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Satellite bio-optical and altimeter comparisons of phytoplankton blooms induced by natural and artificial iron addition in the Gulf of Alaska

机译:satellite bio-optical and altimeter comparisons of phytoplankton blooms induced by natural and artificial iron addition in the Gulf of alaska

摘要

An iron fertilization experiment conducted during the summer of 2012 dumped over 100 tons of an ironcontaining substance into surface waters of a Haida eddy in the eastern North Pacific to stimulate a large phytoplankton bloom. Announced as a privately funded ocean fertilization effort to increase salmon returns, it attracted considerable press coverage, caused much public controversy and has been widely denounced by the science community. Here, we use available satellite bio-optical measurements from the MODIS/Aqua instrument and AVISO altimeter dynamic height data to examine the timing, magnitude and extent of this artificial iron fertilization experiment, comparing it with natural fertilization events such as volcanic ash deposition and mesascale eddy transport in the Gulf of Alaska. With respect to other Haida eddies over the past 10 years, this event produced the highest chlorophyll concentrations observed late (>400 days) in eddy life history, produced the strongest bloom ever observed in an eddy in late-summer and induced this late-summer bloom earlier in the season than any other eddy. With respect to the local area of the fertilization, this experiment induced the most intensive phytoplanlcton bloom of the past 10 years, similar to 2x stronger than that caused by Kasatochi volcano in 2008, similar to 5 x that typically observed in the region, including any induced by passing eddies of previous years. Due to its limited spatial and temporal scales, however, estimated total annual carbon drawdown over the Gulf of Alaska by this experiment is one order of magnitude smaller than the Kasatochi volcano and mesoscale Haida eddies. The target eddy followed a path typical of previous Haida eddies, but with relatively weak dynamic height and rotational circulation. Satellite-based calculations also suggest that only a small fraction of the dumped iron might have been taken up by phytoplankton. The extent to which this localized experiment may impact higher trophic levels such as salmon remains uncertain. (c) 2014 Elsevier Inc. All rights reserved.
机译:2012年夏季进行的铁肥实验将100吨以上的含铁物质倾倒到北太平洋东部海达涡流的地表水中,以刺激浮游植物的大量繁殖。作为一项私人投资的海洋施肥措施,旨在增加鲑鱼的回报,这项措施被宣布,引起了媒体的广泛报道,引起了许多公众争议,并已被科学界广泛谴责。在这里,我们使用来自MODIS / Aqua仪器和AVISO高度计动态高度数据的可用卫星生物光学测量结果来检查此人工铁施肥实验的时间,幅度和程度,并将其与自然施肥事件(如火山灰沉积和中尺度)进行比较阿拉斯加湾的涡流运输。对于过去10年中的其他Haida涡流,此事件产生了在涡流生命历史中后期(> 400天)观察到的最高叶绿素浓度,在夏末的涡流中产生了有史以来观察到的最强的花开并诱导了这种夏末。比任何其他涡旋更早地开花。就施肥区域而言,该实验诱发了过去10年中最密集的浮游植物开花,比2008年Kasatochi火山造成的浮游植物强2倍,类似于该地区通常观测到的5倍,包括是由前几年的涡流引起的。但是,由于其时空尺度有限,该实验估计的阿拉斯加湾年总碳排放量比Kasatochi火山和中型海达涡流小一个数量级。目标涡流遵循先前海达涡流的典型路径,但动态高度和旋转循环相对较弱。基于卫星的计算还表明,浮游植物可能只吸收了一部分废铁。这项本地化试验可​​能影响诸如鲑鱼等较高营养水平的程度仍不确定。 (c)2014 Elsevier Inc.保留所有权利。

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    Xiu P; Thomas AC; Chai F;

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