Brewin Robert J W, Dall'Olmo Giorgio, Sathyendranath Shubha, Hardman-Mountford Nick J
Plymouth Marine Laboratory (PML), Prospect Place, The Hoe, Plymouth PL1 3DH, UK.
Opt Express. 2012 Jul 30;20(16):17632-52. doi: 10.1364/OE.20.017632.
Using an extensive database of in situ observations we present a model that estimates the particle backscattering coefficient as a function of the total chlorophyll concentration in the open-ocean (Case-1 waters). The parameters of the model include a constant background component and the chlorophyll-specific backscattering coefficients associated with small (<20 μm) and large (>20 μm) phytoplankton. The new model performed with similar accuracy when compared with a traditional power-law function, with the additional benefit of providing information on the role of phytoplankton size. The observed spectral-dependency (γ) of model parameters was consistent with past observations, such that γ associated with the small phytoplankton population was higher than that of large phytoplankton. Furthermore, γ associated with the constant background component suggests this component is likely attributed to submicron particles. We envisage that the model would be useful for improving Case-1 ocean-colour models, assimilating light into multi-phytoplankton ecosystem models and improving estimates of phytoplankton size structure from remote sensing.
利用一个广泛的原位观测数据库,我们提出了一个模型,该模型可根据开阔海洋(一类水体)中的总叶绿素浓度估算颗粒后向散射系数。该模型的参数包括一个恒定的背景成分以及与小型(<20μm)和大型(>20μm)浮游植物相关的叶绿素特定后向散射系数。与传统的幂律函数相比,新模型的表现具有相似的准确性,此外还能提供有关浮游植物大小作用的信息。模型参数的观测光谱依赖性(γ)与过去的观测结果一致,即与小型浮游植物群体相关的γ高于大型浮游植物的γ。此外,与恒定背景成分相关的γ表明该成分可能归因于亚微米颗粒。我们设想该模型将有助于改进一类海洋颜色模型、将光同化到多浮游植物生态系统模型中以及改进从遥感数据估算浮游植物大小结构的方法。