PyCantPhi is a Python package for calculating anthropogenic carbon (Cant) in the North Atlantic Ocean using the φ CT° (Phi) method, and cStar and Troca methods. The cStar and Troca methods can be applyied globally for general purpose.
- Implementation of the φ CT° method for anthropogenic carbon calculation
- Integration with Mauna Loa CO2 data
- Support for water mass analysis using Optimum MultiParameter (OMP)
- Preformed alkalinity calculations
- Mediterranean water influence calculations
- CO2 system calculations using PyCO2SYS
You can install PyCantPhi using pip:
pip install pycantphi
import numpy as np
import pandas as pd
import xarray as xr
from pycantphi import cantphi, CantCalculator
# Define dimensions for dataset
loc = ["loc1", "loc2", "loc3"]
pressure = [0, 250, 2000] # in dbar
time = pd.date_range(start='2020', end='2023', freq='Y')
lon = [-10, -20, -40]
lat = [10, 20, 65]
# Create coordinate data for xarray
coords = {
"location": loc,
"pressure": pressure,
"time": time,
"longitude": ("location", lon),
"latitude": ("location", lat),
"year": ("time", time.year),
}
# Note that it's also possible to have no location variable (here, we're creating a three-dimensional dataset) and rely solely on longitude or latitude. The other variable (longitude or latitude) is always required as a function of the first.
# Generate synthetic data arrays
data_vars = {
"theta": (["location", "pressure", "time"], np.random.uniform(1, 15, (3, 3, 3))), # in Celsius
"salinity": (["location", "pressure", "time"], np.random.uniform(30, 37, (3, 3, 3))), # in PSU
"alkalinity": (["location", "pressure", "time"], np.random.uniform(2200, 2400, (3, 3, 3))), # in µmol/kg
"oxygen": (["location", "pressure", "time"], np.random.uniform(310, 330, (3, 3, 3))), # in µmol/kg
"carbon": (["location", "pressure", "time"], np.random.uniform(1800, 2100, (3, 3, 3))), # in µmol/kg
"phosphate": (["location", "pressure", "time"], np.random.uniform(0, 3, (3, 3, 3))), # in µmol/kg
"nitrate": (["location", "pressure", "time"], np.random.uniform(0, 40, (3, 3, 3))), # in µmol/kg
"silicate": (["location", "pressure", "time"], np.random.uniform(0, 150, (3, 3, 3))) # in µmol/kg
}
# Create the xarray Dataset
ds = xr.Dataset(data_vars, coords=coords)
# Display the dataset
ds
# Initialize the calculator
calc = cantphi(ds)
# Process the dataset
results = calc.process()
# Access the calculated Cant values
cant_phi = results.cAntPhiCt0ML
cant_troca = results.cAntTroca
cant_cstar = results.cStar
# Access only the Cant calculator for the different methods. They can be run outside but required specific parameters.
CantCalculator.calculate_cstar(ct, aou, ct_preformed, delta_ca_corrected)
CantCalculator.calculate_ctroca(ct, at, oxygen, theta)
CantCalculator.calculate_cphi(calc.ds)
Your input dataset should include the following variables:
- longitude
- latitude
- pressure
- theta (potential temperature)
- salinity
- oxygen
- silicate
- nitrate
- phosphate
- carbon
- alkalinity
- year
The documentation is in progress. For detailed documentation, examples, and API reference, visit our documentation page once finished.
Contributions are welcome! I'm working on generating pytests before taking new contributions into account. If you encounter a problem with the package, please raise an issue.
This project is licensed under the MIT License - see the LICENSE file for details.
If you use this package in your research, please cite both the original CantPhiCt0 paper and this implementation in python:
For the method:
@article{vázquez2009anthropogenic,
title={Anthropogenic carbon distributions in the Atlantic Ocean: data-based estimates from the Arctic to the Antarctic},
author={V{\'a}zquez-Rodr{\'\i}guez, M and Touratier, F and Lo Monaco, C and Waugh, DW and Padin, XA and Bellerby, RGJ and Goyet, C and Metzl, N and R{\'\i}os, AF and P{\'e}rez, FF},
journal={Biogeosciences},
volume={6},
number={3},
pages={439--451},
year={2009},
doi={10.5194/bg-6-439-2009},
publisher={Copernicus GmbH}
}
For the software:
@software{pyphi2024,
title = {PyCantPhi: A Python implementation of the φ CT° method for anthropogenic carbon calculation},
author = {Bajon R.},
year = {2024},
version = {0.0.0},
url = {https://github.com/RaphaelBajon/pyphi}
}
The implementation is based on the φ CT° method described in Vázquez-Rodríguez et al. (2009).