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首页> 外文期刊>Frontiers in Marine Science >Trends in Primary Production in the Canary Current Upwelling System—A Regional Perspective Comparing Remote Sensing Models
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Trends in Primary Production in the Canary Current Upwelling System—A Regional Perspective Comparing Remote Sensing Models

机译:金丝雀流上升系统中初级生产的趋势-比较遥感模型的区域视角

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After Andrew (Bakun, 1990) formulated his hypothesis of upwelling intensification caused by increasing global warming, contradictory results have been published on whether primary productivity is increasing or decreasing in Eastern Boundary Upwelling Ecosystems (EBUE). The present work is focused in comparing three net primary production (NPP) models -the VGPM (Vertically Generalized Production Model), the Eppley-VGPM and the CbPM (Carbon-based Production Model)- in the Canary Current (CanC) EBUE during the 1998-2015 period, making use of both SeaWiFS (Sea-viewing Wide Field-of-view Sensor) and MODIS (MODerate-resolution Imaging Spectroradiometer) derived data. We looked for the first time for seasonal to interannual trends of NPP under a regional perspective, with the aim of searching for temporal patterns that could support or reject the intensification hypothesis. According to previous studies based on the seasonality of the upwelling regime, the CanC EBUE was divided into three subregions: a seasonal upwelling zone (SUZ; 13-20oN), a permanent upwelling zone (PUZ; 20-26oN) and a weak permanent upwelling zone (WPUZ; 26-33oN). Our analyses do not show significant increasing trends in NPP with any of the productivity models used, challenging Bakun’s hypothesis. Nevertheless, differences in the output of the models are important, both at regional and subregional scales, questioning the accuracy of the models. The comparison made in this work clearly shows the disagreements between some of the best-known NPP models and calls for a validation effort in this region. Contrary to the open-ocean, temperature trends show significant decreases in certain areas over the shelf waters, which might indicate an increase of cool, upwelled waters in those regions. Seasonal to decadal anomalies of NPP and sea-surface temperature (SST) are estimated and analyzed in relation to selected climate indices, yielding only significant correlations between SST and the North Atlantic Oscillation (NAO) indices.
机译:在安德鲁(Bakun,1990年)提出由全球变暖加剧引起的上升流加剧的假说之后,有关东部边界上升流生态系统(EBUE)的初级生产力是增加还是减少的矛盾结果已经发表。本工作着重于比较三大净初级生产(NPP)模型-VGPM(垂直通用生产模型),Eppley-VGPM和CbPM(基于碳的生产模型)- 1998年至2015年期间,利用了SeaWiFS(海景宽视场传感器)和MODIS(中等分辨率成像光谱仪)得出的数据。我们首次从区域角度探讨了NPP的季节性至年际趋势,目的是寻找可能支持或否定集约化假设的时间模式。根据先前基于上升流体制的季节性的研究,CanC EBUE分为三个子区域:季节性上升流带(SUZ; 13-20oN),永久上升流带(PUZ; 20-26oN)和弱的永久上升流区域(WPUZ; 26-33oN)。我们的分析没有显示使用任何一种生产率模型的NPP的显着增长趋势,这对Bakun的假设提出了挑战。然而,在区域和次区域范围内,模型输出的差异很重要,这对模型的准确性提出了质疑。这项工作进行的比较清楚地表明了一些最著名的NPP模型之间的分歧,并要求对该地区进行验证。与开放海洋相反,温度趋势显示了架子水域某些区域的显着下降,这可能表明这些地区的凉爽上升水域有所增加。相对于选定的气候指数,估计和分析了NPP的季节到年代际异常和海面温度(SST),仅在SST和北大西洋涛动(NAO)指数之间产生了显着的相关性。

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