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Does horizontal mixing explain phytoplankton dynamics?

机译:水平混合能解释浮游植物的动态吗?

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摘要

The modern era of biological oceanography arguably began in 1978 with the successful launch of the Coastal Zone Color Scanner on the Nimbus 7 satellite. Although limited by today's standards, the Coastal Zone Color Scanner provided the first glimpse of the complex, beautiful, and difficult-to-sample interactions between single-celled phytoplankton and the turbulent mixing of the surface ocean. In the intervening decades, oceanographers have made tremendous advances, with more and better ocean color sensors such as the Sea-viewing Wide Field-of-view Sensor, Moderate Resolution Imaging Spectro-radiometer, and Medium Resolution Imaging Spectrometer. The PNAS report by d'Ovidio et al. (1) shows us how much further we need to go and provides a glimpse into the true complexity of the surface ocean and the mechanisms driving this ecological landscape.
机译:可以说,现代海洋生物学时代始于1978年,当时Nimbus 7卫星成功发射了沿海区彩色扫描仪。尽管受当今标准的限制,但沿海地区彩色扫描仪提供了单细胞浮游植物与地表海洋湍流混合之间复杂,美观且难以采样的相互作用的第一印象。在过去的几十年中,海洋学家取得了长足的进步,拥有越来越多的海洋颜色传感器,例如海景宽视场传感器,中分辨率成像光谱辐射仪和中分辨率成像光谱仪。 d'Ovidio等人的PNAS报告。 (1)向我们展示了我们还需要走多远,并且可以窥见到地表海洋的真正复杂性以及驱动这种生态景观的机制。

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