南黄海冷水团海域溶解氧和叶绿素最大现象值及营养盐累积的季节演变

韦钦胜; 傅明珠; 李艳; 王保栋; 于志刚

doi:10.3969/j.issn.0253-4193.2013.04.017

南黄海冷水团海域溶解氧和叶绿素最大现象值及营养盐累积的季节演变

doi: 10.3969/j.issn.0253-4193.2013.04.017

1.
国家海洋局第一海洋研究所海洋生态环境科学与工程国家海洋局重点实验室, 山东青岛 266061;中国海洋大学海洋化学理论与工程技术教育部重点实验室, 山东青岛 266100
2.
国家海洋局第一海洋研究所海洋生态环境科学与工程国家海洋局重点实验室, 山东青岛 266061
3.
中国海洋大学海洋化学理论与工程技术教育部重点实验室, 山东青岛 266100

基金项目: 国家重点基础研究发展计划973项目课题 (2011CB403602)“海洋环境变化与水母暴发的相互作用”;我国近海海洋综合调查与评价专项课题(908-01-ST03);中央级公益性科研院所基本科研业务费专项资金项目(2013G10)。

计量
- 文章访问数: 4456
- HTML全文浏览量: 47
- PDF下载量: 17376
- 被引次数: 0
出版历程
- 收稿日期: 2012-08-27
- 修回日期: 2013-02-28

Observation of the seasonal evolution of DO, chlorophyll a maximum phenomena and nutrient accumulating in the southern Huanghai (Yellow) Sea Cold Water Mass area

1.
Key Laboratory of Science and Engineering for Marine Ecological Environment, First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China;Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, China
2.
Key Laboratory of Science and Engineering for Marine Ecological Environment, First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China
3.
Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao 266100, China

摘要

摘要: 基于2006-2007年在南黄海冷水团海域开展的4个季度月的调查资料, 重点研究了该海域溶解氧(DO)、叶绿素a(Chl a)最大值现象和营养盐累积的季节演变规律。结果表明:春至秋季黄海冷水团海域DO和Chl a最大值层深度具有先加深后变浅的趋势, 出现最大值层的海域面积呈现出先增大后缩小的变化过程, DO和Chl a最大值层的深度及面积在夏季均达到最大, 至冬季DO和Chl a最大值现象消失;夏季冷水团海域深水区DO最大值处的氧含量整体高于春季, 而冷水团边界附近氧最大值处的氧含量整体低于春季;春至秋季冷水域深水区次表层Chl a最大值处的Chl a含量先降低后升高, 于夏季时最低, 入秋后开始升高, 而一年四季中冷水域边界附近Chl a最大值处的Chl a含量却在夏季时最高, 而且显著高于深水区。黄海冷水团海域的底层营养盐储库具有一定的空间异质性, 冷水域底层通常分别在深水区和西部边界处存在营养盐高值核心, 其中位于深水区的高值核心位置季节变化不明显, 而位于冷水域西部边界附近的高值核心位置则呈现出自春季至夏季向西移动、入秋后又向东部移动的季节变化特征。水文物理因素和生物化学过程对DO、Chl a最大值及营养盐储库的季节演变具有重要的调控作用。
- 黄海冷水团 /
- DO最大值现象 /
- 次表层Chla最大值现象 /
- 营养盐累积
Abstract: Based on the data obtained in four seasonal surveys during 2006-2007 in the southern Huanghai (Yellow) Sea Cold Water Mass area, the seasonal evolution of dissolved oxygen(DO), chlorophyll a(Chl a)maximum phenomena and nutrient accumulating process was analyzed.The result showed that:(1)From spring to autumn, the depth of DO and Chl a maximum layer had the trend of deepening first and then shallowing, the scope of DO and Chl a maximum layer increased firstly and then decreased, the depth and scope of DO and Chl a maximum layer were the largest in summer;the DO and Chl a maximum phenomena disappeared in winter.(2)In DO maximum layer in the deep waters of the cold water mass in summer, DO concentration in summer was higher than in spring, while in DO maximum layer in the boundary area of the cold water mass in summer, DO concentration in summer was lower than in spring.(3)From spring to autumn, Chl a concentration in Chl a maximum layer had the trend of decreasing firstly and then increasing, and it was the lowest in summer;in Chl a maximum layer located in the frontal region of the cold water mass in summer, Chl a concentration in summer was the largest all the year round, and was much higher than in deep waters.(4)The nutrient storage in the bottom cold water mass area of the southern Huanghai Sea had spatial heterogeneity, generally, there was a high-concentration core of nutrients in the deep waters and the boundary region of the cold water mass area respectively, the one situating in the deep water had the fixed position on the whole all the year round, while the one located in the boundary region of the cold water mass moved westward from spring to summer, and then moved eastward again when autumn was coming.(5)Hydrological factors and bio-chemical effect played an important role in regulating the seasonal evolution of the DO and Chl a maximum phenomena as well the nutrient storage．
- Huanghai(Yellow) Sea Cold Water Mass /
- DO maximum phenomenon /
- subsurface Chl a maximum phenomenon /
- nutrient accumulating

