Chromophoric dissolved organic matter dynamics revealed through the optimization of an optical–biogeochemical model in the northwestern Mediterranean Sea

Eva Álvarez, G. Cossarini, A. Teruzzi, J. Bruggeman, Karsten Bolding, S. Ciavatta, Vincenzo Vellucci, F. D’Ortenzio, David Antoine, P. Lazzari
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Abstract

Abstract. Chromophoric dissolved organic matter (CDOM) significantly contributes to the non-water absorption budget in the Mediterranean Sea. The absorption coefficient of CDOM, aCDOM(λ), is measurable in situ and can be retrieved remotely, although ocean-colour algorithms do not distinguish it from the absorption of detritus. These observations can be used as indicators for the concentration of other relevant biogeochemical variables in the ocean, e.g. dissolved organic carbon. However, our ability to model the biogeochemical processes that determine CDOM concentrations is still limited. Here we propose a novel parameterization of the CDOM cycle that accounts for the interplay between the light- and nutrient-dependent dynamics of local CDOM production and degradation, as well as its vertical transport. The parameterization is included in a one-dimensional (1D) configuration of the Biogeochemical Flux Model (BFM), which is here coupled to the General Ocean Turbulence Model (GOTM) through the Framework for Aquatic Biogeochemical Models (FABM). Here the BFM is augmented with a bio-optical component that resolves spectrally the underwater light transmission. We run this new GOTM-(FABM)-BFM configuration to simulate the seasonal aCDOM(λ) cycle at the deep-water site of the Bouée pour l'acquisition de Séries Optiques à Long Terme (BOUSSOLE) project in the northwestern Mediterranean Sea. Our results show that accounting for both nutrient and light dependence of CDOM production improves the simulation of the seasonal and vertical dynamics of aCDOM(λ), including a subsurface maximum that forms in spring and progressively intensifies in summer. Furthermore, the model consistently reproduces the higher-than-average concentrations of CDOM per unit chlorophyll concentration observed at BOUSSOLE. The configuration, outputs, and sensitivity analyses from this 1D model application will be instrumental for future applications of BFM to the entire Mediterranean Sea in a three-dimensional configuration.
通过优化地中海西北部的光学-生物地球化学模型揭示色相溶解有机物的动态变化
摘要。色度溶解有机物(CDOM)对地中海的非水吸收预算有重大贡献。CDOM的吸收系数(aCDOM(λ))可在现场测量,也可远程检索,尽管海洋颜色算法无法将其与碎屑的吸收区分开来。这些观测结果可作为海洋中其他相关生物地球化学变量(如溶解有机碳)浓度的指标。然而,我们为决定 CDOM 浓度的生物地球化学过程建模的能力仍然有限。在此,我们提出了一种新的 CDOM 循环参数化方法,该方法考虑了依赖于光和营养物质的本地 CDOM 生成和降解动态及其垂直传输之间的相互作用。该参数化包含在生物地球化学通量模型(BFM)的一维(1D)配置中,该模型通过水生生物地球化学模型框架(FABM)与一般海洋湍流模型(GOTM)耦合。在这里,BFM 增加了一个生物光学组件,从光谱上解决了水下光传输问题。我们在地中海西北部的 Bouée pour l'acquisition de Séries Optiques à Long Terme(BOUSSOLE)项目深水站点运行这种新的 GOTM-(FABM)-BFM 配置来模拟 aCDOM(λ)的季节性循环。我们的研究结果表明,考虑到 CDOM 产量的营养和光照依赖性,可以改进对 aCDOM(λ) 的季节和垂直动态的模拟,包括在春季形成并在夏季逐渐增强的次表层最大值。此外,该模式一致地再现了在布苏勒观测到的每单位叶绿素浓度中 CDOM 的浓度高于平均值的情况。该一维模型的配置、输出和敏感性分析将有助于今后将 BFM 应用于整个地中海的三维配置。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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