• 제목/요약/키워드: Sea Surface

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Variations of Sea Level and Sea Surface Temperature in Korean Seas by Topex/Poseidon and NOAA

  • Yoon, Hong-Joo;Kang, Heung-Soon;Lee, Bong-Sic;Jeong, Young-Deok
    • 대한원격탐사학회:학술대회논문집
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    • 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume II
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    • pp.880-883
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    • 2006
  • Altimeter(Topex/Poseidon) and AVHRR(NOAA) data were used to study the variations and correlations of Sea Level(SL) and Sea Surface Temperature (SST) in the North East Asian Seas from November 1993 to May 1998. This region is influenced simultaneously to continental and oceanic climate as the border of the East Sea(Japan Sea). SL and SST have increased gradually every year because the global warming, and presented usually a strong annual variations in Kuroshio extension region with the influence of bottom topography.

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Variations of Sea Level and Sea Surface Temperature in Korean Seas by Topex/Poseidon and NOAA

  • Yoon, Hong-Joo;Kang, Heung-Soon;Cho, Han-Keun
    • 대한원격탐사학회지
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    • 제23권1호
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    • pp.59-63
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    • 2007
  • Altimeter (Topex/Poseidon) and AVHRR (NOAA) data were used to study the variations and correlations of Sea Level (SL) and Sea Surface Temperature (SST) in the North East Asian Seas from November 1993 to May 1998. This region is influenced simultaneously to continental and oceanic climate as the border of the East Sea (Japan Sea). SL and SST have increased gradually every year because the global warming, and presented usually a strong annual variations in Kuroshio extension region with the influence of bottom topography.

1994년 인천 연안역의 열수지 (Heat Budget in Incheon Coastal Area in 1994)

  • 최용규;윤홍주
    • 한국환경과학회지
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    • 제8권3호
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    • pp.293-297
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    • 1999
  • Based on the monthly weather report of Korea Meteorological Administration (KMA) and daily sea surface temperature (SST) in Incheon harbor of National Fisheries Research and Development Institute, heat budget in Incheon coastal area was estimated. The temperature differences between the sea surface and near bottom were nearly within 1$^{\circ}C$. This indicate the mixing from the sea surface and the bottom. The net heat flux through the sea surface and the advection through the inner and outer bay was affected uniformly to the water body in Incheon coastal area. The net heat flux was about 110W/$m^2$ in maximum value on May, about -80W/$m^2$ in minimum on January. The net heat flux through the sea surface from the solar radiation was about 2.35$\times$${10}^5$W during the year. This heat flux flew out the bay through the advection by the same flux.

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비음향신호(난류항적)를 이용한 대잠 탐색 및 감시체계 적용방안 연구 (A Study on Anti-Submarine Surveillance Systems using Submarine's Turbulent Wake)

  • 이용철;임세한;박종진;진종한;강웅;이문진;김윤배
    • 한국군사과학기술학회지
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    • 제15권2호
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    • pp.138-146
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    • 2012
  • Using Shear-free Ship wake theory it was predicted the detectable submarine's turbulent wake on the sea surface was about 12km long when there was no breaking waves on the sea surface. It means that there are sufficient detectable turbulent kinetic energies on the sea surface as well as in the water. In this paper, we have proposed some concepts of non acoustic anti-submarine surveillance systems; SAR for sea surface surveillance, LIDAR for sub-surface surveillance and propelled gliders for under -water surveillance.

Impact of a New Formula on the Fresnel Reflectance on Microwave Remote Sensing

  • Qing, Xu;Yuguang, Liu
    • 대한원격탐사학회:학술대회논문집
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    • 대한원격탐사학회 2003년도 Proceedings of ACRS 2003 ISRS
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    • pp.1340-1342
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    • 2003
  • In microwave remote sensing, the Fresnel reflectance formula is widely used in the sea surface emissivity modeling. As an essential contribution to microwave remote sensing, a new formula on the Fresnel reflectance has been derived based on our understanding of the complex index of refraction and continuity condition of E-M waves at the interface between two mediums. The proposed formula can be used to obtain the emissivity of sea surface, which is useful to retrieve sea surface temperature, sea surface salinity and the brightness temperature. Considering Bragg-resonant scatter, it is useful for the calculation of the normalized radar cross-section, and the retrieval of sea surface wind either.

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Comparative Analysis of Surface Heat Fluxes in the East Asian Marginal Seas and Its Acquired Combination Data

  • Sim, Jung-Eun;Shin, Hong-Ryeol;Hirose, Naoki
    • 한국지구과학회지
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    • 제39권1호
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    • pp.1-22
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    • 2018
  • Eight different data sets are examined in order to gain insight into the surface heat flux traits of the East Asian marginal seas. In the case of solar radiation of the East Sea (Japan Sea), Coordinated Ocean-ice Reference Experiments ver. 2 (CORE2) and the Objectively Analyzed Air-Sea Fluxes (OAFlux) are similar to the observed data at meteorological stations. A combination is sought by averaging these as well as the Climate Forecast System Reanalysis (CFSR) and the National Centers for Environmental Prediction (NCEP)-1 data to acquire more accurate surface heat flux for the East Asian marginal seas. According to the Combination Data, the annual averages of net heat flux of the East Sea, Yellow Sea, and East China Sea are -61.84, -22.42, and $-97.54Wm^{-2}$, respectively. The Kuroshio area to the south of Japan and the southern East Sea were found to have the largest upward annual mean net heat flux during winter, at -460- -300 and at $-370--300Wm^{-2}$, respectively. The long-term fluctuation (1984-2004) of the net heat flux shows a trend of increasing transport of heat from the ocean into the atmosphere throughout the study area.

