Simulations With the Marine Biogeochemistry Library (MARBL)

被引:69
|
作者
Long, Matthew C. [1 ]
Moore, J. Keith [2 ]
Lindsay, Keith [1 ]
Levy, Michael [1 ]
Doney, Scott C. [3 ]
Luo, Jessica Y. [1 ,4 ]
Krumhardt, Kristen M. [1 ]
Letscher, Robert T. [5 ]
Grover, Maxwell [1 ]
Sylvester, Zephyr T. [6 ]
机构
[1] Natl Ctr Atmospher Res, Climate & Global Dynam Lab, POB 3000, Boulder, CO 80307 USA
[2] Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA USA
[3] Univ Virginia, Dept Environm Sci, Clark Hall, Charlottesville, VA 22903 USA
[4] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA
[5] Univ New Hampshire, Coll Engn & Phys Sci, Durham, NH 03824 USA
[6] Univ Colorado, Environm Studies Program, Boulder, CO 80309 USA
基金
美国国家科学基金会;
关键词
PHYTOPLANKTON COMMUNITY STRUCTURE; CLIMATE SYSTEM MODEL; ANTHROPOGENIC CO2; DISSOLVED IRON; SOUTHERN-OCEAN; NITROGEN-FIXATION; SEASONAL CYCLE; CARBON FLUXES; NUTRIENT; WATER;
D O I
10.1029/2021MS002647
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The Marine Biogeochemistry Library (MARBL) is a prognostic ocean biogeochemistry model that simulates marine ecosystem dynamics and the coupled cycles of carbon, nitrogen, phosphorus, iron, silicon, and oxygen. MARBL is a component of the Community Earth System Model (CESM); it supports flexible ecosystem configuration of multiple phytoplankton and zooplankton functional types; it is also portable, designed to interface with multiple ocean circulation models. Here, we present scientific documentation of MARBL, describe its configuration in CESM2 experiments included in the Coupled Model Intercomparison Project version 6 (CMIP6), and evaluate its performance against a number of observational data sets. The model simulates present-day air-sea CO2 flux and many aspects of the carbon cycle in good agreement with observations. However, the simulated integrated uptake of anthropogenic CO2 is weak, which we link to poor thermocline ventilation, a feature evident in simulated chlorofluorocarbon distributions. This also contributes to larger-than-observed oxygen minimum zones. Moreover, radiocarbon distributions show that the simulated circulation in the deep North Pacific is extremely sluggish, yielding extensive oxygen depletion and nutrient trapping at depth. Surface macronutrient biases are generally positive at low latitudes and negative at high latitudes. CESM2 simulates globally integrated net primary production (NPP) of 48 Pg C yr(-1) and particulate export flux at 100 m of 7.1 Pg C yr(-1). The impacts of climate change include an increase in globally integrated NPP, but substantial declines in the North Atlantic. Particulate export is projected to decline globally, attributable to decreasing export efficiency associated with changes in phytoplankton community composition. Plain Language Summary Numerical models of the ocean carbon cycle and biogeochemistry play a key role in understanding the fate of human carbon dioxide emissions and the magnitude of expected climate change over the next several decades to a century. Models are needed to quantify changes in the carbon reservoirs of the ocean and atmosphere and to explore interactions between climate change and carbon reservoirs that could amplify or damp future warming. This paper presents the Marine Biogeochemistry Library (MARBL), which is an ocean biogeochemistry model coupled to the Community Earth System Model (CESM). MARBL was designed to be compatible with multiple ocean models, a design motivated by an interest in building a diverse community of researchers around the development of MARBL. This paper presents a technical description of MARBL and an evaluation of the ocean biogeochemical simulation in CESM version 2. Overall, the model captures large-scale biogeochemical distributions, though several important biases are highlighted, including those dependent on the representation of circulation. MARBL provides a robust platform for researchers to address critical questions related to the impacts of climate variability and change on marine ecosystems.
引用
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页数:37
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