Open AccessOcean Biogeochemistry in GFDL's Earth System Model 4.1 and Its Response to Increasing Atmospheric CO 2
Author(s) -
Stock Charles A.,
Dunne John P.,
Fan Songmiao,
Ginoux Paul,
John Jasmin,
Krasting John P.,
Laufkötter Charlotte,
Paulot Fabien,
Zadeh Niki
Publication year - 2020
Publication title -
journal of advances in modeling earth systems
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.03
H-Index - 58
ISSN - 1942-2466
DOI - 10.1029/2019ms002043
Subject(s) - biogeochemistry , biogeochemical cycle , environmental science , biological pump , atmospheric sciences , geophysical fluid dynamics , carbon cycle , coupled model intercomparison project , climate model , climatology , oceanography , climate change , phytoplankton , chemistry , nutrient , geology , environmental chemistry , ecology , ecosystem , organic chemistry , biology
This contribution describes the ocean biogeochemical component of the Geophysical Fluid Dynamics Laboratory's Earth System Model 4.1 (GFDL‐ESM4.1), assesses GFDL‐ESM4.1's capacity to capture observed ocean biogeochemical patterns, and documents its response to increasing atmospheric CO 2 . Notable differences relative to the previous generation of GFDL ESM's include enhanced resolution of plankton food web dynamics, refined particle remineralization, and a larger number of exchanges of nutrients across Earth system components. During model spin‐up, the carbon drift rapidly fell below the 10 Pg C per century equilibration criterion established by the Coupled Climate‐Carbon Cycle Model Intercomparison Project (C4MIP). Simulations robustly captured large‐scale observed nutrient distributions, plankton dynamics, and characteristics of the biological pump. The model overexpressed phosphate limitation and open ocean hypoxia in some areas but still yielded realistic surface and deep carbon system properties, including cumulative carbon uptake since preindustrial times and over the last decades that is consistent with observation‐based estimates. The model's response to the direct and radiative effects of a 200% atmospheric CO 2 increase from preindustrial conditions (i.e., years 101–120 of a 1% CO 2 yr −1 simulation) included (a) a weakened, shoaling organic carbon pump leading to a 38% reduction in the sinking flux at 2,000 m; (b) a two‐thirds reduction in the calcium carbonate pump that nonetheless generated only weak calcite compensation on century time‐scales; and, in contrast to previous GFDL ESMs, (c) a moderate reduction in global net primary production that was amplified at higher trophic levels. We conclude with a discussion of model limitations and priority developments.