Supplementary figures for ‘Sparse observations induce large biases in estimates of the global ocean CO2 sink - an ocean model subsampling experiment’
Estimates of ocean ${\rm CO}_2$ uptake from global ocean biogeochemistry models and ${\rm p{CO}}_2$-based data-products differ substantially, especially in high latitudes and in the trend of the ${\rm CO}_2$ uptake since 2000. Here, we assess the effect of data sparsity on two ${\rm p{CO}}_2$-based...
| Main Authors: | , , , , , |
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| Format: | Other Non-Article Part of Journal/Newspaper |
| Language: | unknown |
| Published: |
2023
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| Subjects: | |
| Online Access: | https://doi.org/10.6084/m9.figshare.22389314.v2 https://figshare.com/articles/journal_contribution/Supplementary_figures_for_Sparse_observations_induce_large_biases_in_estimates_of_the_global_ocean_CO2_sink_-_an_ocean_model_subsampling_experiment_/22389314 |
| Summary: | Estimates of ocean ${\rm CO}_2$ uptake from global ocean biogeochemistry models and ${\rm p{CO}}_2$-based data-products differ substantially, especially in high latitudes and in the trend of the ${\rm CO}_2$ uptake since 2000. Here, we assess the effect of data sparsity on two ${\rm p{CO}}_2$-based estimates by subsampling output from a global ocean biogeochemistry model. The estimates of the ocean ${\rm CO}_2$ uptake are improved from a sampling scheme that mimics present-day sampling to an ideal sampling scheme with 1000 evenly distributed sites. In particular, insufficient sampling has given rise to strong biases in the trend of the ocean carbon sink in the ${\rm p{CO}}_2$ products. The overestimation of the ${\rm CO}_2$ flux trend by 20–35% globally and 50–130% in the Southern Ocean with the present-day sampling is reduced to less than $15\% $ with the ideal sampling scheme. A substantial overestimation of the decadal variability of the Southern Ocean carbon sink occurs in one product and appears related to a skewed data distribution in ${\rm p{CO}}_2$ space. With the ideal sampling, the bias in the mean ${\rm CO}_2$ flux is reduced from 9–12% to 2–9% globally and from 14–26% to 5–17% in the Southern Ocean. On top of that, discrepancies of about $0.4\, {\rm PgC\, yr}^{-1}$ (15%) persist due to uncertainties in the gas-exchange calculation.This article is part of a discussion meeting ‘Heat and carbon uptake in the Southern Ocean: the state of the art and future priorities’. |
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