시뮬레이션을 이용한 마이크로웨이브 도플러 레이더 해면관측법의 평가 (Simulation and Evaluation of Sea Surface Observations Using a Microwave Doppler Radar)

  • 요시다타케로;임창규
    • 한국해양환경ㆍ에너지학회지
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    • 제18권2호
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    • pp.116-122
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    • 2015
  • 해면으로부터의 마이크로웨이브 후방산란 시뮬레이션을 이용하여 마이크로웨이브 도플러 레이더에 의한 파고와 해면 흐름 관측법을 평가하였다. 해면으로부터 후방산란하는 마이크로웨이브의 도플러 스펙트럼은 마이크로웨이브 해면 조사폭과 스펙트럼 해석 시간폭의 영향을 받는다. 본 연구에서는 마이크로웨이브 해면 조사폭과 스펙트럼 해석 시간폭의 영향을 조사하기 위하여, 다양한 파랑과 해면 흐름 조건의 수치 해면 생성과 마이크로웨이브 후방산란 시뮬레이션을 통하여 도플러 스펙트럼을 구하였다. 결과에 의하면 마이크로웨이브 해면 조사폭을 파장의 1/5이하, 스펙트럼 해석 시간폭을 파주기의 1/5이하로 설정하면, 충분한 정도의 파고계측이 가능하다. 또한, 파주기에 비해서 충분히 긴 스펙트럼 해석 시간폭을 설정하면 해면 흐름의 상대유속 계측이 가능하다. 시뮬레이션을 이용하여 마이크로웨이브 도플러 레이더에 의한 해면관측의 적절한 계측방법을 찾을 수 있다.

기후변화에 따른 한국 연근해 어업생산량 변화 분석 (An Analysis of Changes in Catch Amount of Offshore and Coastal Fisheries by Climate Change in Korea)

  • 엄기혁;김홍식;한인성;김도훈
    • 수산경영론집
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    • 제46권2호
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    • pp.31-41
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    • 2015
  • This study aimed to analyze the relationship between sea surface temperature as a climatic element and catch amount of offshore and coastal fisheries in Korea using annual time series data from 1970 to 2013. It also tried to predict the future changes in catch amount of fisheries by climate change. Time series data on variables were estimated to be non-stationary from unit root tests, but one long-term equilibrium relation between variables was found from a cointegration test. The result of Granger causality test indicated that the sea surface temperature would cause directly changes in catch amount of offshore and coastal fisheries. The result of regression analysis on sea surface temperature and catch amount showed that the sea surface temperature would have negative impacts on the catch amount of offshore and coastal fisheries. Therefore, if the sea surface temperature would increase, all other things including the current level of fishing effort being equal, the catch amount of offshore and coastal fisheries was predicted to decrease.

양상태 해수면 음파산란 측정 (Measurements of Bistatic Sea Surface Scattering Signals)

  • 최지웅;나정열;나영남
    • 한국음향학회지
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    • 제20권4호
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    • pp.81-86
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    • 2001
  • 126-kHz양상태 해수면 음파산란 측정을 강원도 삼척시 연안에서 수행하였다. 수평입사각을38%, 52%로 고정시킨 상태에서 트랜스듀서와 청음기의 거리를 변화시키면서 산란각의 변화에 따른 전방산란 신호의 변화를 관찰하였다. 해저면 산란신호와는 달리 해수면 산란신호는 해수면 유동성에 의해서 도달시간 변이와 진폭의 변이를 나타내었으며 신호간의 상관관계도 불규칙적인 경향을 나타내었다. 전방산란강도를 계산하여 Kirchhoff approximation (KA)과 small slope approximation (SSA)을 비교한 결과 두 모델 모두 실측치와 잘 일치하였다.

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열대 및 북태평양에서 ENSO와 관련된 표층수온과 해면고도의 경년 변동성 (Interannual Variabilities of Sea Surface Temperature and Sea Level Anomaly related to ENSO in the Tropical and North Pacific Ocean System)

  • 김응;전동철
    • Ocean and Polar Research
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    • 제30권3호
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    • pp.313-324
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    • 2008
  • In order to understand the variation of ENSO-related oceanic environments in the tropical and North Pacific Ocean, spatio-temporal variations of sea surface temperature anomaly (SSTA) and sea surface height anomaly (SSHA) are analyzed from distributions of complex empirical orthogonal functions (CEOF). Correlations among warm pool variation, southern oscillation index, and ocean surface currents were also examined with respect to interannual variability of the warm pool in western tropical Pacific. Spatio-temporal distributions of the first CEOF modes for SSTA and SSHA indicate that their variabilities are associated with ENSO events, which have a variance over 30% in the North Pacific. The primary reasons for their variabilities are different; SST is predominantly influenced by the change of barrier layer thickness, while SSH fluctuates with the same phase as propagation of an ENSO episode in the zonal direction. Horizontal boundary of warm pool area, which normally centered around $149^{\circ}E$ in the tropics, seemed to be expanded to the middle and eastern tropical regions by strong zonal currents through the mature phase of an ENSO episode.