Alternate histories: synthetic large ensembles of sea-air CO 2 flux
International audience We use a statistical emulation technique to construct synthetic ensembles of global and regional sea-air carbon dioxide (CO 2 ) flux from four observation-based products over 1985-2014. Much like ensembles of Earth system models that are constructed by perturbing their initial...
Published in: | Global Biogeochemical Cycles |
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Main Authors: | , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2022
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Subjects: | |
Online Access: | https://insu.hal.science/insu-03721925 https://insu.hal.science/insu-03721925/document https://insu.hal.science/insu-03721925/file/Global%20Biogeochemical%20Cycles%20-%202022%20-%20Olivarez%20-%20Alternate%20Histories%20Synthetic%20Large%20Ensembles%20of%20Sea%25E2%2580%2590Air%20CO2%20Flux.pdf https://doi.org/10.1029/2021GB007174 |
Summary: | International audience We use a statistical emulation technique to construct synthetic ensembles of global and regional sea-air carbon dioxide (CO 2 ) flux from four observation-based products over 1985-2014. Much like ensembles of Earth system models that are constructed by perturbing their initial conditions, our synthetic ensemble members exhibit different phasing of internal variability and a common externally forced signal. Our synthetic ensembles illustrate an important role for internal variability in the temporal evolution of global and regional CO 2 flux and produce a wide range of possible trends over 1990-1999 and 2000-2009. We assume a specific externally forced signal and calculate the rank of the observed trends within the distribution of statistically modeled synthetic trends during these periods. Over the decade 1990-1999, three of four observation-based products exhibit small negative trends in globally integrated sea-air CO 2 flux (i.e., enhanced ocean CO 2 absorption with time) that are within one standard deviation of the mean in their respective synthetic ensembles. Over the decade 2000-2009, however, three products show large negative trends in globally integrated sea-air CO 2 flux that have a low rate of occurrence in their synthetic ensembles. The largest positive trends in global and Southern Ocean flux over 1990-1999 and the largest negative trends over 2000-2009 fall nearly two standard deviations away from the mean in their ensembles. Our approach provides a new perspective on the important role of internal variability in sea-air CO 2 flux trends, and furthers understanding of the role of internal and external processes in driving observed sea-air CO 2 flux variability. |
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