• 제목/요약/키워드: Kuroshio

검색결과 194건 처리시간 0.023초

SEASONAL VARIATION OF THE OCEANIC WATER INTRUSIONS INTO KAGOSHIMA BAY DERIVED FROM THE SATELLITE SST AND CHL-A IMAGES

  • Hosotani, Kazunori
    • 대한원격탐사학회:학술대회논문집
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    • 대한원격탐사학회 2008년도 International Symposium on Remote Sensing
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    • pp.61-64
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    • 2008
  • Seasonal distribution of the oceanic water intrusion was investigated using satellite SST (sea surface temperature) and chl-a (chlorophyll-a) images taken by the MODIS Aqua sensor. The warm water mass emanating periodically from the meandering Kuroshio Current brings the oceanic water intrusion, known as the 'Kyucho' phenomenon, into Kagoshima bay during the winter. Satellite SST images and buoy robot data show that this warm water intrusion has the characteristics of a semigeostrophic gravity current influenced by the Coriolis effect. However, it is difficult to find the oceanic water intrusion during the summer season considering that it is accompanied by thermal stratification, and SST shows almost the same temperature between the inner side of the bay and the ocean. In this research, the satellite chl-a images taken by MODIS Aqua were employed instead of SST images to reveal the oceanic water intrusion in each season. The enclosed bay has the tendency to undergo eutrophication caused by organic materials from land and differences in chl-a concentration of the bay water and the oceanic water. As a result, distribution of low concentration chl-a with oceanic water intrusion in summer season shows almost the same pattern in winter season. On the other hand, in spring season, both SST and chl-a images are available to differentiate the oceanic water intrusion. Therefore, applying the suitable satellite sensor images for each season is effective in the monitoring of oceanic water intrusion. Moreover, in this area, SST and chl-a distribution reveal not only the oceanic water intrusion into Kagoshima bay but also the intrusion at Fukiage seashore facing East China Sea.

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제주도 남동부해역에서 채집된 은붕장어, Gnathophis nystromi (뱀장어목: 붕장어과) 엽상자어의 분포특성 및 형태발달 (Distribution and morphological development of a Gnathophis nystromi (Congridae: Anguilliformes) leptocephalus collected from southeastern waters of Jeju Island)

  • 지환성;최정화;윤상철;주형운
    • 수산해양기술연구
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    • 제51권4호
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    • pp.527-534
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    • 2015
  • The twenty six specimens of leptocephali (15.8-32.6 mm TL) of the family Congridae, collected from southeastern waters offshore of Jeju Island during August 2014, and were identified by means of morphology and genetics. Those specimens were identified as belonging to the family Congridae based on various combinations of morphological characters. An analysis of the partial 12S rRNA sequences (886 base pairs) of mitochondrial DNA showed that our specimens must be Gnathophis nystromi, because their sequences were concordant with those of G. nystromi adult (genetic distance= 0.001), furthermore their total myomeres being consistent with those of G. nystromi adult. Catch rates of G. nystromi leptocephali were higher in the offshore regions than coastal regions of Jeju Island. The smallest leptocephali (< 20 mm TL) were collected offshore from Jeju Island. We hypothesize that one of the spawning grounds of G. nystromi is located offshore in the Jeju Island. In conclusion, the hatched preleptocephali of G. nystromi might have been transported from offshore near Jeju Island to the Korea Strait by the Kuroshio Current and Tsushima Warm Current.

