eCite Digital Repository

Pacific anthropogenic carbon between 1991 and 2017

Citation

Carter, BR and Feely, RA and Wanninkhof, R and Kouketsu, S and Sonnerup, RE and Pardo, PC and Sabine, CL and Johnson, GC and Sloyan, BM and Murata, A and Mecking, S and Tilbrook, B and Speer, K and Talley, LD and Millero, FJ and Wijffels, SE and Macdonald, AM and Gruber, N and Bullister, JL, Pacific anthropogenic carbon between 1991 and 2017, Global Biogeochemical Cycles, 33, (5) pp. 597-617. ISSN 0886-6236 (2019) [Refereed Article]


Preview
PDF
4Mb
  

Copyright Statement

Copyright 2019 The Authors. Licensed under Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0) https://creativecommons.org/licenses/by-nc-nd/4.0/

DOI: doi:10.1029/2018GB006154

Abstract

We estimate anthropogenic carbon (Canth) accumulation rates in the Pacific Ocean between 1991 and 2017 from 14 hydrographic sections that have been occupied two to four times over the past few decades, with most sections having been recently measured as part of the Global Ocean Ship‐based Hydrographic Investigations Program. The rate of change of Canth is estimated using a new method that combines the extended multiple linear regression method with improvements to address the challenges of analyzing multiple occupations of sections spaced irregularly in time. The Canth accumulation rate over the top 1,500 m of the Pacific increased from 8.8 (1.1, 1σ) Pg of carbon per decade between 1995 and 2005 to 11.7 (1.1) PgC per decade between 2005 and 2015. For the entire Pacific, about half of this decadal increase in the accumulation rate is attributable to the increase in atmospheric CO2, while in the South Pacific subtropical gyre this fraction is closer to one fifth. This suggests a substantial enhancement of the accumulation of Canth in the South Pacific by circulation variability and implies that a meaningful portion of the reinvigoration of the global CO2 sink that occurred between ~2000 and ~2010 could be driven by enhanced ocean Canth uptake and advection into this gyre. Our assessment suggests that the accuracy of Canth accumulation rate reconstructions along survey lines is limited by the accuracy of the full suite of hydrographic data and that a continuation of repeated surveys is a critical component of future carbon cycle monitoring.

Item Details

Item Type:Refereed Article
Keywords:anthropogenic carbon, Pacific decadal variability, eMLR, ocean acidification, repeat hydrography
Research Division:Earth Sciences
Research Group:Oceanography
Research Field:Chemical Oceanography
Objective Division:Environment
Objective Group:Other Environment
Objective Field:Marine Oceanic Processes (excl. climate related)
UTAS Author:Tilbrook, B (Dr Bronte Tilbrook)
ID Code:137406
Year Published:2019
Web of Science® Times Cited:2
Deposited By:Directorate
Deposited On:2020-02-12
Last Modified:2020-05-26
Downloads:0

Repository Staff Only: item control page