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Contrasting correlation patterns between environmental factors and chlorophyll levels in the global ocean

机译:全球海洋中环境因素与叶绿素水平之间的对比相关模式

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In this study we analyze large-scale satellite-derived data using generalized additive models to characterize the global correlation patterns between environmental forcing and marine phytoplankton biomass. We found systematic differences in the relationships between key environmental drivers (temperature, light, and wind) and ocean chlorophyll in the subtropical/tropical and temperate oceans. For the subtropical/tropical and equatorial oceans, the chlorophyll generally declined with increasing temperature and light, while in temperate oceans, chlorophyll was best explained by bell-shaped or positive functions of temperature and light. The relationship between chlorophyll and wind speed is generally positive in low-latitude oceans and bell shaped in temperate oceans. Our analyses also demonstrated strong and geographically consistent positive autoregressive effects of chlorophyll from 1 month to the next and negative autoregressive effects for measurements 2 months apart. These findings imply possibly different regional phytoplankton responses to environmental forcing, suggesting that future environmental change could affect the tropical and temperate upper ocean chlorophyll levels differently.
机译:在这项研究中,我们使用广义加性模型分析了大规模的卫星数据,以表征环境强迫与海洋浮游生物量之间的全球相关性模式。我们发现在亚热带/热带和温带海洋中,关键环境驱动因素(温度,光和风)与海洋叶绿素之间的关系存在系统差异。对于亚热带/热带和赤道海洋,叶绿素通常随着温度和光照的增加而下降,而在温带海洋中,叶绿素最好通过温度和光照的钟形或正函数来解释。在低纬度海洋中,叶绿素与风速之间的关系通常为正,而在温带海洋中则呈钟形。我们的分析还表明,从1个月到下个月,叶绿素具有强的且在地理上一致的正自回归效应,而相隔2个月的测量则为负自回归效应。这些发现可能暗示了区域浮游植物对环境强迫的不同反应,表明未来的环境变化可能对热带和温带上层海洋叶绿素水平产生不同的影响。

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