위성 고도계 자료를 활용한 한반도 해수면 높이 변동 연구 (Study on Sea Level Changes in Korean Peninsula by Using Satellite Altimetry Data)

  • 황도현;윤홍주;서원찬
    • 한국전자통신학회논문지
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    • 제11권3호
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    • pp.325-330
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    • 2016
  • 해수면은 19세기 말부터 상승 추세에 있으며, 20세기 이후 상승률이 더욱 가속화되고 있다. 해수면 높이는 지역적인 차이가 크기 때문에 한반도 주변 해역을 대상으로 해수면 변동에 관하여 알아보고자 하였다. 사용된 자료는 해상도 $1/4^{\circ}$의 Topex/Poseidon, Jason-1, Jason-2 위성의 고도계 자료를 이용하였다. 1993년부터 2013년까지 21년간 월별 평균 해수면 아노말리는 1~4월은 음의 값을 보였으며, 5~10월까지 양의 값을 보였다. 중국 보하이만은 대륙성 기후의 영향을 받아 해수면 변동이 큰 것으로 나타났다. 21년 자료를 평균한 결과 중국 보하이만은 대륙성 기후 영향을 받는 것이 두드러지게 나타났으며, 쿠로시오 해류 및 와동류 영향을 받아 해수면 변동이 나타나는 것을 알 수 있었다.

고해상도 기후예측시스템의 표층해류 예측성능 평가 (Assessment of Ocean Surface Current Forecasts from High Resolution Global Seasonal Forecast System version 5)

  • 이효미;장필훈;강기룡;강현석;김윤재
    • Ocean and Polar Research
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    • 제40권3호
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    • pp.99-114
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    • 2018
  • In the present study, we assess the GloSea5 (Global Seasonal Forecasting System version 5) near-surface ocean current forecasts using globally observed surface drifter dataset. Annual mean surface current fields at 0-day forecast lead time are quite consistent with drifter-derived velocity fields, and low values of root mean square (RMS) errors distributes in global oceans, except for regions of high variability, such as the Antarctic Circumpolar Current, Kuroshio, and Gulf Stream. Moreover a comparison with the global high-resolution forecasting system, HYCOM (Hybrid Coordinate Ocean Model), signifies that GloSea5 performs well in terms of short-range surface-current forecasts. Predictions from 0-day to 4-week lead time are also validated for the global ocean and regions covering the main ocean basins. In general, the Indian Ocean and tropical regions yield relatively high RMS errors against all forecast lead times, whilst the Pacific and Atlantic Oceans show low values. RMS errors against forecast lead time ranging from 0-day to 4-week reveal the largest increase rate between 0-day and 1-week lead time in all regions. Correlation against forecast lead time also reveals similar results. In addition, a strong westward bias of about $0.2m\;s^{-1}$ is found along the Equator in the western Pacific on the initial forecast day, and it extends toward the Equator of the eastern Pacific as the lead time increases.

Himawari-8/AHI 자료를 활용한 표층 해류 산출 알고리즘 비교 (Comparison of Algorithms for Sea Surface Current Retrieval using Himawari-8/AHI Data)

  • 김희애;박경애;박지은
    • 대한원격탐사학회지
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    • 제32권6호
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    • pp.589-601
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    • 2016
  • Himawari-8/Advanced Himawari Imager (AHI) 열적외 채널 자료에 Maximum Cross Correlation (MCC), Zero-mean Sum of Absolute Distances (ZSAD), Zero-mean Sum of Squared Distances (ZSSD) 알고리즘을 적용하여 표층 해류를 산출하고, 그 결과를 비교 분석하였다. 각 알고리즘으로 쿠로시오해류 해역의 표층 해류장을 산출한 결과 서로 유사한 양상을 보였다. 오차 발생 비율은 알고리즘에 따른 차이가 거의 나타나지 않았으며, 표층 해류 산출 연산에 소요되는 시간은 ZSAD와 ZSSD 알고리즘이 MCC 알고리즘에 비해 각각 24%, 18% 감소하였다. 산출된 표층 해류는 인공위성 추적 표층 뜰개 자료와 인공위성 고도계 자료로 계산한 표층 해류를 통해 검증하였고, 세 가지 알고리즘의 정확도는 모두 유사한 범위의 값으로 나타났다. 또한 산출된 표층 해류의 정확도는 휘도 온도 수평 구배의 크기와 두 영상 사이의 시간 간격에 의해 영향을 받았다.

