Japan Geoscience Union Meeting 2019

Presentation information

[J] Poster

A (Atmospheric and Hydrospheric Sciences ) » A-OS Ocean Sciences & Ocean Environment

[A-OS16] Chemical and Biological Oceanography

Mon. May 27, 2019 1:45 PM - 3:15 PM Poster Hall (International Exhibition Hall8, Makuhari Messe)

convener:Namiha Yamada(National Institute of Advanced Industrial Science and Technology), Sayaka Yasunaka(Japan Agency for Marine-Earth Science and Technology), Hiroaki Saito(Atmosphere and Ocean Research Institute, The University of Tokyo)

[AOS16-P02] Pacific anthropogenic carbon between 1991 and 2017

*Akihiko Murata1, Carter B.R.2,3, Feely, R.A. Feely, R.A.3, Wanninkhof, R. Wanninkhof, R.3, Shinya Kouketsu1, Sonnerup R.E.2, Pardo P.C.4, Sabine C.L.5, Johnson G. C.3, Sloyan B.M.6, Mecking S.2, Tilbrook B.6, Speer K.7, Talley L.D.8, Millero F.J.9, Wijffels S.E.6,10, Macdonald A.M.10, Gruber N.11, Bullister J. L.3 (1.Japan Agency for Marine-Earth Science and Technology, 2.University of Washington, 3.NOAA, 4.University of Tasmania, 5.University of Hawaii Manoa, 6.CSIRO, 7.The Florida State University, 8.University of California, 9.University of Miami, 10.Woods Hole Oceanographic Institution, 11.IBP)

The ocean is storing between a fourth and a third of anthropogenic CO2 (Canth) emissions. Monitoring the oceanic CO2 sink is critical to assessing the global carbon budget. We estimate total Canth storage and accumulation rates from 14 Pacific hydrographic sections that have been occupied two to four times over the past decades, with most sections having been recently measured as part of the Global Ocean Hydrographic Investigations Program (GO-SHIP). The Canth sink over the top 1500 m of the Pacific increased from 8.6 (±1.1, 1σ) Pg of carbon decade-1 from 1995 to 2005 to 10.8 (±1.1) PgC decade-1 from 2005 to 2015. We estimate 1.2 of this observed 2.2 PgC decade-1 increase in the rate of accumulation between decades is attributable to atmospheric anthropogenic CO2 increases alone, while the remaining increase is consistent with recent literature suggesting there was an increase in the ocean carbon sink during the mid-2000s. Methods that allow for analysis of multiple occupations of sections and comparisons between different sections spaced irregularly in time are introduced. The accuracy of the resulting Canth accumulation reconstructions is limited by the accuracy of the data, suggesting that a continuation of repeat hydrographic surveys with a high emphasis on obtaining multiple independent realizations of the most accurate possible measurements is a critical piece of future carbon cycle monitoring.