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한인성,이준수 해양환경안전학회 2020 海洋環境安全學會誌 Vol.26 No.3
We examined long-term variations in sea surface temperature (SST) and annual amplitudes of SST around the Korean Peninsula. Two SST data sets with data periods of approximately 51 years and longer than 100 years, respectively, were obtained from the National Institute of Fisheries Science and Japan Meteorological Agency. SST of Korean waters clearly increased during last 51 years (1968-2018), which was 2.5 times higher than the global trend. This significant increasing trend was caused by the dominant increasing SST trend during winter. However, a negative and positive SST anomaly frequently appeared during winter and summer, respectively, in a recent decade. These features of seasonal SST variation have changed the annual amplitude of SST, and resulted in a drastically increasing trend after 2009. Using the longer SST data set, it was revealed that the decreasing SST trend in winter began in the 2000s and the increasing SST trend in summer bagan in the 1990s. During a recent decade, there was a distinctive SST increase in summer, whereas a clear decrease in winter. In summary, the annual amplitude of SST around the Korean Peninsula significantly changed from a decreasing trend to an increasing trend during a recent decade.
Wind-induced Spatial and Temporal Variations in the Thermohaline Front in the Jeju Strait, Korea
한인성,서영상,성기택 한국수산과학회 2013 Fisheries and Aquatic Sciences Vol.16 No.2
We investigated the short-term and local changes in the thermohaline front in the Jeju Strait, Korea, which is usually formed during winter and spring. To do so, we compared Real-Time Observation System by Ferryboat (RTOSF) data with wind data and routinely collected oceanographic data. During February and April 2007, a thermohaline front formed in the Jeju Strait around the 13-14°C isotherms and 33.0-33.5 isohalines. The thermohaline was clearly weakened and began moving southward in mid-March. The variations in the surface temperature and salinity showed a continuous north-south oscillation of the thermohaline front with a period of 3-10 days. The speed of the short-term and local fluctuation of thermohaline front was about 5-30 cm/s. We confirmed these findings by examining the variation in the maximum temperature gradient and 14°C isotherm during the study period. These short-term and local changes had not been previously detected using serial oceanographic and satellite data. Analysis of local wind data revealed a northerly wind fluctuation with a period of 3-10 days, which was clearly related to the short-term and local changes in the thermohaline front. The short-term and local changes of the thermohaline front in the Jeju Strait originated from local changes in the winter monsoon in this area.
Evidence of Vertical Mixing Caused by High Frequency Internal Waves along the Eastern Coast of Korea
한인성,이주,장이현,서영상,성기택 한국수산과학회 2008 Fisheries and Aquatic Sciences Vol.11 No.1
Internal waves and internal tides occur frequently along the eastern coast of Korea. During the spring-tide period in April 2003, the East Korean Warm Current (EKWC) flowed near the Korean East Coast Farming Forecast System (KECFFS; a moored oceanographic measurement system), creating a strong thermocline at the intermediate layer. Weakened stratification and well-mixed water appeared frequently around the KECFFS, with duration of approximately 1 day. The results suggest the following scenario. Baroclinic motion related to the internal tide generated high frequency internal waves around the thermocline. The breaking of those waves then created turbulence around the thermocline. After well-mixed water appeared, a current component with perpendicular direction to the EKWC appeared within the inertial period. The change in stratification around the KECFFS locally broke the geostrophic balance as a transient state. This local vertical mixing formed an ageostrophic current within the inertial period.
한인성,이준수,김주연,홍지연 해양환경안전학회 2019 海洋環境安全學會誌 Vol.25 No.3
During the winter of 2017/2018, significantly low water temperatures were detected around the western and southern coasts of Korea (WSCK). In this period, sea surface temperature (SST) in the Korea Waters was about 2℃ lower than mean temperature. Using the real-time observation system, we analyzed the temporal variation of SST during this period around the western and southern coasts. Low water temperature usually manifested over a period of about 10~20 days. The daily Arctic oscillation index was also similarly detectable with the variation of SST. From the cross-correlation function, we compared two periodic variations, which were SST around the WSCK and the Arctic oscillation index. The cross correlation coefficients between both variations were approximately 0.3~0.4. The time lag of the two time series was about 6 to 7 days. Therefore, significanlyt low water temperatures during winter in the Korean coastal areas usually became detectable 6to7 days after the negative peak of Arctic oscillation.
