Global Estimates of Particulate Organic Carbon Concentration From the Surface Ocean to the Base of the Mesopelagic

被引:0
作者
Fox, James [1 ]
Behrenfeld, Michael J. [2 ]
Halsey, Kimberly H. [1 ]
Graff, Jason R. [2 ]
机构
[1] Oregon State Univ, Dept Microbiol, Corvallis, OR 97331 USA
[2] Oregon State Univ, Dept Bot & Plant Pathol, Corvallis, OR USA
基金
美国国家航空航天局;
关键词
biological carbon pump; particulate organic carbon; BGC-Argo; mesopelagic; SOUTHERN-OCEAN; EXPORT; FLUX; ATLANTIC; MODEL; SEQUESTRATION; ATTENUATION; VARIABILITY; SATELLITE; MATTER;
D O I
10.1029/2024GB008149
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The gravitational settling of organic particles from the surface to the deep ocean is an important export pathway and one of the largest components of the ocean carbon pump. The strength and efficiency of the gravitational pump are often measured using metrics reliant on reference depths and empirical formulations that parameterize the relationship between depth and the flux or concentration of particulate organic carbon (POC). Here, BGC-Argo profiles were used to identify the isolume where POC concentration, [POC], starts to decline, revealing attenuation trends below this isolume that are remarkably consistent across the global ocean. We developed a simple empirical approach that uses observations from the first optical depth to predict [POC] from the surface ocean to the base of the mesopelagic (1,000 m), allowing assessments of spatial and temporal variability in gravitational pump efficiencies. We find that rates of [POC] attenuation are high in areas of high biomass and low in areas of low biomass, supporting the view that bloom events sometimes result in a relatively weak deep biological pump that is characterized by low transfer efficiency to the base of the mesopelagic. Our isolume-based attenuation model was applied to satellite data to yield the first remote sensing-based estimate of integrated global POC stock of 3.02 Pg C over the top 1,000 m, with an uncertainty of 0.69 Pg C. Of this total stock, approximately 1.02 Pg was located above the reference isolume where [POC] begins to attenuate. Float profiles of POC concentration reveal globally consistent trends in attenuation for depths below an isolume of 0.451 mol photons m-2 d-1 An empirical modeling approach can be used to estimate POC concentration from the surface ocean to the base of the mesopelagic (1,000 m) The new approach enables the assessment of remineralization trends and standing stocks of POC concentration across the global ocean
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页数:16
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