Changes in MCSST and Chlorophyll-a Off Sanriku Area (38-43N, 141-l50N) from NOAA/AVHRR and SeaWiFS Data

  • Kim, Myoung-Sun;Asanuma, Ichio
    • 대한원격탐사학회:학술대회논문집
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    • 대한원격탐사학회 1998년도 Proceedings of International Symposium on Remote Sensing
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    • pp.95-100
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    • 1998
  • The purpose of this study is to describe the change of the spring bloom and oceanographic condition. The variation of pigment concentration derived from the satellite ocean color data has been analyzed. According to the movement of blooming area, blooming was very concerned with a rising trend of sea surface temperature and a supply of nutrients. A nutrient rich water carried by the Oyashio encounters with the warm Core ring, where mixings and blooms are observed. We examined the correlation by using the satellite observations of the temperature and chlorophyll-a for the spring seasons (May, June, July) of 1998 the off Sanriku area (38-43N, 141- l50E). Using the SeaWiFS data, we process the data into the level-3, which contains the geophysical value of chlorophyll-a. And chlorophyll-a data is mapped for the water between 110E and 160E, and 15N and 52N with a 0.08 * 0.05 degree grid for each image. And Sea Surface Temperature (SST) data is produced using the AVHRR onboard the NOAA. The SST is derived by the MCSST. Then, the data is mapped for the water as much as chi-a data. And these gridded image was made by detection of each water masses, which are Kuroshio Extension, the warm-core ring and the Oyashlo Intrusion, etc., using those satellite images to determine short term change. Off Sanriku is a place where warm-water pool and the Oyashio at-e mixed. When warm streamer has intruded in cold water, the volume of phytoplankton increases at the tip of warm streamer. Warm water streamer was trigger of occurring blooming. And also, SeaWiFS images provided as much information for the studies of chlorophyll-a concentrations in the surface.

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초여름 韓國 西南海域 植物플랑크톤의 群集構造와 分布 (Community Structure and Spatial Distribution of Phytoplankton in the Southwestern Sea of Korea, in Early Summer)

  • 심재형;박용철
    • 한국해양학회지
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    • 제19권1호
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    • pp.68-81
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    • 1984
  • 한국 서남해역에 있어서 식물플랑크톤의 군집구조와 분포를 밝히기 위하여 1980년 여름에 수평적, 수직적으로 채집한 정량 자료를 분석하였다. 연구해역은 상이한 水塊를 대표하는 상이한 3개의 특징적인 군집을 이루고 있음을 보여준다. 제 1 군집은 대부분 연안성 및 내수성 硅藻類로 구성되어 서남해의 연안 수역을 대표하며, 제 2 군집은 외양성 및 연안성 구조류와 2-3종의 鞭毛藻類로 구성되어 黑潮의 지류로 생각되는 高鹽 水性인 제주 부근의 수역을 대표한다. 제 3 군집은 주로 소형인 鞭毛藻류와 微細藻類로 구성되고 底鹽 수성인 중간 수역을 대표하는 것으로 나타났다. 또한 식물플랑크톤과 환경요인의 수직분포에서 세포수, chlorophyll-a, 및 용존산소등이 특히 계절적인 pycnocline 부근의 수층에서 높은 농도를 보여준다. nanoplankton은 군집내에서 90% 이상에 이를 만큼 점유율을 보여 중요성이 높음을 나타낸다.

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한국 남해의 요각류 및 모악류의 분포와 수괴특성 (The Distributions of Copepods and Chaetognaths in the Southern Waters of Korea and Their Relationship to the Characteristics of Water Masses)

