

FOLLOWUS
1.North China Sea Marine Forecasting and Hazard Mitigation Center, Ministry of Natural Resources, Qingdao 266061, China
2.Shandong Key Laboratory of Marine Ecological Environment and Disaster Prevention and Mitigation, Qingdao 266061, China
3.National Engineering Laboratory for Integrated Aero-Space-Ground-Ocean Big Data Application Technology, Xi’an 710129, China
4.East China Sea Marine Forecasting and Hazard Mitigation Center, Ministry of Natural Resources, Shanghai 200136, China
5.North China Sea Ecological Center, Ministry of Natural Resources, Qingdao 266033, China
gaosong@ncs.mnr.gov.cn
yuanchao@ncs.mnr.gov.cn
收稿:2023-05-12,
录用:2023-07-03,
网络首发:2023-09-21,
纸质出版:2024-05-01
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Analysis on the causes of massive stranding of Yellow Sea green tide on Lianyungang and Rizhao coasts in 2022[J]. 海洋湖沼学报(英文), 2024,42(3):816-830.
WU Lingjuan,HUANG Juan,DING Yi,et al.Analysis on the causes of massive stranding of Yellow Sea green tide on Lianyungang and Rizhao coasts in 2022[J].Journal of Oceanology and Limnology,2024,42(03):816-830.
Analysis on the causes of massive stranding of Yellow Sea green tide on Lianyungang and Rizhao coasts in 2022[J]. 海洋湖沼学报(英文), 2024,42(3):816-830. DOI:
WU Lingjuan,HUANG Juan,DING Yi,et al.Analysis on the causes of massive stranding of Yellow Sea green tide on Lianyungang and Rizhao coasts in 2022[J].Journal of Oceanology and Limnology,2024,42(03):816-830. DOI:
In 2022
Yellow Sea green tide caused by
Ulva
prolifera
reached a historic minimum and the coastal areas of Shandong Peninsula were less affected. However
the largest amount of seaweed biomass has been washed ashore on Lianyungang and Rizhao coasts since 2015. We studied the development pattern of Yellow Sea green tide in 2022
and analyzed the key environmental factors on the growth and drifting
then discussed the possible reasons that resulted in the massive stranding of green tide biomass in Lianyungang and Rizhao. Results show under the combined influence of the east to southeast winds and currents with shoreward anomalies
green tide drifted to the coastal waters between Shandong and Jiangsu provinces and the distribution areas located westward compared with previous years (2008–2021). Floating
U
.
prolifera
rafts from the coastal waters of Binhai and Sheyang drifted continuously into the coastal waters of Lianyungang and Rizhao
providing important supplements for Yellow Sea green tide. Because green tide in 2022 distributed close to the coastal waters
the abundant nutrients might support their continuous high growth rate. I
n addition
the amount of rainfall around Shandong Peninsula from late June to early July were significantly higher than in previous years
which might promote the development of green tide to some extent.
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