Biogeochemical versus ecological consequences of modeled ocean physics

被引:20
作者
Clayton, Sophie [1 ,2 ]
Dutkiewicz, Stephanie [1 ]
Jahn, Oliver [1 ]
Hill, Christopher [1 ]
Heimbach, Patrick [1 ,3 ,4 ]
Follows, Michael J. [1 ]
机构
[1] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA
[2] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA
[3] Univ Texas Austin, Inst Computat Engn & Sci, Austin, TX 78712 USA
[4] Univ Texas Austin, Jackson Sch Geosci, Austin, TX 78712 USA
基金
美国国家科学基金会;
关键词
MESOSCALE VARIABILITY; NORTH-ATLANTIC; PHYTOPLANKTON; PRODUCTIVITY; IMPACT; EDDY; SEA; CHLOROPHYLL; COMMUNITIES; CIRCULATION;
D O I
10.5194/bg-14-2877-2017
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
We present a systematic study of the differences generated by coupling the same ecological-biogeochemical model to a 1 degrees, coarse-resolution, and 1 = 6 degrees, eddy-permitting, global ocean circulation model to (a) biogeochemistry (e.g., primary production) and (b) phytoplankton community structure. Surprisingly, we find that the modeled phytoplankton community is largely unchanged, with the same phenotypes dominating in both cases. Conversely, there are large regional and seasonal variations in primary production, phytoplankton and zooplankton biomass. In the subtropics, mixed layer depths (MLDs) are, on average, deeper in the eddy-permitting model, resulting in higher nutrient supply driving increases in primary production and phytoplankton biomass. In the higher latitudes, differences in winter mixed layer depths, the timing of the onset of the spring bloom and vertical nutrient supply result in lower primary production in the eddy-permitting model. Counterintuitively, this does not drive a decrease in phytoplankton biomass but results in lower zooplankton biomass. We explain these similarities and differences in the model using the framework of resource competition theory, and find that they are the consequence of changes in the regional and seasonal nutrient supply and light environment, mediated by differences in the modeled mixed layer depths. Although previous work has suggested that complex models may respond chaotically and unpredictably to changes in forcing, we find that our model responds in a predictable way to different ocean circulation forcing, despite its complexity. The use of frameworks, such as resource competition theory, provides a tractable way to explore the differences and similarities that occur. As this model has many similarities to other widely used biogeochemical models that also resolve multiple phytoplankton phenotypes, this study provides important insights into how the results of running these models under different physical conditions might be more easily understood.
引用
收藏
页码:2877 / 2889
页数:13
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