Ocean Biogeochemistry in GFDL's Earth System Model 4.1 and Its Response to Increasing Atmospheric CO2

Journal of Advances in Modeling Earth Systems

Charlotte Laufkötter¹  Paul Ginoux²  Jasmin John²  John P. Krasting²  Charles A. Stock²  Songmiao Fan²  Fabien Paulot²  John P. Dunne²  Niki Zadeh³ 

[1] Climate and Environmental Phys University of Bern Bern Switzerland;National Ocean and Atmospheric Administration Geophysical Fluid Dynamics Laboratory Princeton NJ USA;SAIC/GFDL Princeton NJ USA;

关键词: Earth System Model;    ocean biogeochemistry;    climate change;    carbon cycle;    marine ecosystems;   

DOI  :  10.1029/2019MS002043

来源: DOAJ

【 摘 要 】

Abstract 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 CO2. 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 CO2 increase from preindustrial conditions (i.e., years 101–120 of a 1% CO2 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.

【 授权许可】

Unknown