Anthropogenic CO2 of High Emission Scenario Compensated After 3500 Years of Ocean Alkalinization With an Annually Constant Dissolution of 5 Pg of Olivine

Anthropogenic CO2 of High Emission Scenario Compensated After 3500 Years of Ocean Alkalinization With an Annually Constant Dissolution of 5 Pg of Olivine

The CO2 removal model inter-comparison (CDRMIP) has been established to approximate the usefulness of climate mitigation by some well-defined negative emission technologies. I here analyze ocean alkalinization in a high CO2 world (emission scenario SSP5-85-EXT++ and CDR-ocean-alk within CDRMIP) for...

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Bibliographic Details
Main Author: Peter Köhler
Format: Article
Language:English
Published: Frontiers Media S.A. 2020-12-01
Series:Frontiers in Climate
Subjects:
carbon cycle
CDRMIP
negative emissions
geoengineering
ocean
future
Online Access:https://www.frontiersin.org/articles/10.3389/fclim.2020.575744/full

Internet

https://www.frontiersin.org/articles/10.3389/fclim.2020.575744/full

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