PyESPER is a Python implementation of MATLAB Empirical Seawater Property Estimation Routines (ESPERs), and the present version consists of a preliminary package which implements these routines. These routines provide estimates of seawater biogeochemical properties at user-provided sets of coordinates, depth, and available biogeochemical properties.
This package is developed in parallel with TRACE-Python.
This is [C]Worthy's fork of LarissaMDias/PyESPER. It is
not published to PyPI or conda (pip install PyESPER installs the upstream package, which has
none of the fork's additions); install it from a clone, at a tagged version. Fork versions are
<upstream version>+cworthy.<n> (a PEP 440 local version that sorts after the upstream release
it builds on), with a matching git tag:
git clone --branch v1.1.1+cworthy.1 https://github.com/CWorthy-ocean/PyESPER
cd PyESPER
pip install -e .Use a virtual environment if you like; the editable install brings in the dependencies from
setup.py and, because the package stays in the clone, lets PyESPER find its data directories
(Mat_fullgrid/ and NeuralNetworks/) next to it. Note: Examples rely on the GLODAPv2.2023
dataset, which requires the separate glodap package.
PyESPER offers three algorithms to predict desired variables:
- PyESPER_LIR: Interpolated linear networks (LIRv.3 / ESPERv1.1).
- PyESPER_NN: Neural network estimations (ESPERv1.1).
- PyESPER_Mixed: An averaged ensemble of LIR and NN estimates.
The routines calculate coefficients and intercepts across up to 16 equation combinations. The base predictors are always Salinity (S) and Temperature (T). The remaining predictors (A, B, C) shift depending on the target variable.
| Desired Variable | Predictor A | Predictor B | Predictor C |
|---|---|---|---|
| TA, DIC, pH, phosphate | Nitrate | Oxygen | Silicate |
| nitrate | Phosphate | Oxygen | Silicate |
| silicate | Phosphate | Oxygen | Nitrate |
| oxygen | Phosphate | Nitrate | Silicate |
Equation Options:
- S, T, A, B, C
- S, T, A, C
- S, T, B, C
- S, T, C
- S, T, A, B
- S, T, A
- S, T, B
- S, T
- S, A, B, C
- S, A, C
- S, B, C
- S, C
- S, A, B
- S, A
- S, B
- S
import PyESPER
outputs = PyESPER.emlr_estimate(
DesiredVariables=["TA", "DIC"],
Path="/path/to/Mat_fullgrid/",
OutputCoordinates={
"longitude": [0.0, 180.0],
"latitude": [85.0, -20.0],
"depth": [10, 1000]
},
PredictorMeasurements={
"salinity": [35.0, 34.1],
"temperature": [0.1, 10.0],
"oxygen": [202.3, 214.7],
"silicate": [15.0, 45.2],
"nitrate": [1.2, 30.5]
},
EstDates=[2020.5, 2020.5],
Equations=[1, 2, 8, 16],
PerKgSwTF=True
)| Parameter | Type | Description |
|---|---|---|
DesiredVariables |
list[str] |
Variables to return. Options: "TA", "DIC", "pH", "phosphate", "nitrate", "silicate", "oxygen". |
Path |
str |
Absolute or relative path to the downloaded LIR .mat files. |
OutputCoordinates |
dict |
Keys: "longitude" (°E), "latitude" (°N), "depth" (m). Values must be arrays of length n. |
PredictorMeasurements |
dict |
Keys: "salinity", "temperature", "phosphate", "nitrate", "silicate", "oxygen". Values are arrays of length n. Unmeasured variables can be omitted or filled with NaN. |
| Parameter | Type | Default | Description |
|---|---|---|---|
EstDates |
list[float] |
2002.0 |
Decimal dates for the estimates. Crucial for DIC and pH accuracy. |
Equations |
list[int] |
1:16 |
Specific equation permutations to run (1-16). |
MeasUncerts |
dict |
WOCE Defaults | Keys: "sal_u", "temp_u", "phosphate_u", "nitrate_u", "silicate_u", "oxygen_u". |
pHCalcTF |
bool |
False |
Recalculates pH as if derived from TA/DIC rather than measured via dye. |
PerKgSwTF |
bool |
True |
Set to False if your inputs are volumetric (µmol/L) rather than molal (µmol/kg). Outputs are always molal. |
VerboseTF |
bool |
True |
Toggles terminal logging. |
ESPER was fit to GLODAP bottle data, which has almost no tropical or mid-latitude
observations below ~31 PSU. Fed a river-plume salinity the nets extrapolate unphysically
(silicate > 100 µmol/kg, negative nutrients, DIC above TA). The dask-lazy wrappers
PyESPER.nn_xr / lir_xr / mixed_xr can instead evaluate the nets at a raised-cosine
blend of the model salinity toward the WOA23 annual-mean climatology below a band
(default 31–34 PSU), and then dilute the TA/DIC estimates from that salinity back to the
model salinity along a conservative mixing line (freshwater endmember 770 µmol/kg for both
by default, ta_endmember/dic_endmember), so alkalinity and DIC scale with salinity in a
plume. The DIC/TA ratio is the nets' own at the conditioned salinity and tends to
dic_endmember/ta_endmember (1 by default, approached from below) in fresh water; keep
dic_endmember <= ta_endmember so DIC never crosses above TA. Above the band nothing
changes. The climatology file is not
downloaded by PyESPER — pass its path, and the error names the download URL if it is
missing:
from PyESPER import nn_xr
from PyESPER.salinity_conditioning import SalinityConditioning
cond = SalinityConditioning("/path/to/woa23_decav_s00_01.nc") # low=31, high=34
est = nn_xr(salinity, temperature, longitude, latitude, depth,
variables=["nitrate", "TA", "DIC"], est_dates=dates,
salinity_conditioning=cond)See PyESPER/salinity_conditioning.py for the rationale and the measurements behind
the default band.
PyESPER returns three dictionaries, shape (n, e) where n is the number of coordinates and e is the number of equations computed:
- Estimates: The computed variables (µmol/kg, except for unitless pH).
- Coefficients: The equation intercepts and weights used for the estimation (LIR algorithm only).
- Uncertainties: The propagated uncertainty bounds for the estimate.
Missing Data Handling: Passing NaN as a coordinate or required predictor parameter will cascade and return NaN for all dependent equation estimates.
If you use this package, cite the relevant publications:
- PyESPER Implementation: Carter et al., 2021 (doi: 10.1002/lom3/10461)
- LIRv3 / ESPER_NN (ESPERv1.1): Carter, 2021 (doi: 10.5281/ZENODO.5512697)
- LIARv1: Carter et al., 2016 (doi: 10.1002/lom3.10087)
- LIARv2, LIPHR, LINR: Carter et al., 2018 (doi: 10.1002/lom3.10232)
- LIPR, LISIR, LIOR: Carter et al., 2021 (doi: 10.1002/lom3/10232)
- Neural Network Inspiration (CANYON-B): Bittig et al., 2018 (doi: 10.3389/fmars.2018.00328)