nc")        # needs xarray/netcdf4; CF grid mapping included
geo.to_tiff("footprint.tif")         # needs rasterio
geo.to_shapefile("contours.shp", rs=[0.5, 0.8])  # needs fiona

Adding a model

A model is a callable mapping micrometeorological inputs to one 2-D Footprint in the local frame. Register it by name and it becomes selectable everywhere:

from fluxprint.model import register_model
from fluxprint.footprint import Footprint

@register_model("my_model", description="My footprint parameterisation")
def calc(*, zm, ustar, pblh, mo_length, v_sigma, wind_dir, z0=None, umean=None,
         domain=None, dx=None, dy=None, tower=None, tower_crs=None, time=None,
         **kwargs) -> Footprint:
    f = ...  # 2-D field on a regular grid centred on the tower
    return Footprint.from_grid(f, dx=dx, tower=tower, tower_crs=tower_crs, time=time)

from fluxprint.model import available_models, get_model
available_models()        # ['kljun2015', 'my_model']
get_model("my_model")(...)

The registry is backed by regorator. New models are expected to come with a reference oracle in tests/test_reference_regression.py pinning them against their original implementation — CI enforces this.

API reference

Top level (import fluxprint)

• calculate_footprint(data, by=None, model="kljun2015", ...) — footprint each group of a table; returns a FootprintSeries.
• wrapper(...) — calculate_footprint + aggregation + optional file output.
• empty_footprint(model, domain=..., dx=...) — a NaN template on the model's grid.
• read_handler / read_from_url / read_from_file — table/NetCDF/TIFF readers.
• Legacy write_to_* helpers are deprecated: use the Footprint.to_* methods.

fluxprint.model

• get_model(name) — return the registered model callable.
• available_models() — list registered model names.
• register_model(name, description="", **attrs) — decorator to register a model.
• FootprintModel — the callable protocol models conform to.

fluxprint.footprint.Footprint

• Footprint.from_grid(f, dx, dy=None, **meta) — build a local, tower-centred footprint.
• georeference(target_crs) / to_lonlat() — local → projected; display lon/lat.
• total(), peak_xy(), normalized(), contours(rs) — analysis helpers.
• plot(rs=None) — matplotlib quick look (never calls plt.show()).
• to_netcdf / from_netcdf, to_tiff / from_tiff, to_xarray / from_xarray, to_shapefile.

fluxprint.footprint.FootprintSeries

• aggregate(smooth=True) — collapse the stack to a 2-D climatology.
• georeference(target_crs), to_netcdf / from_netcdf, to_xarray / from_xarray.

See CHANGELOG.md for release notes and deprecations.

Examples

See the sample/ directory for usage examples.

Citing FluxPrint

If FluxPrint contributes to your research, please cite the software (see CITATION.cff) alongside the footprint-model paper you used (e.g. Kljun et al., 2015 — the models' own citations and DOIs are stamped into every output's metadata).

Contributing

Contributions are welcome — see CONTRIBUTING.md for the development setup, and open a pull request from a feature branch.

License

Licensed under the European Union Public Licence v. 1.2 (EUPL-1.2). See the LICENSE file for details. The vendored Kljun et al. (2015) FFP reference code (fluxprint/model/Kljun_et_al_2015_original/) is distributed under its own permissive licence (see the license.txt alongside it), copyright (C) 2015–2023 Natascha Kljun.

Acknowledgments

• Kljun, N., Calanca, P., Rotach, M. W., Schmid, H. P. (2015): The simple two-dimensional parameterisation for Flux Footprint Predictions (FFP), Geosci. Model Dev. 8, 3695–3713, doi:10.5194/gmd-8-3695-2015.
• Hsieh, C.-I., Katul, G., Chi, T. (2000): An approximate analytical model for footprint estimation of scalar fluxes in thermally stratified atmospheric flows, Adv. Water Resour. 23, 765–772, doi:10.1016/S0309-1708(99)00042-1.
• Kormann, R., Meixner, F. X. (2001): An analytical footprint model for non-neutral stratification, Boundary-Layer Meteorol. 99, 207–224, doi:10.1023/A:1018991015119.

Contact

• Pedro Henrique Coimbra
• GitHub Issues