  • 박주석;이삼석;강영실;이병돈;허성회
    • 한국수산과학회지
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    • 제23권3호
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    • pp.245-252
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    • 1990
  • 한국 남해에 분포하는 요각류와 모악류의 수괴 지표성종으로써의 가치를 이용하여 수괴의 특성을 구명하기 위하여 1988년 2, 4 및 8월에 한국 남해안28개 정점에서 NORPAC net를 이용하여 수직 채집한 동물성 부유생물을 분석하였다. 요각류와 모악류중 한국 남해의 주요 수괴 지표성종으로써 Acartia clausi, Centropages abdominalis는 연안 저온성종으로, Sagitta crassa는 연안성종으로, Pleuromamma gracilis, Undinula darwini, Calocalanus plumulosus, Calanopia elliptica와 Sagitta enflata는 난류 외양성종으로, 그리고 Temora discaudata, Centropages furcatus는 난류성종인 것으로 밝혀졌으며, 이들 종의 분포와 수심 30m에서 수온과를 비교 분석하였다. 또한 Cluster분석을 실시하여 수괴의 계절적 변동을 파악하였다. 2월에는 크게 2개의 해역으로 남해 연안 해역과 남해 외양역으로 대별되었으며 4월에는 크게 4개의 해역으로 대별되었다. 8월에는 크게 3개의 해역으로 대별되었으며, 쓰시마난류가 연안으로 강하게 영향을 미침을 나타내었다.

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2015/16 겨울 동아시아-한반도 기후 특성 분석 (Assessment of Climate Variability over East Asia-Korea for 2015/16 Winter)

  • 정지훈;박태원;최자현;손석우;송강현;국종성;김백민;김현경;임소영
    • 대기
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    • 제26권2호
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    • pp.337-345
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    • 2016
  • This paper is to assess the state of climate over East Asia and Korea during 2015/16 winter. There was a distinct intraseasonal climate variation during the period: the record-breaking warmth in December 2015 vs. strong cold surge outbreaks in January 2016. It is suggested that the anomalous warming in December 2015 was contributed by an intensification of Kuroshio anticyclone associated with 2015/16 El $Ni{\tilde{n}}o$ and polar vortex intensification. In January 2016, a strong cold surge outbroke over East Asia bringing severe cold more than two weeks. The cold surge was a blocking-type one which followed extremely negative AO developed from early January. It was suggested that the intensification of cold surge might be contributed indirectly by a strong Arctic warming and MJO activity during the period.

춘계와 하계의 영양염 농도와 그 구성비가 식물플랑크톤의 군집구조에 미치는 영향평가 (The Influence of Nutrients Concentration and the Ratio on Phytoplankton Community Structure during Late Spring and Early Summer in Sagami Bay, Japan)

  • 백승호;시모데신지;한명수;키쿠치토모히코
    • ALGAE
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    • 제23권4호
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    • pp.277-288
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    • 2008
  • The relationship between nutrients and phytoplankton dynamics was investigated daily from 12 April to 22 July 2003 in Sagami Bay, Japan. According to multidimensional scaling (MDS) and cluster analysis, phytoplankton community was divided into four distinct groups. The first group was consisted of centric diatom species, such as Guinardia spp., Detonula spp., Letocylindrus danicus, Skeletonema costatum, Eucampia zodiacus and Chaetoceros spp.. The second and third clusters comprised mainly diatoms and dinoflagellates, respectively. The other cluster was restricted to the samples collected during the last sampling period when the rainfall and river discharge was frequently recorded. Canonical correspondence analysis (CCA) was applied to analyze four groups respectively, which focused on the effects of nutrients concentration and ratio on phytoplankton variations. Based on CCA analysis, most species of centric diatom were negatively correlated with DSi concentrations and Si/N ratio. Nutrients were strongly limited phytoplankton growth during the summer when the rainfall was not observed, whereas river discharge by rainfall and counterclockwise coastal currents (although the surface circulation pattern is often altered by Kuroshio Current, the counterclockwise coastal currents are generally dominant) has brought phytoplankton population accumulation and triggered the micoalgae growth in western part of the bay. Phosphorous (P) was strongly limited after significantly increases in the phytoplankton abundances. However, silicate (Si) was not a major limiting factor for phytoplankton production, since Si/DIN and Si/P ratio did not create any potential stoichiometric limitation. This indicates that high Si availability contributes favorably to the maintenance of diatom ecosystems in Sagami Bay.