Find in Library
Search millions of books, articles, and more
Indexed Open Access Databases
Assessing improvements in global ocean <i>p</i>CO<sub>2</sub> machine learning reconstructions with Southern Ocean autonomous sampling
oleh: T. H. Heimdal, G. A. McKinley, A. J. Sutton, A. R. Fay, L. Gloege
Format: | Article |
---|---|
Diterbitkan: | Copernicus Publications 2024-04-01 |
Deskripsi
<p>The Southern Ocean plays an important role in the exchange of carbon between the atmosphere and oceans and is a critical region for the ocean uptake of anthropogenic CO<span class="inline-formula"><sub>2</sub></span>. However, estimates of the Southern Ocean air–sea CO<span class="inline-formula"><sub>2</sub></span> flux are highly uncertain due to limited data coverage. Increased sampling in winter and across meridional gradients in the Southern Ocean may improve machine learning (ML) reconstructions of global surface ocean <span class="inline-formula"><i>p</i></span>CO<span class="inline-formula"><sub>2</sub></span>. Here, we use a large ensemble test bed (LET) of Earth system models and the “<span class="inline-formula"><i>p</i></span>CO<span class="inline-formula"><sub>2</sub></span>-Residual” reconstruction method to assess improvements in <span class="inline-formula"><i>p</i></span>CO<span class="inline-formula"><sub>2</sub></span> reconstruction fidelity that could be achieved with additional autonomous sampling in the Southern Ocean added to existing Surface Ocean CO<span class="inline-formula"><sub>2</sub></span> Atlas (SOCAT) observations. The LET allows for a robust evaluation of the skill of <span class="inline-formula"><i>p</i></span>CO<span class="inline-formula"><sub>2</sub></span> reconstructions in space and time through comparison to “model truth”. With only SOCAT sampling, Southern Ocean and global <span class="inline-formula"><i>p</i></span>CO<span class="inline-formula"><sub>2</sub></span> are overestimated, and thus the ocean carbon sink is underestimated. Incorporating uncrewed surface vehicle (USV) sampling increases the spatial and seasonal coverage of observations within the Southern Ocean, leading to a decrease in the overestimation of <span class="inline-formula"><i>p</i></span>CO<span class="inline-formula"><sub>2</sub></span>. A modest number of additional observations in Southern Hemisphere winter and across meridional gradients in the Southern Ocean leads to an improvement in reconstruction bias and root-mean-squared error (RMSE) of as much as 86 % and 16 %, respectively, as compared to SOCAT sampling alone. Lastly, the large decadal variability of air–sea CO<span class="inline-formula"><sub>2</sub></span> fluxes shown by SOCAT-only sampling may be partially attributable to undersampling of the Southern Ocean.</p>