TY - JOUR
T1 - Unusual distribution of floating seaweeds in the East China Sea in the early spring of 2012
AU - Komatsu, Teruhisa
AU - Mizuno, Shizuha
AU - Natheer, Alabsi
AU - Kantachumpoo, Attachai
AU - Tanaka, Kiyoshi
AU - Morimoto, Akihiko
AU - Hsiao, Sheng Tai
AU - Rothäusler, Eva A.
AU - Shishidou, Hirotoshi
AU - Aoki, Masakazu
AU - Ajisaka, Tetsuro
N1 - Funding Information:
Acknowledgments We thank the captain and crew of the R/V Tansei Maru, Japan Agency for Marine-Earth Science and Technology, for their help during the research cruises. We are also grateful to the researchers who helped with the observation and sampling of seaweed rafts. We thank Dr. W. Yanase and Mr. M. Hamana of the Atmosphere and Ocean Research Institute, The University of Tokyo, for their help with preparing the figures showing the distribution of surface currents in the East China Sea. This work was supported by the Japan Society for the Promotion of Science (JSPS), Grant-in-Aid for Scientific Research (A), no. 22255010, and Grant-in-Aid for JSPS Fellows, no. 22 00413. Coauthor Eva A. Rothäusler thanks the JSPS for inviting her to Japan through the program of Postdoctoral Fellowships for Foreign Researchers. Finally, we thank Prof. M. Thiel at the Universidad del Norte for his valuable comments and help with finalizing this study.
Publisher Copyright:
© 2013, The Author(s).
PY - 2014/4/1
Y1 - 2014/4/1
N2 - Floating seaweeds play important ecological roles in offshore waters. Recently, large amounts of rafting seaweed have been observed in the East China Sea. In early spring, juveniles of commercially important fish such as yellowtail accompany these seaweed rafts. Because the spatial distributions of seaweed rafts in the spring are poorly understood, research cruises were undertaken to investigate them in 2010, 2011, and 2012. Floating seaweed samples collected from the East China Sea during the three surveys contained only Sargassum horneri. In 2010 and 2011, seaweed rafts were distributed only in the continental shelf and the Kuroshio Front because they had become trapped in the convergence zone of the Kuroshio Front. However, in 2012, seaweed was also distributed in the Kuroshio Current and its outer waters, and massive strandings of seaweed rafts were observed on the northern coast of Taiwan and on Tarama Island in the Ryukyu Archipelago. Environmental data (wind, currents, and sea surface height) were compared among the surveys of 2010, 2011, and 2012. Two factors are speculated to have caused the unusual distribution in 2012. First, a continuous strong north wind produced an Ekman drift current that transported seaweed southwestward to the continental shelf and eventually stranded seaweed rafts on the coast of Taiwan. Second, an anticyclonic eddy covering northeast Taiwan and the Kuroshio Current west of Taiwan generated a geostrophic current that crossed the Kuroshio Current and transported the rafts to the Kuroshio Current and its outer waters. Such unusual seaweed distributions may influence the distribution of fauna accompanying the rafts.
AB - Floating seaweeds play important ecological roles in offshore waters. Recently, large amounts of rafting seaweed have been observed in the East China Sea. In early spring, juveniles of commercially important fish such as yellowtail accompany these seaweed rafts. Because the spatial distributions of seaweed rafts in the spring are poorly understood, research cruises were undertaken to investigate them in 2010, 2011, and 2012. Floating seaweed samples collected from the East China Sea during the three surveys contained only Sargassum horneri. In 2010 and 2011, seaweed rafts were distributed only in the continental shelf and the Kuroshio Front because they had become trapped in the convergence zone of the Kuroshio Front. However, in 2012, seaweed was also distributed in the Kuroshio Current and its outer waters, and massive strandings of seaweed rafts were observed on the northern coast of Taiwan and on Tarama Island in the Ryukyu Archipelago. Environmental data (wind, currents, and sea surface height) were compared among the surveys of 2010, 2011, and 2012. Two factors are speculated to have caused the unusual distribution in 2012. First, a continuous strong north wind produced an Ekman drift current that transported seaweed southwestward to the continental shelf and eventually stranded seaweed rafts on the coast of Taiwan. Second, an anticyclonic eddy covering northeast Taiwan and the Kuroshio Current west of Taiwan generated a geostrophic current that crossed the Kuroshio Current and transported the rafts to the Kuroshio Current and its outer waters. Such unusual seaweed distributions may influence the distribution of fauna accompanying the rafts.
KW - East China Sea
KW - Ekman drift current
KW - Floating seaweed
KW - Kuroshio
KW - Phaeophyta
KW - Sargassum horneri
KW - SSH
KW - Transport
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U2 - 10.1007/s10811-013-0152-y
DO - 10.1007/s10811-013-0152-y
M3 - Article
AN - SCOPUS:84887525899
SN - 0921-8971
VL - 26
SP - 1169
EP - 1179
JO - Journal of Applied Phycology
JF - Journal of Applied Phycology
IS - 2
ER -