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Remote sensing of size structure of phytoplankton communities using optical properties of the Chukchi and Bering Sea shelf region

机译:利用楚科奇和白令海陆架区的光学特性遥感浮游植物群落的大小结构

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Recent ocean warming and subsequent sea ice decline resulting from climatechange could affect the northward shift of the ecosystem structure in theChukchi Sea and Bering Sea shelf region (Grebmeier et al., 2006b). The sizestructure of phytoplankton communities provides an index of trophic levelsthat is crucial to understanding the mechanisms underlying such ecosystemchanges and their implications for the future. This study proposes a newocean color algorithm for deriving this characteristic by using the region'soptical properties. The size derivation model (SDM) estimates thephytoplankton size index FL on the basis of size-fractionatedchlorophyll-a (chl-a) using the light absorption coefficient of phytoplankton,aph(λ), and the backscattering coefficient of suspended particlesincluding algae, bbp(λ). FL was defined as the ratio of algal biomassattributed to cells larger than 5 μm to the total. It was expressed bya multiple regression model using the aph(λ) ratio,aph(488)/aph(555), which varies with phytoplankton pigmentcomposition, and the spectral slope of bbp(λ), γ, which is an index of themean suspended particle size. A validation study demonstrated that 69% ofunknown data are correctly derived within FL range of ±20%. Thespatial distributions of FL for the cold August of 2006 and the warmAugust of 2007 were compared to examine application of the SDM to satelliteremote sensing. The results suggested that phytoplankton size was responsiveto changes in sea surface temperature. Further analysis of satellite-derivedFL values and other environmental factors can advance our understandingof ecosystem structure changes in the shelf region of the Chukchi and BeringSeas.
机译:气候变化导致的近期海洋变暖和随后的海冰减少可能会影响楚科奇海和白令海陆架区生态系统结构的北移(Grebmeier等,2006b)。浮游植物群落的大小结构提供了营养水平的指数,这对于理解这种生态系统变化的潜在机制及其对未来的影响至关重要。本研究提出了一种新的海洋颜色算法,通过利用该区域的光学特性来推导该特征。大小推导模型(SDM)根据大小分级的叶绿素- a (chl- a)估算浮游植物大小指数 F L )使用浮游植物的光吸收系数 a ph (λ)和悬浮颗粒(包括藻类, b )的反向散射系数 bp (λ)。 F L 定义为归因于大于5μm的细胞的藻类生物质占总数的比例。它是通过多元回归模型使用 a ph (λ)比, a ph (488)/来表示的 a ph (555),随浮游植物色素成分和 b bp (λ)的光谱斜率而变化,γ,这是固有悬浮粒径的指标。一项验证研究表明,在 F L 的±20%范围内正确得出了69%的未知数据。比较2006年8月寒冷和2007年8月温暖的 F L 的空间分布,以检验SDM在卫星遥感中的应用。结果表明,浮游植物的大小对海表温度的变化有响应。对卫星衍生的 F L 值和其他环境因素的进一步分析可以增进我们对楚科奇海和白令海陆架区域生态系统结构变化的理解。

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