北洪堡洋流系统模型初级生产率的时空变化和驱动因素

IF 3.1 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Ocean Modelling Pub Date : 2024-03-15 DOI:10.1016/j.ocemod.2024.102347
Rodrigo Mogollón , François Colas , Vincent Echevin , Jorge Tam , Dante Espinoza-Morriberón
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引用次数: 0

摘要

采用物理-生物地球化学耦合模式探索了北洪堡洋流系统(NHCS)初级生产率的时空动态。从南纬 3 度到 18 度,距海岸 250 公里的沿岸带是一个高产上升流区,地表初级生产率平均值为 2.5 摩尔碳米/年。相应地,透光层内的平均垂直整合 PP 值为 13 摩尔碳米/年。在这种情况下,夏季成为生产力的高峰期,年产量为 18 摩尔碳米,而冬季则是生产力最低的时期,年产量为 9 摩尔碳米。我们的研究表明,地表光合产物的变化主要受地表叶绿素和浮游植物生物量(主要是硅藻)变化的驱动,其次是光合有效辐射(PAR)水平的变化。在夏季,这三个驱动因素造成了地表光合产物的大幅正向异常。然而,上升流-顺风的减弱导致营养物质供应减少,对地表 PP 率产生了轻微的负面影响。然而,在温暖季节,这种下降被正热效应所抵消。与此相反,在冬季,由于叶绿素浓度垂直重新分布到更深的混合层,表层叶绿素浓度显著下降,从而大大降低了表层 PP。此外,PAR 水平和生物量浓度的降低也会产生类似的影响,进一步导致冬季地表 PP 率的降低。在水深 20 米处,PP 的变化主要受 PAR 和叶绿素浓度的对立影响。PAR 全年都遵循升温和降温的季节性循环,而叶绿素驱动的异常则受混合层内垂直稀释效应的影响,呈现出与地表异常相反的模式。总之,这项研究为了解世界上最富饶的海洋区域之一不同深度的光合作用动态所受驱动因素的复杂相互作用提供了宝贵的见解。
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Spatiotemporal variability and drivers of modeled primary production rates in the Northern Humboldt Current System

A coupled physical-biogeochemical model was employed to explore the spatiotemporal dynamics of primary production (PP) rates within the Northern Humboldt Current System (NHCS). The coastal zone spanning 250 km from the shore, from 3°to 18°S, stands out as a highly productive upwelling region, exhibiting an average surface PP value of 2.5 mol C m−3 yr−1. Correspondingly, the average vertically integrated PP within the euphotic layer amounts to 13 mol C m−2 yr−1. In this context, summer emerges as the peak of productivity, yielding 18 mol C m−2 yr−1, while winter signifies the period of least productivity, with 9 mol C m−2 yr−1. Our study revealed that surface PP variability is primarily driven by changes in surface chlorophyll and phytoplanktonic biomass (mainly diatoms), followed by changes in photosynthetically active radiation (PAR) levels. During summertime, these three drivers contribute to substantial positive anomalies in surface PP. However, the reduction in nutrient availability resulting from weakened upwelling-favorable winds has a slight negative impact on surface PP rates. Yet, this decline is offset by a positive thermal effect during the warmer season. In contrast, during the winter season, a significant decrease in surface chlorophyll concentrations due to a vertical redistribution into a deeper mixed layer significantly diminishes surface PP. Furthermore, the reduction in both PAR levels and biomass concentrations has a comparable effect, further contributing to the decrease in surface PP rates during wintertime. At a depth of 20 m, changes in PP are primarily driven by variations between the opposing influences of PAR and chlorophyll concentrations. While PAR adheres to the seasonal cycle of warming and cooling throughout the year, chlorophyll-driven anomalies exhibit an inverse pattern to those at the surface, influenced by the vertical dilution effect within the mixed layer. Overall, this study provides valuable insights into the complex interplay of drivers that govern PP dynamics across various depths within one of the world’s most productive marine regions.

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来源期刊
Ocean Modelling
Ocean Modelling 地学-海洋学
CiteScore
5.50
自引率
9.40%
发文量
86
审稿时长
19.6 weeks
期刊介绍: The main objective of Ocean Modelling is to provide rapid communication between those interested in ocean modelling, whether through direct observation, or through analytical, numerical or laboratory models, and including interactions between physical and biogeochemical or biological phenomena. Because of the intimate links between ocean and atmosphere, involvement of scientists interested in influences of either medium on the other is welcome. The journal has a wide scope and includes ocean-atmosphere interaction in various forms as well as pure ocean results. In addition to primary peer-reviewed papers, the journal provides review papers, preliminary communications, and discussions.
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