Distribution of dissolved inorganic nitrogen over the continental slope of the Yellow Sea and East China Sea
Based on survey data from April to May 2009, distribution and its influential factors of dissolved inorganic nitrogen (DIN) over the continental slopes of the Yellow Sea (YS) and East China Sea (ECS) are discussed. Influenced by the Changjiang (Yangtze) River water, alongshore currents, and the Kuro...
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| Published in | Chinese journal of oceanology and limnology Vol. 31; no. 1; pp. 227 - 236 |
|---|---|
| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
Heidelberg
Springer-Verlag
2013
SP Science Press Springer Nature B.V |
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| Abstract | Based on survey data from April to May 2009, distribution and its influential factors of dissolved inorganic nitrogen (DIN) over the continental slopes of the Yellow Sea (YS) and East China Sea (ECS) are discussed. Influenced by the Changjiang (Yangtze) River water, alongshore currents, and the Kuroshio current off the coast, DIN concentrations were higher in the Changjiang River estuary, but lower (<1 μmol/L) in the northern and eastern YS and outer continental shelf area of the ECS. In the YS, the thermocline formed in spring, and a cold-water mass with higher DIN concentration (about 11 μmol/L) formed in benthonic water around 123.2°E. In Changjiang estuary (around 123°E, 32°N), DIN concentration was higher in the 10 m layer; however, the bottom DIN concentration was lower, possibly influenced by mixing of the Taiwan Warm Current and offshore currents. |
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| AbstractList | Based on survey data from April to May 2009, distribution and its influential factors of dissolved inorganic nitrogen (DIN) over the continental slopes of the Yellow Sea (YS) and East China Sea (ECS) are discussed. Influenced by the Changjiang (Yangtze) River water, alongshore currents, and the Kuroshio current off the coast, DIN concentrations were higher in the Changjiang River estuary, but lower (<1 mu mol/L) in the northern and eastern YS and outer continental shelf area of the ECS. In the YS, the thermocline formed in spring, and a cold-water mass with higher DIN concentration (about 11 mu mol/L) formed in benthonic water around 123.2 degree E. In Changjiang estuary (around 123 degree E, 32 degree N), DIN concentration was higher in the 10 m layer; however, the bottom DIN concentration was lower, possibly influenced by mixing of the Taiwan Warm Current and offshore currents. Based on survey data from April to May 2009, distribution and its influential factors of dissolved inorganic nitrogen (DIN) over the continental slopes of the Yellow Sea (YS) and East China Sea (ECS) are discussed. Influenced by the Changjiang (Yangtze) River water, alongshore currents, and the Kuroshio current off the coast, DIN concentrations were higher in the Changjiang River estuary, but lower (<1 μmol/L) in the northern and eastern YS and outer continental shelf area of the ECS. In the YS, the thermocline formed in spring, and a cold-water mass with higher DIN concentration (about 11 μmol/L) formed in benthonic water around 123.2°E. In Changjiang estuary (around 123°E, 32°N), DIN concentration was higher in the 10 m layer; however, the bottom DIN concentration was lower, possibly influenced by mixing of the Taiwan Warm Current and offshore currents. Based on survey data from April to May 2009, distribution and its influential factors of dissolved inorganic nitrogen （DIN） over the continental slopes of the Yellow Sea （YS） and East China Sea （ECS） are discussed. Influenced by the Changjiang （Yangtze） River water, alongshore currents, and the Kuroshio current off the coast, DIN concentrations were higher in the Changjiang River estuary, but lower （〈1 μmol/L） in the northern and eastern YS and outer continental shelf area of the ECS. In the YS, the thermocline formed in spring, and a cold-water mass with higher DIN concentration （about 11 μmol/L） formed in benthonic water around 123.2°E. In Changjiang estuary （around 123°E, 32°N）, DIN concentration was higher in the 10 m layer; however, the bottom DIN concentration was lower, possibly influenced by mixing of the Taiwan Warm Current and offshore currents. |
