| 夏季南极长城湾海流变化特征及其对浮游植物生物量的影响 |
| |
| 引用本文： | 罗光富,何剑锋,张芳,蔡明红,林凌,蓝木盛.夏季南极长城湾海流变化特征及其对浮游植物生物量的影响[J].海洋学报,2016,38(10):113-124. |
| |
| 作者姓名： | 罗光富 何剑锋 张芳 蔡明红 林凌 蓝木盛 |
| |
| 作者单位： | 1.中国极地研究中心 国家海洋局极地科学重点实验室, 上海 200136 |
| |
| 基金项目： | 南北极环境综合考察与评估专项（CHINARE2016-01-05）；国家高技术研究发展计划（2007AA09Z121） |
| |
| 摘 要： | 通过对2010/2011年夏季南极长城湾叶绿素a浓度和海流等环境参数的传感器连续观测；研究其时空变化特征及海流对浮游植物生物量的影响。结果表明；12.9 m水层叶绿素a浓度从12月中旬开始增长；直至2月上旬开始维持相对稳定；期间出现两个高值点（2.74 μg/L和3.76 μg/L）。叶绿素a浓度表现出了24 h周期变化特征；每日叶绿素a浓度最高值出现在正午前后时段的概率要高于其他时段。表层海水受西北风影响；流速较大；约为60~100 cm/s；中层和底层水体流速较小；约为10 cm/s。表层的风海流使海水在长城湾发生辐散；下层海水向上涌升；驱动了水体的垂直交换。长城湾与麦克斯韦尔湾存在水体交换；水体主要从中层进入湾内；从表层输出。长城湾的叶绿素a浓度与流速呈显著负相关；表明低流速环境有利于长城湾浮游植物的生长。
|
| 关 键 词： | 叶绿素a浓度 海流 浮游植物 长城湾 南极 |
| 收稿时间： | 2016/1/11 0:00:00 |
Effects of current velocity on phytoplankton biomass in Great Wall Bay, Antarctica during summer 2010/2011 |
| |
| Luo Guangfu,He Jianfeng,Zhang Fang,Cai Minghong,Lin Ling and Lan Musheng.Effects of current velocity on phytoplankton biomass in Great Wall Bay, Antarctica during summer 2010/2011[J].Acta Oceanologica Sinica (in Chinese),2016,38(10):113-124. |
| |
| Authors: | Luo Guangfu He Jianfeng Zhang Fang Cai Minghong Lin Ling and Lan Musheng |
| |
| Institution: | 1.The Key Laboratory for Polar Science of State Ocean Administration, Polar Research Institute of China, Shanghai 200136, China2.The Key Laboratory for Polar Science of State Ocean Administration, Polar Research Institute of China, Shanghai 200136, China;College of Environmental Science and Engineering, Tongji University, Shanghai 200092, China |
| |
| Abstract: | Understanding the mechanism by which environmental factors affects phytoplankton growth in summer is essential for determining polar marine ecosystem responses to global climate change. Here we deployed an online mooring system in Great Wall Bay to determine how current velocity and local physical forcing affect the temporal and spatial distribution of phytoplankton biomass in Antarctic coastal waters. The results show that chlorophyll a(Chl a)concentrations accumulated from mid-December and two significant blooms developed in January (2.74 μg/L and 3.76 μg/L) and were then maintained at a relatively high level. The diurnal variations of cholorophyll a concentrations were observed in both upper and middle layers during the monitoring period. The surface current velocity reached approximately (60-100)cm/s, while the middle and bottom current velocity was limited to about 10 cm/s. We conclude that summer winds played an important role in the surface current velocity and direction. The monitoring site appears to exchange with adjacent oceanic waters, such an intrusion of water would bring in varied phytoplankton species. The results of Pearson correlation analysis showed the significant and positive influence of low current velocity on chlorophyll a concentrations, especially during phytoplankton blooms, whereas the increased current velocity showed the significant and negative correlations with phytoplankton biomass. |
| |
| Keywords: | chlorophyll a concentrations current phytoplankton biomass Great Wall Bay |
| 本文献已被 CNKI 等数据库收录！ |
| 点击此处可从《海洋学报》浏览原始摘要信息 |
| 点击此处可从《海洋学报》下载免费的PDF全文 |
|
