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首页> 外文期刊>Marine ecology progress series >Interannual variability in phytoplankton blooms and plankton productivity over the Nova Scotian Shelf and in the Gulf of Maine
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Interannual variability in phytoplankton blooms and plankton productivity over the Nova Scotian Shelf and in the Gulf of Maine

机译:新斯科舍大陆架和缅因州湾浮游植物开花和浮游生物生产力的年际变化

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摘要

A 1D ecosystem model, driven by surface heat and wind forcing and relaxed toward observed salinity profiles, was applied to simulate the interannual and decadal scale variability of phytoplankton blooms and plankton production from 1984 to 2007 in the Nova Scotian Shelf (NSS) and Gulf of Maine (GoM) region. The model captured the mean observed timing and magnitude of the spring (SPB) and fall phytoplankton bloom (FPB) in both systems, as well as observed interannual variations in SPB peak timing. Model simulations for both the GoM and NSS exhibited marked interannual variability in SPB and FPB timing (±2 to 3 wk) and magnitude (up to ~1 mg chlorophyll m~(-3)). Earlier SPBs and delayed FPBs are linked to enhanced water column stability generated by less saline surface water or sharper salinity gradients over the top 50 m of the water column. The modeled variation in annual primary productivity, mesozooplankton productivity, and particle export flux was modest (<10% of the mean). Years with high primary production were weakly associated with early SPBs (GoM: r = -0.205; NSS: r = -0.51), but there was no significant relationship with water column stability. This suggests that variation in annual productivity in the GoM and NSS reflects a combination of variation in light limitation (which is alleviated by increased water column stability) and nutrient limitation (which is exacerbated by increased water column stability) that offset and are of near equal importance when averaged over the year. Interannual variations in fisheries production due to changes in annual productivity are thus likely secondary to profound shifts in fisheries recruitment and production that have been linked to variations in SPB and FPB timing.
机译:利用一维生态系统模型,该模型由地表热和风强迫驱动,并向观察到的盐度分布方向放松,用于模拟1984年至2007年新斯科舍大陆架(NSS)和墨西哥湾的浮游植物大花和浮游生物产量的年际和年代际尺度变化。缅因州(GoM)地区。该模型捕获了两个系统中春季(SPB)和浮游植物降落(FPB)的平均观测时间和幅度,以及观测到的SPB峰值时间的年际变化。 GoM和NSS的模型模拟均显示SPB和FPB时序(±2至3 wk)和幅度(高达〜1 mg叶绿素m〜(-3))的年际变化显着。较早的SPB和延迟的FPB与水柱顶部50 m上较少的盐分地表水或盐分梯度较大而产生的增强的水柱稳定性有关。年初级生产力,中层浮游生物生产力和颗粒出口通量的模型变化很小(小于平均值的10%)。初级生产量高的年份与早期SPB弱相关(GoM:r = -0.205; NSS:r = -0.51),但与水柱稳定性没有显着关系。这表明GoM和NSS的年生产力变化反映了光限制(通过增加水柱稳定性而减轻)和养分限制(通过增加水柱稳定性而加剧)的变化的组合,其抵消并接近相等一年平均时的重要性。因此,由于年生产力的变化,渔业生产的年际变化很可能是继渔业招募和生产的重大变化之后的继发性变化,而这种变化与SPB和FPB时间的变化有关。

著录项

  • 来源
    《Marine ecology progress series》 |2011年第28期|p.105-118|共14页
  • 作者单位

    Key Lab of Science and Engineering for Marine Ecological Environment, The First Institute of Oceanography, SOA,Qingdao 266061, PR China,Department of Biology, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA;

    Department of Biology, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA,Marine Ecosystem and Environment Laboratory, College of Marine Sciences, Institutes for Marine Sciences, Shanghai Ocean University, Shanghai 201306, PR China;

    NOAA Geophysical Fluid Dynamics Laboratory, Princeton University Forrestal Campus, Princeton, New Jersey 08540, USA;

    Department of Geosciences, Princeton University, Princeton, New Jersey 08540, USA;

    Key Lab of Science and Engineering for Marine Ecological Environment, The First Institute of Oceanography, SOA,Qingdao 266061, PR China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    phytoplankton bloom; interannual variability; modeling; nova scotian shelf; gulf of maine;

    机译:浮游植物开花;年际变化;建模;新斯科舍陆架;缅因州海湾;

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