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Nutrient distributions in the Gulf of Maine: An analysis of spatial and temporal patterns of dissolved inorganic nitrate and silicate.

机译:缅因湾的营养分布:溶解的无机硝酸盐和硅酸盐的时空分布图分析。

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摘要

While the Gulf of Maine has been historically well sampled relative to remote offshore regions, descriptions of the nutrient distributions and dynamics have provided only brief glimpses of restricted areas in space and time. The primary objectives of this study are to compile and evaluate the historical nutrient data within the region to determine the spatial and temporal variability of nutrient distributions, identify the environmental influences responsible for these patterns, and quantify the variability that exists within nutrient fluxes throughout the Gulf of Maine.;Within five distinct regions in the Gulf of Maine, average seasonal cycles of dissolved inorganic nitrogen are similar, although there is regionally variable timing and magnitude of both nitrate and satellite measured chlorophyll biomass. A seasonal cycle of nitrate exists at all depths, however the variability is greater interannually than seasonally at depths greater than 50m. Seasonal surface anomalies can be explained by the timing of the spring phytoplankton bloom, correlated with salinity anomalies, and even related to zooplankton populations. All localized regions and depths within the Gulf of Maine are positively correlated, suggesting the entire Gulf typically varies as a cohesive unit.;An objective analysis kriging interpolation generates a spatially explicit monthly climatology and identifies major features of the average nitrate concentrations in the water. This analysis also provides an objective measure of the historical sampling effort and indentifies locations and seasons lacking descriptive observations. A coupled nitrate-silicate box model for the Gulf of Maine shows that while nitrate is influenced heavily by offshore inputs, silicate has a dominant continental source. The historical data suggest biologically available nutrient fluxes can vary by as much as 50% annually and are highly dependent on outflows of Maine Intermediate Water. While the variability in nutrient concentrations is not the only factor determining biological productivity, these results show the possible influence of nutrient variability from a bottom-up trophic perspective within the Gulf of Maine.
机译:尽管缅因湾相对于偏远的近海地区在历史上得到了很好的采样,但是对营养物分布和动态的描述仅提供了时空有限区域的简要介绍。这项研究的主要目标是汇编和评估该区域内的历史养分数据,以确定养分分布的时空变化,确定造成这些模式的环境影响,并量化整个海湾养分通量内存在的变化。在缅因州海湾的五个不同区域中,尽管硝酸盐和卫星测得的叶绿素生物量在区域和时间上存在差异,但溶解的无机氮的平均季节性周期却相似。硝酸盐的季节性循环在所有深度都存在,但是在深度大于50m时,年际变化大于季节性。季节性表面异常可以通过春季浮游植物开花的时间来解释,其与盐度异常有关,甚至与浮游动物种群有关。缅因州海湾内的所有局部区域和深度都呈正相关,表明整个海湾地区通常以粘性单位变化。;客观分析克里金插值法产生了空间上明确的每月气候,并确定了水中平均硝酸盐浓度的主要特征。该分析还提供了历史采样工作的客观度量,并确定了缺乏描述性观测的位置和季节。缅因州海湾的硝酸盐-硅酸盐盒子耦合模型表明,尽管硝酸盐受到海上投入的严重影响,但硅酸盐却是主要的大陆来源。历史数据表明,可生物利用的养分通量每年可能变化多达50%,并且高度依赖于缅因州中级水的流出。尽管营养物浓度的变化不是决定生物生产力的唯一因素,但这些结果从缅因湾自下而上的营养角度显示了营养物变化的可能影响。

著录项

  • 作者

    Rebuck, Nathan D.;

  • 作者单位

    The University of Maine.;

  • 授予单位 The University of Maine.;
  • 学科 Chemical Oceanography.
  • 学位 Ph.D.
  • 年度 2011
  • 页码 194 p.
  • 总页数 194
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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