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首页> 外文期刊>Journal of Marine Science and Engineering >Inter-Annual Variability of the Seawater Light Absorption in Surface Layer of the Northeastern Black Sea in Connection with Hydrometeorological Factors
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Inter-Annual Variability of the Seawater Light Absorption in Surface Layer of the Northeastern Black Sea in Connection with Hydrometeorological Factors

机译:东北黑海表层海水光吸收的年际变化与水文气象因素的关系

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Data on the light absorption by seawater and its components are needed in many theoretical and practical aspects of marine science and engineering. However, up to now, there is a lack of such data for the northeastern part of the Black Sea. This article presents the data on light absorption measured by a portable integrated cavity absorption meter (ICAM) spectrophotometer in the Gelendzhik region of the Black Sea during field studies in June 2017 and 2018, together with other bio-optical and oceanographic data from in situ measurements and satellite observations. In 2018, the elevated values of the colored dissolved organic matter (CDOM) absorption in the surface layer were observed concurrently with high values of salinity, contradicting the idea of river runoff being the main CDOM source. The vertical profiles of salinity differed in 2017 and 2018, especially in shallow waters; in the upper layer, the salinity increased from 17.1 psu in 2017 to 17.8 psu in 2018, while the values of CDOM absorption increased from 0.10 to 0.16 m ?1 . The analysis of available hydrometeorological data pointed to intensive vertical mixing due to the strong wind forcing as a main factor in increasing values of both salinity and the CDOM absorption in the surface layer in 2018.
机译:海洋科学和工程学的许多理论和实践方面都需要有关海水及其成分吸收光的数据。但是,到目前为止,黑海东北部尚缺乏此类数据。本文介绍了在2017年6月和2018年6月进行的野外研究期间,由便携式集成腔吸收计(ICAM)分光光度计在黑海格连吉克地区测得的光吸收数据,以及其他原位测量的生物光学和海洋学数据和卫星观测。 2018年,观测到表层有色溶解有机物(CDOM)吸收值升高,同时盐度值很高,这与河流径流是主要CDOM来源的想法背道而驰。盐度的垂直分布在2017年和2018年有所不同,尤其是在浅水区;在上层,盐度从2017年的17.1 psu增加到2018年的17.8 psu,而CDOM吸收值从0.10增加到0.16 m?1。对现有水文气象数据的分析表明,由于强风强迫,强烈的垂直混合是2018年表层盐度和CDOM吸收值增加的主要因素。

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