2009-2010年黄海绿潮起源与发生过程调查研究

范士亮; 傅明珠; 李艳; 王宗灵; 方松; 姜美洁; 王洪平; 孙萍; 屈佩

2009-2010年黄海绿潮起源与发生过程调查研究

1.
国家海洋局第一海洋研究所, 山东青岛 266061;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
2.
国家海洋局第一海洋研究所, 山东青岛 266061

基金项目: 国家重点基础研究发展计划(973):我国近海藻华灾害演变机制与生态安全(2010 CB428703);国家自然科学基金:黄海大规模浒苔绿潮起源与早期发生的生态学机理研究(41276119);科技部国际合作课题(2010-2012)绿潮灾害预警与应急关键技术研究(2010DFA24340)。

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出版历程
- 收稿日期: 2012-05-04
- 修回日期: 2012-08-30

Origin and development of Huanghai (Yellow) Sea green-tides in 2009 and 2010

1.
First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China;Key Lab of Science and Engineering for Marine Ecological Environment, State Oceanic Administration, Qingdao 266061, China
2.
First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China

摘要

摘要: 绿潮是我国近海一种新型的海洋生态灾害,自2007年以来,每年5-7月在黄海海域周期性暴发与消亡,给沿海地区造成不同的环境影响和经济损失。本文基于2009-2010年黄海绿潮潜在起源区和绿潮发生过程的海上连续跟踪观测资料,对黄海浒苔绿潮的起源和发生发展过程进行了分析。结果表明,2009年和2010年黄海漂浮绿潮藻均首先发现于江苏南通小洋口外的太阳岛附近,随后,在小洋口至大丰港的近岸海域逐渐出现漂浮绿藻,并随时间逐渐向北漂移,分布面积和生物量均不断增大。不同年份间,黄海浒苔绿潮具有相似的发生发展过程,主要可以分为绿潮藻漂浮发生阶段、绿潮藻聚集阶段以及规模性绿潮形成阶段;但绿潮的发生时间、发生规模和漂移路径有所差异;2009年绿潮漂移线路为逐渐远离海岸线,而2010年绿潮藻的漂移路径基本为平行于海岸线;温度升高与绿潮暴发具有明显相关性。
- 黄海绿潮 /
- 起源 /
- 发生过程
Abstract: Green tides is a new kind of marine ecological disaster in the HuanghaiSea recurrent every year from May to July since 2007 which caused great environmental impacts and economy loss. To determine the origin and early development process of this phenomenon, our group carried out multi-cruise observations in Jiangsu coastal areas from April to June during 2009-2010 and studied the main causes and variations of floating algal transport pathways. The results showed that the floating green algae patches were all first observed around the Sun Island around Xiaoyangkou in the south part of Jiangsu coast during 2009-2010, and drifting northward later on with the expansion of covering and influenced area. The developmental processes were similar in the 2 studied years which can be divided into the patches floating, aggregation and massive green tide forming stage. The blooming time, covering area and transportation pathways of the green tides varied between 2009 and 2010. The seawater temperature may be an important role in the blooming of the green tides.
- the Huanghai Sea green-tides /
- Origin /
- development process

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参考文献(24)

CHARLIER R H, PHILIPPE M, CHARLES W F, et al. Green tides on the Brittany coasts. Environmental Research[J]. Engineering and Management, 2007, 3(41): 52-59.

NELSON T A, HABERLIN K, NELSON A V, et al.. Ecological and physiological controls of species composition in green macroalgal blooms[J]. Ecology, 2008, 89: 1287-1298.

SUN S, WANG F, LI C L, et al. Emerging challenges: Massive green algae blooms in the Yellow Sea[J]. Nature Precedings, 2008, hdl:10101/npre.2266.1.

YABE T, ISHII Y, AMANO Y, et al. Green tide formed by free-floating Ulva spp. at Yatsu tidal flat, Japan[J]. Limnology, 2009, 10: 239-245.

LIU D Y, KEESING J K, XING Q G, et al. World's largest macroalgal bloom casused by expansion of seaweed aquaculture in China[J]. Marine Pollution Bulletin, 2009, 888-895.

HU C M, LI D Q, CHEN C S, et al. On the recurrent Ulva prolifera blooms in the Yellow Sea and East China Sea[J]. Journal of Geophysical Research,2010, 115, C05017.

LIU D, KEESING J K, DONG Z, et al.Recurrence of Yellow Sea green tide in June 2009 confirms coastal seaweed aquaculture provides nursery for generation of macroalgal blooms[J]. Marine Pollution Bulletin, 2010, 60:1423-1432.

PANG S J, LIU F, SHAN T F, et al. Tracking the algal origin of the Ulva bloom in the Yellow Sea by a combination of molecular, morphological and physiological analyses[J]. Marine Environment Research, 2010, 69(4): 207-215.

乔方利,王关锁,吕新刚,等. 2008与2010年黄海浒苔漂移输运特征对比[J]. 科学通报,2011,56(18):1470-1476.

衣立,张苏平,殷玉齐. 2009年黄海绿潮浒苔暴发与漂移的水文气象环境[J]. 中国海洋大学学报,2010,40(10):15-23.

国家海洋局. 2008-2009年海洋灾害公报.

LV 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(6):620-632.

邢飞,汪亚平,高建华,等. 江苏近岸海域悬沙浓度的时空分布特征[J]. 海洋与湖沼,2010,41(3):459-468.

刘志亮,胡敦欣.黄海夏季近岸海区环流的初步分析及其与风速的关系[J]. 海洋学报,2009,31:1-7.

李尧. 中国东部近海夏季环流特征及其动力机制. 青岛:中国科学院海洋研究所,2010:1-14.

XIA C S, QIAO F L, YANG Y Z, et al. Three-dimensional structure of the summertime circulation in the Yellow Sea from a wave-tide-circulation coupled model[J]. Journal of Geophysical Research, 2006, 111:C11S03.

LEE H J, PANG I C, MOON I J, et al. On physical factors that controlled the massive green tide occurrence along the southern coast of the Shandong Peninsula in 2008: A numerical study using a particle-tracking experiment[J]. Journal of Geophysical Research, 2011, JC007512.

RAFFAELI D G, RAVEN J A, POOLE L J. Ecological impat of green macroalgal blooms[J]. Oceanogr Mar Biol,1998, 36:97-125.

梁宗英,林祥志,马牧,等. 浒苔漂流聚集绿潮现象的初步分析[J]. 中国海洋大学学报,2008, 38(4):601-604.

PEDERSEN M F, BORUM J. Nutrient control of estuarine macroalgae: growth strategy and the balance between nitrogen requirements and uptake[J]. Marine Ecology Progress Series, 1997, 161: 155-163.

LIN A P, SHEN S D,WANG J W, et al. Reproduction diversityof Enteromorpha prolifera[J]. Journal of Integrative Plant Biology, 2008, 50:622-629.

张华伟,马家海,胡翔,等. 绿潮漂浮浒苔繁殖特性的研究[J]. 上海海洋大学学报,2011,20(4):600-606.

TAYLOR R, FLETCHER R L, RAVEN J A. Preliminary studies on the growth of selected "green tide" algae in laboratory culture: effects of irradiance, temperature, salinity and nutrients on growth rate[J]. Botanica Marina, 2001, 44: 327-336.

马洪瑞,陈聚法,崔毅,等. 灌河和射阳河水质状况分析及主要污染物入海量估算[J]. 渔业科学进展,2010,31(3):92-99.

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