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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Seasonal variability in satellite-measured surface chlorophyll in the Patagonian Shelf
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Seasonal variability in satellite-measured surface chlorophyll in the Patagonian Shelf

机译:巴塔哥尼亚大陆架卫星测量的表面叶绿素的季节变化

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Six years (January 1998-December 2003) of SeaWiFS ocean color satellite data are used to estimate monthly climatological means and to present the near-surface chlorophyll-a seasonal evolution in the Patagonian Shelf. The southern part of the shelf presents elevated chlorophyll concentrations from spring through autumn, while the northern part shows three regions with particular characteristics. The external region, bordering the 200 in isobath, presents elevated concentrations from spring through autumn supported by the nutrient-rich waters from the Malvinas (Falkland) Current. The central region presents a typical pattern of temperate regions, characterized by two well-defined maxima, a stronger spring bloom and a weaker fall bloom, and low chlorophyll values throughout summer (scarce availability of nutrients) and winter (light being the limiting factor). Even though the displacement direction of the spring and fall blooms do not agree with previous information reported in the literature, they are interpreted based on the heat exchange in the air-sea interface that controls the development and erosion of the seasonal thermocline. Finally, the coastal region presents less-marked seasonal variability and isolated small areas with elevated concentrations associated with frontal areas are observed. The spatial mean chlorophyll evolution, averaged over the whole shelf (less than 200 in depth), shows a marked annual cycle with high values from spring to autumn, supporting the importance of frontal regions as a fertilization mechanism. An increasing trend in chlorophyll concentrations, within the 6 years analyzed here (in the order of 23%), is apparent based on an increasing of the maximum annual values. From the comparison with in situ data it can be concluded that satellite information reproduces the spatial patterns of chlorophyll fields obtained from more classical data, while differences exist in absolute values obtained from both methodologies. (C) 2006 Elsevier Ltd. All rights reserved.
机译:SeaWiFS六年(1998年1月至2003年12月)的海洋彩色卫星数据被用于估算每月的气候变化手段并呈现巴塔哥尼亚大陆架中近地表叶绿素的季节性变化。架子的南部从春季到秋季呈现出较高的叶绿素浓度,而北部则显示出三个具有特定特征的区域。外部区域与等压线中的200个边界接壤,从春季到秋季,在马尔维纳斯(福克兰)洋流的营养丰富的水域的支持下,浓度升高。中部地区呈典型的温带地区格局,其特征是两个明确的最大值,春季开花较强,秋季开花较弱,整个夏季(营养物质缺乏)和冬季(光是限制因素)的叶绿素值较低。 。即使春季和秋季水华的位移方向与文献中报道的先前信息不一致,也可以根据控制季节性温跃层的发展和侵蚀的海气界面中的热交换进行解释。最后,沿海地区的季节变化不那么明显,并且观察到孤立的小区域与额叶相关的浓度升高。空间平均叶绿素的演变,在整个陆架(深度小于200)上平均,显示出明显的年循环,从春季到秋季都有很高的值,这支持了额叶区域作为施肥机制的重要性。基于最大年值的增加,在此处分析的6年内,叶绿素浓度呈上升趋势(约为23%)。从与原位数据的比较可以得出结论,卫星信息再现了从更经典的数据中获得的叶绿素场的空间格局,而从两种方法获得的绝对值却存在差异。 (C)2006 Elsevier Ltd.保留所有权利。

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