An Analytical Framework for the Steady State Impact of Carbonate Compensation on Atmospheric CO[subscript 2]
The deep-ocean carbonate ion concentration impacts the fraction of the marine calcium carbonate production that is buried in sediments. This gives rise to the carbonate compensation feedback, which is thought to restore the deep-ocean carbonate ion concentration on multimillennial timescales. We fo...
Main Authors: | Omta, Anne Willem, Ferrari, Raffaele, McGee, William David |
---|---|
Other Authors: | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences |
Format: | Article |
Language: | en_US |
Published: |
American Geophysical Union (AGU)
2019
|
Online Access: | http://hdl.handle.net/1721.1/120290 https://orcid.org/0000-0002-3736-1956 |
Similar Items
-
Dependence of the ocean-atmosphere partitioning of carbon on temperature and alkalinity
by: Omta, Anne Willem, et al.
Published: (2018) -
Multiple regimes of air-sea carbon partitioning identified from constant-alkalinity buffer factors
by: Goodwin, Philip, et al.
Published: (2018) -
The Production and Dissipation of Compensated Thermohaline Variance by Mesoscale Stirring
by: Smith, K. Shafer, et al.
Published: (2010) -
A Mechanistic Model of Macromolecular Allocation, Elemental Stoichiometry, and Growth Rate in Phytoplankton
by: Omta, Anne Willem, et al.
Published: (2020) -
On the potential role of marine calcifiers in glacial-interglacial dynamics: CALCIFIERS AND GLACIAL DYNAMICS
by: Omta, Anne Willem, et al.
Published: (2020)