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서지반출
남해와 동중국해에서 위성으로 추정된 표층수온 및 클로로필의 장기 변화
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  • 남해와 동중국해에서 위성으로 추정된 표층수온 및 클로로필의 장기 변화
저자명
손영백,유주형,노재훈,주세종,김상현,Son. Young-Baek,Ryu. Joo-Hyung,Noh. Jae-Hoon,Ju. Se-Jong,Kim. Sang-Hyun
간행물명
Ocean and polar research
권/호정보
2012년|34권 2호|pp.201-218 (18 pages)
발행정보
한국해양과학기술원
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이 논문은 한국과학기술정보연구원과 논문 연계를 통해 무료로 제공되는 원문입니다.
서지반출

기타언어초록

The purpose of this study is to investigate climatological variations from the sea surface temperature (SST), chlorophyll-a concentration (Chl-a), and phytoplankton size class (PSC), using NOAA AVHRR, SeaWiFS, and MODIS data in the South Sea of Korea (SSK) and East China Sea (ECS). 26-year monthly SST and 13-year monthly Chl-a and PSC data, separated by whole and nine-different areas, were used to understand seasonal and inter-annual variations. SST and Chl-a clearly showed seasonal variations: higher SST and Chl-a were observed during the summer and spring, and lower values occurred during the winter and summer. The annual and monthly SST over 26 years increased by $0.2{sim}1.0^{circ}C$. The annual and monthly Chl-a concentration over 13 years decreased by $0.2{sim}1.1mg/m^3$. To determine more detailed spatial and temporal variations, we used the combined data with monthly SST, Chl-a, and PSC. Between 1998 and 2010, the inter-annual trend of Chl-a decreased, with decreasing micro- and nano-size plankton, and increasing pico-size plankton. In regional analysis, the west region of the study area was spatially and temporally correlated with the area dominated by decreasing micro-size plankton; while the east region was less sensitive to coastal and land effects, and was dominated by increasing pico-size plankton. This phenomenon is better related to one or more forcing factors: the increased stratification of ocean driven by changes occurring in spatial variations of the SST caused limited contributions of nutrients and changed marine ecosystems in the study area.