中国东部陆架海锋面的时空变化及其对细颗粒沉积物输运和沉积的影响

袁萍; 王厚杰; 毕乃双; 吴晓; 张勇

doi:10.16562/j.cnki.0256-1492.2019050602

中国东部陆架海锋面的时空变化及其对细颗粒沉积物输运和沉积的影响

1.
中国海洋大学海洋地球科学学院，海底科学与探测技术教育部重点实验室，青岛 266100

2.
中国地质调查局青岛海洋地质研究所，青岛 266071

基金项目: 国家杰出青年科学基金项目“河口海岸学：现代黄河入海沉积物从源到汇的关键沉积动力过程”（41525021）；国家重点研发计划项目课题“大型水库调控下河口沉积动力过程及其生物地球化学效应”（2016YFA0600903）

详细信息

作者简介: 袁萍（1989—），女，博士研究生，海洋地质专业，E-mail：yuanping89@sina.cn

通讯作者: 王厚杰（1970—），男，教授，主要从事近海沉积动力学研究，E-mail：hjwang@ouc.edu.cn

中图分类号: P76

收稿日期: 2019-05-06

修回日期: 2019-05-21

刊出日期: 2020-06-25

Temporal and spatial variations of oceanic fronts and their impact on transportation and deposition of fine-grained sediments in the East China Shelf Seas

1.
College of Marine Geosciences, Ocean University of China, Key Laboratory of Submarine Geosciences and Prospecting Technique, Ministry of Education, Qingdao 266100,China

2.
Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071,China

More Information

Corresponding author: WANG Houjie, hjwang@ouc.edu.cn

Received Date: 06 May 2019

Revised Date: 21 May 2019

Publish Date: 25 June 2020

摘要

摘要:
本文利用中国东部陆架海不同季节的航次观测数据与HYCOM模式数据，分析了HYCOM模式输出的水体温盐数据在中国东部陆架海的适用性，并探讨了中国东部陆架海表底层温盐锋面的时空变化及其对细颗粒沉积物输运和沉积的影响。研究结果表明，中国东部陆架海表、底层温度锋（盐度锋）的分布趋势基本一致（不考虑冲绳海槽以东的海域），但底层锋面的强度和锋区范围明显大于表层。锋面的位置很好的体现了海区流系的基本格局。表、底层温度锋面基本处于几大水团的交界处，说明表、底层温度锋面的分布与研究区环流和水团配置情况密切相关。而表、底层盐度锋面的分布则与研究区入海径流、沿岸流以及暖流等的分布密切相关。此外，对比锋面与中国东部陆架各泥质沉积区的位置可以发现，研究区温盐锋面的空间分布和季节变化对于泥质沉积区的形成具有重要的控制作用。
- 中国东部陆架海 /
- 锋面 /
- 时空变化 /
- 细颗粒沉积物 /
- 沉积物输运 /
- 泥质沉积区
Abstract:
Observed hydrologic datasets and HYCOM modelling data were used in this paper to evaluate the applicability and stability of the HYCOM temperature and salinity data to the temporal-spatial distribution of oceanic fronts and its impact on transportation and deposition of fine-grained sediments in the East China Shelf Seas. The results show that the distribution of thermal fronts or salinity fronts are similar on the surface and bottom in the Bohai, Yellow and East China Seas excluding the east of Okinawa Trough. However, the strength and coverage of the fronts on the bottom are larger than those on the surface. The location of thermal fronts depends on the basic structure of currents. Both the surface and bottom thermal fronts develop along the boundaries of water masses, suggesting that thermal current fronts are closely related to the current and water masses of the study area. However, the distribution of the salinity fronts is greatly influenced by water discharge, coastal currents and warm currents. In addition, the distribution of mud patches in the Eastern China Shelf Sea are closely related to the patterns of oceanic fronts, which means that the thermal and salinity fronts do play a critical role in the formation of mud deposits.
- East China Shelf Seas /
- oceanic fronts /
- temporal and spatial variation /
- fine-grained sediment /
- sediment transportation /
- mud patches

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图 1 中国东部陆架海冬季（A）与夏季（B）环流示意图（改绘自Guan, 1994^[47]和苏纪兰等，2005^[42]）

Figure 1.

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图 2 调查站位分布图（a. 春季航次，b. 夏季航次，c. 秋季航次，d. 冬季航次）

Figure 2.

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图 3 中国东部陆架海实测温盐与HYCOM温盐相关性分析

Figure 3.

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图 4 中国东部陆架海表层流场分布图（底图为流速大小；图中箭头方向表示余流的方向，箭头大小表示流速大小）

Figure 4.

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图 5 中国东部陆架海底层流场分布图（底图为流速大小；图中箭头方向表示余流的方向，箭头大小表示流速大小）

Figure 5.

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图 6 中国东部陆架海HYCOM表层温度锋面分布图

Figure 6.

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图 7 中国东部陆架海HYCOM底层温度锋面分布图

Figure 7.

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图 8 中国东部陆架海HYCOM表层盐度锋面分布图

Figure 8.

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图 9 中国东部陆架海HYCOM底层盐度锋面分布图

Figure 9.

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图 10 中国东部陆架海泥质区分布（改绘自Saito 和 Yang, 1995^[56]）及全新世沉积物等厚度图（单位：m，改绘自Yang 和 Liu, 2007^[74]；Liu 等, 2007^[3]）

Figure 10.

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表 1 7个航次信息

Table 1. Information of cruises

航次类型		起止日期	站位数	CTD型号
春季航次	渤黄海	2014.4.28—2014.5.18（21 d）	127	Seabird 911 plus
	东海	2016.3.7—2016.3.19（13 d）	77	Seabird 25和Seabird 37
夏季航次	渤黄海	2016.6.29—2016.7.15（17 d）	109	Seabird 911 plus
	东海	2016.7.4—2016.7.15（12 d）	57	Seabird 25
秋季航次	渤黄海	2010.9.8—2010.9.21（14 d）	90	Seabird 911 plus
	东海	2010.11.1—2010.11.10（10 d）	44	Seabird 19 plus
冬季航次	渤黄海	2016.12.29—2017.1.13（16 d）	112	Seabird 911 plus
注：冬季航次东海的数据缺失，故未能列出。

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