A thermal acid calcification cause for seasonal oscillations in the increasing Keeling curve

Fuente: arXiv
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Autori principali: Kennedy, Ivan R., Runcie, John, Crossan, Angus N., Ritchie, Ray, Marohasy, Jennifer
Natura: Preprint
Pubblicazione: 2025
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author Kennedy, Ivan R.
Runcie, John
Crossan, Angus N.
Ritchie, Ray
Marohasy, Jennifer
author_facet Kennedy, Ivan R.
Runcie, John
Crossan, Angus N.
Ritchie, Ray
Marohasy, Jennifer
contents Why do atmospheric carbon dioxide levels rise and fall seasonally measured on Mauna Loa? This study explores the thermal acid-calcification (TAC) hypothesis, suggesting that seasonal temperature shifts in surface seawater trigger acid pH-driven CO2 emissions caused by calcification. Using oceanographic data, we modeled how temperature affects dissolved inorganic carbon including CO2, bicarbonate, and carbonate. Our findings reveal that warming waters absorb atmospheric CO2 by promoting calcium carbonate formation, acidifying seawater and boosting CO2 release to the atmosphere in late autumn and winter, when atmospheric CO2 becomes highest. The model predicts a net annual CO2 rise of 2 ppmv, driven by calcification rather than land-based processes. Seasonal pH swings of 0.04 units corroborate this mechanism. The TAC hypothesis indicates that continued ocean warming, not just fossil fuels, contribute to rising CO2 levels, calling for deeper investigation into marine carbon dynamics.
format Preprint
id arxiv_https___arxiv_org_abs_2505_06253
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle A thermal acid calcification cause for seasonal oscillations in the increasing Keeling curve
Kennedy, Ivan R.
Runcie, John
Crossan, Angus N.
Ritchie, Ray
Marohasy, Jennifer
Geophysics
Atmospheric and Oceanic Physics
Why do atmospheric carbon dioxide levels rise and fall seasonally measured on Mauna Loa? This study explores the thermal acid-calcification (TAC) hypothesis, suggesting that seasonal temperature shifts in surface seawater trigger acid pH-driven CO2 emissions caused by calcification. Using oceanographic data, we modeled how temperature affects dissolved inorganic carbon including CO2, bicarbonate, and carbonate. Our findings reveal that warming waters absorb atmospheric CO2 by promoting calcium carbonate formation, acidifying seawater and boosting CO2 release to the atmosphere in late autumn and winter, when atmospheric CO2 becomes highest. The model predicts a net annual CO2 rise of 2 ppmv, driven by calcification rather than land-based processes. Seasonal pH swings of 0.04 units corroborate this mechanism. The TAC hypothesis indicates that continued ocean warming, not just fossil fuels, contribute to rising CO2 levels, calling for deeper investigation into marine carbon dynamics.
title A thermal acid calcification cause for seasonal oscillations in the increasing Keeling curve
topic Geophysics
Atmospheric and Oceanic Physics
url https://arxiv.org/abs/2505.06253