HTML全文

参考文献(26)

赫崇本, 汪园祥, 雷宗友, 等.黄海冷水团的形成及其性质的初步探讨[J].海洋与湖沼, 1959, 2(1):11-15．

于非, 张志欣, 刁新源, 等.黄海冷水团演变过程及其与邻近水团关系的分析[J].海洋学报, 2006, 28(5):26-34．

顾宏堪.海水溶解氧夏季垂直分布中的最大值[J].海洋与湖沼, 1966, 8(2):85-91．

顾宏堪.黄海溶解氧垂直分布中的最大值[J].海洋学报, 1980, 2(6):70-79．

刁焕祥, 沈志良.黄海冷水域水化学要素的垂直分布特性[J].海洋科学集刊, 1985, 25:41-51．

熊庆成, 丁宗信, 赵保仁.秋末南黄海冷水团区溶解氧垂直结构及其最大值的分析研究[J].1986, 27:107-114．

刘克修, 赵保仁.黄海溶解氧垂直分布最大值的数值研究[J].海洋学报, 1997, 19(4):80-89．

王保栋.黄海溶解氧垂直分布最大值的成因[J].黄渤海海洋, 1996, 15(3):10-15．

王保栋, 王桂云, 郑昌洙, 等.南黄海溶解氧的垂直分布特征[J].海洋学报, 1999, 21(5):72-77．

韦钦胜, 葛人峰, 王保栋, 等.南黄海冷水域西部溶解氧垂直分布最大值现象的成因分析[J].海洋学报, 2009, 31(4):69-77．

张书文.黄海冷水团夏季叶绿素垂向分布结构的影响机制[J].海洋与湖沼, 2003, 34(2):179-186．

胡好国, 万振文, 袁业立.南黄海浮游植物季节性变化的数值模拟与影响因子分析[J].海洋学报, 2004, 26(6):74-88．

张书文, 夏长水, 袁业力.黄海冷水团水域物理-生态耦合数值模式研究[J].自然科学进展, 2002, 12(3):315-319

傅明珠, 王宗灵, 孙萍, 等.2006年夏季南黄海浮游植物叶绿素 a 分布特征及其环境调控机制[J].生态学报, 2009, 29(10):5366-5375．

夏洁, 高会旺.南黄海东部海域浮游生态系统要素季节变化的模拟研究[J].安全与环境学报, 2006, 6(4):59-65．

Li H B, Xiao T, Ding T, et al.Effect of the Yellow Sea Cold Water Mass(YSCWM)on distribution of bacterioplankton[J].Acta Ecologica Sinica, 2006, 26:1012-1020．

王保栋, 王桂云, 郑昌洙, 等.南黄海营养盐的平面分布及横向输运[J].海洋学报, 1999, 21(6):124-129．

王保栋.黄海冷水域生源要素的变化特征及相互关系[J].海洋学报, 2000, 22(6):47-54．

国家质量监督总局.GB17378.4-1998 海洋监测规范第4部分:海水分析[S].北京:中国标准出版社, 1998．

Parsons T R, Maita Y, Lalli C M.A manual of Chemical and Biological Methods for Seawater Analysis[M].Oxford:Pergamon Press, 1984:107-109, 115-122．

邹娥梅, 郭炳火, 汤毓祥, 等.1996年春季南黄海水文特征和水团分析[J].海洋学报, 2000, 22(1):17-26．

韦钦胜, 葛人峰, 李瑞香, 等.南黄海西部36°N断面生态环境特征及其季节变化[J].海洋学报, 2011, 33(5):61-72．

赵保仁.南黄海西部的陆架锋及冷水团锋区环流结构的初步研究[J].海洋与湖沼, 1987, 18(3):217-226．

韦钦胜, 葛人峰, 臧家业, 等.夏季南黄海跨锋断面的生态环境特征及锋区生态系的提出[J].海洋学报, 2011, 33(3):74-84．

Lü X G, Qiao F L, Xia C S, et al.Upwelling and surface cold patches in the Yellow Sea in summer:Effects of tidal mixing on the vertical circulation[J].Continental Shelf Research, 2010, 30:620-632．

韦钦胜, 于志刚, 葛人峰, 等.黄海西部沿岸冷水在夏季南黄海西部底层冷水形成和季节演变过程中作用的化学水文学分析[J].海洋与湖沼, 2012, in press．

施引文献

资源附件(0)

访问统计