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Spatial and temporal variation of particulate organic carbon in the PN section of East China Sea

机译:东海PN区颗粒有机碳的时空变化。

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摘要

Variations of the particulate organic carbon and nitrogen (POC/PN) along the PN section in the East China Sea (ECS) were examined based on POC/PN data obtained in September 2002. A comparison with others work indicates that POC is the highest in summer, followed by autumn and spring, and the lowest in winter. Generally, POC concentration decreases seawards, and the in situ productivity in September plays an important role in POC distribution. POC in the PN section is composed of terrestrial, resuspended, in situ produced carbon and carbon originated from the Kuroshio waters. The Changjiang River effects the ECS in the PN section, but the influence is mainly minimiged beyond 123.5° E because of barrier effect. The impact of Kuroshio subsurface water (KSSW) over shelf break can also effect POC distribution, with high POC concentration there.
机译:根据2002年9月获得的POC / PN数据,对东海PN段沿线的颗粒状有机碳和氮(POC / PN)的变化进行了研究。与其他工作的比较表明,POC含量最高。夏季,其次是秋季和春季,冬季最低。通常,POC浓度会向海减少,9月份的原位生产力在POC分布中起着重要作用。 PN区的POC由陆地的,重悬的,原位产生的碳和源自黑潮水域的碳组成。长江在PN区影响ECS,但由于屏障效应,影响主要是在123.5°E以东微移。黑潮地下水(KSSW)对架子破裂的影响也会影响POC的分布,因为那里的POC浓度很高。

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