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Nutrients in melt ponds and snows on Arctic sea ice during 2014 sea ice camp

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Nutrients in melt ponds and snows on Arctic sea ice during 2014 sea ice camp
Other Titles
2014년 해빙캠프 기간 중 해빙 위에 존재하는 얼음호수와 눈의 영양염 성분들
Jung, Jinyoung
Kang, Sung-Ho
Lee, Sang H.
Yang, Eun Jin
Min, Jun-Oh
Issue Date
Jung, Jinyoung, et al. 2015. Nutrients in melt ponds and snows on Arctic sea ice during 2014 sea ice camp. The 21st International Symposium on Polar Sciences. 극지연구소. 2015.05.19~2015.05.20.
Melt ponds are the most distinctive summertime feature of Arctic sea ice, which are formed by melting snow and surface sea ice due to surface melt driven by increased short-wave radiation absorption in summer. Although considerable effort has been devoted to investigate physical processes and feedbacks of melt ponds, relatively little is known about biogeochemical properties of melt ponds. To examine chemical components of nutrients (NH4, NO2+NO3, PO4 and SiO2) in different types of melt ponds (i.e., closed and opened ponds) and differences of nutrients in between melt ponds and snows near melt ponds, a total of 36 melt ponds and snow samples were collected at two different sea ice stations located in northern part of the Chukchi Sea during the ARA05B cruise aboard Korean icebreaker Araon. In the closed melt ponds (salinity ? zero), NH4 and NO2+NO3 showed high concentrations, whereas PO4 concentrations were low and SiO2 was not detected. In contrast, in the opened ponds (salinity ? surface seawater), both nitrogen species were depleted as those in surface seawater, while PO4 and SiO2 concentrations were as high as those in surface seawater. In snow samples, mean NH4 concentration was about 9 times higher than that of NO2+NO3, probably due to NO2 and NO3 losses in snows by photolysis. Likewise SiO2 in the closed ponds, SiO2 in snow samples was not detected. From these results, it was suggested that not only salinity, but also nitrogen species, especially NH4, and SiO2 can be used as an indicator to distinguish between the closed and opened ponds, and that high NH4 concentrations in the closed ponds were derived from snows. In addition, all nutrients species concentrations in surface and deep waters of the opend ponds showed large differences, suggesting that the melt pond waters were strongly stratified. Although no statistically significant relationships were found between chlorophyll a and nutrients variation trends, chlorophyll a concentrations in both types of melt ponds were higher than those in surface seawater, implying that additional nutrients supplied to the melt ponds from snows might contribute to more high biological acitivities in the melt ponds. Considering that the Arctic Ocean is currently experiencing rapid environmental change, such as warming and decreases in sea ice concentration and thickness, the role of melt ponds could be important. Further studies on biogeochemical cycles in the melt ponds therefore are required to improve understanding of the Arctic marine ecosystem more clearly.
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The 21st International Symposium on Polar Sciences
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