Vertical Distribution of Bio-Optical Properties of the Azov – Black Sea Basin Waters in April – May, 2019

IF 0.7 Q4 OCEANOGRAPHY Physical Oceanography Pub Date : 2020-11-01 DOI:10.22449/1573-160x-2020-5-525-534
T. Efimova, T. Churilova, E. Skorokhod, N. Moiseeva, E. Zemlianskaia
{"title":"Vertical Distribution of Bio-Optical Properties of the Azov – Black Sea Basin Waters in April – May, 2019","authors":"T. Efimova, T. Churilova, E. Skorokhod, N. Moiseeva, E. Zemlianskaia","doi":"10.22449/1573-160x-2020-5-525-534","DOIUrl":null,"url":null,"abstract":"Purpose. The work is aimed at investigating spatial distribution of the chlorophyll a concentration and the spectral light absorption coefficients by all optically active components in the Azov and Black seas in spring, when the seawater hydrophysical structure changes. Methods and Results. The data collected in the 106th scientific cruise of R/V Professor Vodyanitsky in April 19 – May 10, 2019 were used. The chlorophyll a concentration was measured by the spectrophotometric method. The spectral light absorption coefficients were determined in accordance with the NASA protocol 2018. The optical measurements were performed using the dual-beam spectrophotometer Lambda 35 (PerkinElmer). It was shown that in the surface layer of the Black Sea, the chlorophyll a concentration varied from 0.21 to 1.2 mg/m3. At some stations in the deep-water region, the increased values of this parameter were observed in the lower part of the euphotic zone that was associated with the beginning of seasonal water stratification due to the surface water heating. At these stations, the phytoplankton absorption spectra were more smoothed in the lower part of the euphotic zone than those in the upper layer. In the deep-water region, the non-algal particles contribution to the total particulate light absorption at wavelength 438 nm changed with depth from 40 ± 15 % at the surface to 29 ± 12 % near the bottom of the euphotic zone; whereas in the coastal waters this parameter was almost unchangeable within the water column (54 ± 11 %). No significant change of the colored dissolved organic matter contribution to the total light absorption with depth was revealed (69% on average). In the Sea of Azov, vertical distribution both of the chlorophyll a concentration (6.2 mg/m3 on average) and the spectral light absorption coefficients by all the optically active components was uniform. The non-algal particles contribution to the particulate light absorption was 40 ± 14 %, and the colored dissolved organic matter contribution to the total light absorption constituted 52 ± 6 %. Conclusions. New data on spatial distribution of the chlorophyll a concentration and the spectral light absorption coefficients by the optically active components in the Black and Azov seas were obtained for the spring period when the seawater hydrophysical characteristics changed.","PeriodicalId":43550,"journal":{"name":"Physical Oceanography","volume":" ","pages":""},"PeriodicalIF":0.7000,"publicationDate":"2020-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physical Oceanography","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.22449/1573-160x-2020-5-525-534","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"OCEANOGRAPHY","Score":null,"Total":0}
引用次数: 4

Abstract

Purpose. The work is aimed at investigating spatial distribution of the chlorophyll a concentration and the spectral light absorption coefficients by all optically active components in the Azov and Black seas in spring, when the seawater hydrophysical structure changes. Methods and Results. The data collected in the 106th scientific cruise of R/V Professor Vodyanitsky in April 19 – May 10, 2019 were used. The chlorophyll a concentration was measured by the spectrophotometric method. The spectral light absorption coefficients were determined in accordance with the NASA protocol 2018. The optical measurements were performed using the dual-beam spectrophotometer Lambda 35 (PerkinElmer). It was shown that in the surface layer of the Black Sea, the chlorophyll a concentration varied from 0.21 to 1.2 mg/m3. At some stations in the deep-water region, the increased values of this parameter were observed in the lower part of the euphotic zone that was associated with the beginning of seasonal water stratification due to the surface water heating. At these stations, the phytoplankton absorption spectra were more smoothed in the lower part of the euphotic zone than those in the upper layer. In the deep-water region, the non-algal particles contribution to the total particulate light absorption at wavelength 438 nm changed with depth from 40 ± 15 % at the surface to 29 ± 12 % near the bottom of the euphotic zone; whereas in the coastal waters this parameter was almost unchangeable within the water column (54 ± 11 %). No significant change of the colored dissolved organic matter contribution to the total light absorption with depth was revealed (69% on average). In the Sea of Azov, vertical distribution both of the chlorophyll a concentration (6.2 mg/m3 on average) and the spectral light absorption coefficients by all the optically active components was uniform. The non-algal particles contribution to the particulate light absorption was 40 ± 14 %, and the colored dissolved organic matter contribution to the total light absorption constituted 52 ± 6 %. Conclusions. New data on spatial distribution of the chlorophyll a concentration and the spectral light absorption coefficients by the optically active components in the Black and Azov seas were obtained for the spring period when the seawater hydrophysical characteristics changed.
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
2019年4 - 5月亚速海-黑海水域生物光学特性的垂直分布
意图这项工作旨在研究春季海水水物理结构发生变化时,亚速海和黑海所有光学活性成分的叶绿素a浓度和光谱光吸收系数的空间分布。方法和结果。使用了2019年4月19日至5月10日R/V教授Vodyanitsky在第106次科学巡航中收集的数据。用分光光度法测定了叶绿素a的浓度。光谱光吸收系数是根据NASA 2018协议确定的。使用双光束分光光度计Lambda 35(PerkinElmer)进行光学测量。结果表明,在黑海表层,叶绿素a的浓度在0.21-1.2mg/m3之间。在深水区的一些站点,在透光带的下部观察到该参数的值增加,这与地表水加热导致的季节性水分层的开始有关。在这些站点,浮游植物吸收光谱在透光带的下部比在上层更平滑。在深水区,非藻类颗粒对438nm波长的总颗粒光吸收的贡献随着深度的变化而变化,从表层的40±15%变化到透光带底部附近的29±12%;而在沿海水域,该参数在水柱内几乎不变(54±11%)。着色溶解有机物对总光吸收的贡献没有随深度的显著变化(平均69%)。在亚速海,叶绿素a浓度(平均6.2 mg/m3)和所有光学活性成分的光谱光吸收系数的垂直分布是均匀的。非藻类颗粒对颗粒光吸收的贡献为40±14%,有色溶解有机物对总光吸收的影响为52±6%。结论。获得了春季海水水物理特征发生变化时黑海和亚速海叶绿素a浓度和光学活性组分光谱光吸收系数的空间分布新数据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
Physical Oceanography
Physical Oceanography OCEANOGRAPHY-
CiteScore
1.80
自引率
25.00%
发文量
8
审稿时长
24 weeks
期刊最新文献
Modeling of Marine Ecosystems: Experience, Modern Approaches, Directions of Development (Review). Part 1: End-to-End Models http://physical-oceanography.ru/repository/2022/1/1.html Seasonal and Interannual Variability of the Thermohaline Structure of the Bengel Upwelling Based on the Argo Buoys Data Thermocline Dynamics in the Zone of the Rim Current Action in Winter Period (Based on to the Drifter Experiment Data) Oxygen Dynamics during the Period of Dystrophic Processes in the Black Sea
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1