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Controls on ocean productivity and air-sea carbon flux: An adjoint model sensitivity study

机译:海洋生产力和海气碳通量的控制:伴随模型敏感性研究

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[1] We use the adjoint of a global model of coupled oceanic cycles of carbon, phosphorus and iron to comprehensively and efficiently map the sensitivity of global biological productivity and air-sea carbon fluxes to local perturbations of the atmospheric iron source sustained for a decade or more. Modeled productivity and carbon flux are found to be most sensitive to enhanced iron sources in high nitrate low chlorophyll regions. The relative response of productivity to an enhanced iron source is greatest in the Equatorial Pacific. Although surface macro-nutrients are more abundant in the Southern Ocean, nutrient utilization here is critically regulated by light limitation. Our results differ from those of previous studies which imposed depletion of surface nutrients and ignore the availability of light. However, the enhancement of oceanic carbon storage per unit increase in productivity is strongest in the high latitude oceans.
机译:[1]我们使用碳,磷和铁耦合海洋循环的全球模型的伴随物,全面有效地绘制了全球生物生产力和气海碳通量对十年来持续存在的大气铁源局部扰动的敏感性的图。或者更多。在高硝酸盐含量低的叶绿素区域中,模型化的生产率和碳通量被发现对增强铁源最为敏感。在赤道太平洋地区,生产力对铁源增强的相对响应最大。尽管南大洋的表层宏观营养素含量较高,但这里的营养素利用受到光限制的严格控制。我们的结果与以前的研究不同,后者的研究表明表面营养物质被消耗掉,而忽略了光的可用性。但是,在高纬度海洋中,单位生产力的海洋碳存储量增加的幅度最大。

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