| Author | Zhang, Chuansong Zhang, Xuan Han, Xiurong Shi, Xiaoyong Wen, Tingting |
| AuthorAffiliation | Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education; Ocean University of China, Qingdao266100, China |
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| Cites_doi | 10.1016/j.hal.2008.08.006 10.1023/A:1021162214304 10.1046/j.1365-2419.2002.00215.x 10.1016/S0304-3894(99)00165-X 10.1007/s10872-007-0030-9 10.1016/j.csr.2007.10.002 10.1175/JCLI3793.1 10.1109/TGRS.2004.834649 10.1016/j.ecss.2008.04.002 10.1007/s00343-011-0505-9 10.1029/2002GB002029 10.1016/j.ecss.2006.05.010 10.1016/j.jmarsys.2008.11.016 10.1007/s00343-011-0502-z 10.1016/S0278-4343(02)00150-4 10.1007/s10872-008-0062-9 10.1007/s00343-007-0261-z 10.1016/j.hal.2008.08.018 10.1016/j.jmarsys.2010.05.004 10.1016/S0272-7714(03)00067-2 10.1016/j.ecss.2006.08.013 10.1016/j.dsr.2011.10.008 10.1016/j.pocean.2007.04.019 10.1016/j.csr.2007.02.009 10.4319/lo.1997.42.5_part_2.1154 |
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| Copyright | Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag Berlin Heidelberg 2013 Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag Berlin Heidelberg 2013. |
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| Keywords | dissolved inorganic nitrogen (DIN) East China Sea (ECS) Yellow Sea (YS) distribution |
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| Notes | ZHANG Xuan , SHI Xiaoyong, WEN Tingting, ZHANG Chuansong ,HAN Xiurong Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education; Ocean University of China, Qingdao 266100, China Based on survey data from April to May 2009, distribution and its influential factors of dissolved inorganic nitrogen （DIN） over the continental slopes of the Yellow Sea （YS） and East China Sea （ECS） are discussed. Influenced by the Changjiang （Yangtze） River water, alongshore currents, and the Kuroshio current off the coast, DIN concentrations were higher in the Changjiang River estuary, but lower （〈1 μmol/L） in the northern and eastern YS and outer continental shelf area of the ECS. In the YS, the thermocline formed in spring, and a cold-water mass with higher DIN concentration （about 11 μmol/L） formed in benthonic water around 123.2°E. In Changjiang estuary （around 123°E, 32°N）, DIN concentration was higher in the 10 m layer; however, the bottom DIN concentration was lower, possibly influenced by mixing of the Taiwan Warm Current and offshore currents. 37-1150/P Yellow Sea （YS）; East China Sea （ECS）; dissolved inorganic nitrogen （DIN）; distribution http://dx.doi.org/10.1007/s00343-013-1299-8 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
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| PublicationTitle | Chinese journal of oceanology and limnology |
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| Publisher | Springer-Verlag SP Science Press Springer Nature B.V |
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| Snippet | Based on survey data from April to May 2009, distribution and its influential factors of dissolved inorganic nitrogen （DIN） over the continental slopes of the... Based on survey data from April to May 2009, distribution and its influential factors of dissolved inorganic nitrogen (DIN) over the continental slopes of the... |
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| SubjectTerms | Brackish Chemistry Cold water masses continental shelf Continental shelves Continental slope DIN dissolved inorganic nitrogen Distribution Earth and Environmental Science Earth Sciences Estuaries Estuarine dynamics Eutrophication Freshwater Human influences Marine Nitrogen Oceanographic instruments Oceanography Offshore Outer continental shelf River water Rivers spring surveys Thermocline Water currents Water masses Water temperature 东中国海 台湾暖流 大陆坡 氮分布 溶解无机氮 长江口 黄海 |
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| Title | Distribution of dissolved inorganic nitrogen over the continental slope of the Yellow Sea and East China Sea |
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