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Overview

Iron is one of the most important micronutrients in the ocean, limiting production in some areas. In this notebook, we make a map of iron concentration and compare it to observational data.

  1. General setup

  2. Subsetting

  3. Processing - long-term mean

  4. Comparing to observational data

Prerequisites

ConceptsImportanceNotes
MatplotlibNecessary
Intro to CartopyNecessary
Dask CookbookHelpful
Intro to XarrayHelpful
  • Time to learn: 15 min


Imports

---------------------------------------------------------------------------
ModuleNotFoundError                       Traceback (most recent call last)
Cell In[1], line 7
      3 import numpy as np
      4 import matplotlib.pyplot as plt
      5 import cartopy
      6 import cartopy.crs as ccrs
----> 7 import pop_tools
      8 from dask.distributed import LocalCluster
      9 import pandas as pd
     10 import s3fs

File ~/micromamba/envs/ocean-bgc-cookbook-dev/lib/python3.14/site-packages/pop_tools/__init__.py:4
      1 """Top-level module for pop_tools"""
----> 4 from pkg_resources import DistributionNotFound, get_distribution
      6 from .calc import cfc11sol, cfc12sol
      7 from .datasets import DATASETS

ModuleNotFoundError: No module named 'pkg_resources'

General setup (see intro notebooks for explanations)

Connect to cluster

Bring in POP grid utilities

Load the data

Subsetting

Processing - long-term mean

Pull in the function we defined in the nutrients notebook...

Take the long-term mean of our data set. We process monthly to annual data with our custom function, then use xarray’s built-in .mean() function to process from annual data to a single mean over time, since each year is the same length.

Compare to observational Fe database

This dataset includes observations from the following papers:

as collected by Long et al., 2021 -- see this paper for details.

And close the Dask cluster we spun up at the beginning.


Summary

You’ve learned how to make a map of ocean iron and compare it to observations.

References
  1. Schlitzer, R., Anderson, R. F., Dodas, E. M., Lohan, M., Geibert, W., Tagliabue, A., Bowie, A., Jeandel, C., Maldonado, M. T., Landing, W. M., Cockwell, D., Abadie, C., Abouchami, W., Achterberg, E. P., Agather, A., Aguliar-Islas, A., van Aken, H. M., Andersen, M., Archer, C., … Zurbrick, C. (2018). The GEOTRACES Intermediate Data Product 2017. Chemical Geology, 493, 210–223. 10.1016/j.chemgeo.2018.05.040
  2. Moore, J. K., & Braucher, O. (2008). Sedimentary and mineral dust sources of dissolved iron to the world ocean. Biogeosciences, 5(3), 631–656. 10.5194/bg-5-631-2008
  3. Tagliabue, A., Mtshali, T., Aumont, O., Bowie, A. R., Klunder, M. B., Roychoudhury, A. N., & Swart, S. (2012). A global compilation of dissolved iron measurements: focus on distributions and processes in the Southern Ocean. Biogeosciences, 9(6), 2333–2349. 10.5194/bg-9-2333-2012
  4. Long, M. C., Moore, J. K., Lindsay, K., Levy, M., Doney, S. C., Luo, J. Y., Krumhardt, K. M., Letscher, R. T., Grover, M., & Sylvester, Z. T. (2021). Simulations With the Marine Biogeochemistry Library (MARBL). Journal of Advances in Modeling Earth Systems, 13(12). 10.1029/2021ms002647