한인성,성기택,장이현,서영상 한국수산과학회 2008 Fisheries and Aquatic Sciences Vol.11 No.1
Harmful algal blooms (HABs) of Cochlodinium polykrikoides frequently occur around the South Sea of Korea, causing economic losses in coastal breeding grounds. HAB outbreak scale usually changes each year depending on physical, biological and environmental conditions. Relatively large-scale HABs occurred in 1995, 1997, 1999, 2001, 2002 and 2003 with respect to spatial scale, duration and maximum density. Considering HAB scale and temperature distributions around the South Sea, we found that low coastal temperatures in August correspond to enormous HAB outbreaks. Cold waters created by coastal upwellings around the southeastern coast of Korea also corresponded to these outbreaks. Serial oceanographic investigations in August in the South Sea revealed that sea surface temperature anomalies had distinctively negative values when large-scale HAB outbreaks appeared. With regard to temperature differences between the surface and the 30-m layer, there was a tendency for large-scale outbreaks when temperature gradients around the seasonal thermocline weakened.
Nitrided Pressureless Sintering에 의해 제조된 Si<sub>3</sub>N<sub>4</sub>의 산화거동
한인성,천승호,정용희,서두원,이시우,홍기석,우상국,Han, In-Sub,Cheon, Sung-Ho,Jung, Yong-Hee,Seo, Doo-Won,Lee, Shi-Woo,Hong, Kee-Soeg,Woo, Sang-Kuk 한국세라믹학회 2005 한국세라믹학회지 Vol.42 No.1
Oxidtion behavior of $Si_{3}N_{4}$ ceramics with the different porosity by the Nitrided Pressureless Sintering (NPS) were investigated in pure oxygen gas atmosphere at 1000 to $1300^{circ}C$. The thickness of formed oxide film on the surface of silicon nitride ceramics was increased with oxidation time and temperature. The oxide film thickness of 5A5Y5Si and 5A5Y10Si specimens for 100 h at 1300^{circ}C$ was about 10 $\mu$m and 20 $\mu$m, respectively. The oxidation of 5A5Y5Si and 5A5Y10Si specimens follows the parabolic behavior with an apparent activation energy of 215 kJ/mol and 104 kJ/mol, respectively. The flexural strength of 5A5Y5Si specimens after oxidation test for 500 h at 1300^{circ}C were maintained as-received value of 500 ma. On the other hand, that of 5A5Y10Si specimens were decreased about 100 MPa in as-received value. 질화상압동시소결(NPS) 공정에 의해 제조된 기공율이 다른 질화규소 소결체에 대해 $1300^{circ}C$ 순산소 가스분위기에서 산화거동을 조사하였다. 질화규소 세라믹스 표면에 형성된 산화층의 두께는 산화 시간과 온도에 따라 증가되었으며, $1300^{circ}C$에서 100시간 산화시킨 5A5Y5Si와 5A5Y10Si 시편의 산화층 두께는 각각 10$\mu$m와 20$\mu$m이었다. 5A5YSi와 5A5Y10Si 시편의 산화는 각각 215kJ/mol과 104kJ/mol의 활성화 에너지를 갖고 포물선적 거동을 나타내었다. $1300^{circ}C$에서 500시간 산화시킨 후, 5A5Y5Si 시편에 대해 꺾임 강도를 측정한 결과, 초기의 약 500MPa값을 유지하고 있었으며, 반면 5A5Y10Si의 경우에는 초기의 값에서 약 100MPa의 강도저하를 나타내고 있었다.