1 |
기상연구소, 2002. 전 지구 해양/기후 변화 감시 및 예측에 관한 연구-ARGO자료 활용도 제고 기반 연구. 기상연구소, 141 pp
|
2 |
김철호, 1996. 동해 북서해역의 표층해황 특성. 한국해양학회지, 8: 215-220
|
3 |
An, H. S., K. S. Shim, and H. R. Shin, 1994. On the warm eddies in the southwestern part ofthe East Sea (the Japan Sea). J. Oceanol. Soc. Korea, 29: 152-163
|
4 |
Freeland, H. J., and P. F. Cummins, 2005. Argo: A new tool for environmental monitoring and assessment of the world's oceans, an example from the N.E. pacific. Progress in Oceanography, 64: 31-44
DOI
ScienceOn
|
5 |
Guinehut, L., P. Y. Le Traon, G Lamicol, S. Philipps, 2004. Combining Argo and remote-sensing data to estimate the ocean three-dimensional temperature fields-first approach based on simulated observations. J. Marine Systems, 46: 85-98
DOI
ScienceOn
|
6 |
Iwasaka N., T. Suga, K. Takeuchi, K. Mizuno, Y. Takatsuki et al., 2003. Pre-Japan-ARGO: Experimental Observation of Upper and Middle Layers South of the Kuroshio Extension Region Using Profiling Floats. J. Oceanography, 59: 119-127
DOI
|
7 |
Iwao, T., M. Endoh, N. Shikama, and T. Nakano, 2003. Intermediate circulation in the northwestern North Pacific derived from subsurface floats. J. Oceanography, 59: 893-904
DOI
|
8 |
Senjyu, T. and H. Sudo, 1994. The upper portion of the Japan Sea Proper Water; its source and circulation as deduced from isopycnal analysis. J. Oceanography, 50: 663-690
DOI
|
9 |
Senjyu T., 1999. The Japan Sea intermediate water; Its characteristics and circulation. J. Oceanography, 55: 111-122
DOI
|
10 |
Shin, C. W., S. K. Byun, C. S. Kim, and Y. H. Seung, 1998. Southward intrusion of the East Sea Intermediate Water into the Ulleung basin: Observations in 1992 and 1993. J. Oceanol. Soc. Korea, 33: 146-156
|
11 |
Shimizu, Y., T. Iwao, I. Yasuda, S-I, Ito, T. Watanabe, K. Uehara, N. Shikama, and T. Nakano, 2004. Formation Process of North Pacific Intermediate Water Revealed by Profiling Floats Set to Drift on 26.7s Isopycnal Surface. J. Oceanography, 60: 453-462
DOI
|
12 |
Bohrne, L., and U. Send, 2005. Objective analyses of hydrographic data for referencing profiling float salinities in highly variable environments. Deep-Sea Res. II, 52: 651-664
DOI
ScienceOn
|
13 |
Chapman, P., S. F. DiMarco, R. E. Davis, and A. C. Coward, 2003 Flow at intermediate depths around Madagascar based on ALACE float trajectories. Deep-Sea Res. II, 50: 1957-1986
DOI
ScienceOn
|
14 |
Fischer, J., and F. A. Schott, 2002. Labrador Sea Water Tracked by Profiling Floats-From the Boundary Current into the Open North Atlantic. J. Physical Oceanography, 32: 573-584
DOI
ScienceOn
|
15 |
Argo Science Team, 2000. Report of the Argo Science Team 2nd Meeting (AST-2) March 7-9, 2000, Southampton Oceanography Centre, Southampton, U.K
|
16 |
Isobe, A., M. Ando, T. Watanabe, T. Senjyu, S. Sugihara and A. manda, 2002. Freshwater and temperature transports through the Tsushima-Korea Straits. J. Geophysical Res., 107: doi:10.1029/ 2000JC000702
|
17 |
Kim, K. and J. Y. Chung,1984. On the salinity-minimum and dissolved oxygen-maximum layer in the EAst Sea (Sea of Japan). In: Ocean hydrodynamics of the Japan and East China Seas, edited by Ichiye, T.,Elsevier Science Publisher, Amsterdam,pp 55-65
|
18 |
이석우, 1992.한국근해해상지. 집문당, pp 128-131
|
19 |
Oka, E. and K. Ando, 2004. Stability of temperature and conductivity sensors of ARGO profiling floats. J. Oceanography, 60: 253-258
DOI
|
20 |
Bacon, S., L. R.Centurioni, and W. J. Gould, 2001. The evaluation of salinity measurements from PALACE floats. J.Atmospheric and Oceanic Technology, 18: 1258-1266
DOI
ScienceOn
|
21 |
Kim,K., Y G Kim,Y K.Cho, M. Takematsu, and Y. Volkov,1999. Basin-to-Basin and Year-to-Year variation of temperature and salinity characteristics in the East Sea (sea of Japan). J. Oceanography, 55: 103-109
DOI
|
22 |
이동섭, 김기현, 1998. 룹 이용한 이상 저염 대마난류수의 기원 추적 연구. 한국해양학회지-바다, 3: 175-182
|
23 |
Delcroix, T. and R. Murtugudde, 2002. Sea surface salinity changes in the East China Sea during 1997-2001: Influence of the Yangtze River. J. Geophysical. Res., 107: 8008,doi:10.1029/2001JC000893
DOI
|
24 |
Yanagimoto, D., and K. Taira, 2003. Current measurements of the Japan Sea proper water and intermediate water by ALACE floats. J. Oceanography, 59: 359-368
DOI
|
25 |
신홍렬, 변상경, 김철수, 황상철, 신창웅, 1995. 1992년 울릉도 북서부해역에서 관측된 난수성 소용돌이의 구조 특성, 한국해양 학회지, 30: 39-56
|
26 |
국립수산과학원, 2005. 해양조사연보 제53권. 국립수산과학원, 285pp
|
27 |
Wong, A. P. S., G. C. Johnson, and W. B. Owens, 2003. DelayedMode Calibration of Autonomous CTD Profiling Float Salinity Data by -S Climatology. J. Atmospheric and Oceanic Technology, 20: 308-318
DOI
ScienceOn
|
28 |
Ro, Young Jae, 2001. Interactions of Coastal Boundary Currents with Mesoscale Eddies in the East Sea, pp 75-88 in Recent Advances in Marine Science and Technology edited by N. Saxena, Pacon International 2001, Isbn 0-9634343-4-9
|
29 |
Lavender, K. L., W. B. Owens, and R. E. Davis, 2005. The mid-depth circulation of the subpolar North Atlantic Ocean as measured by subsurface floats. Deep-Sea Res. I, 52: 767-785
DOI
ScienceOn
|
30 |
Chang, K. I., W. J. Teague, S. J. Lyu, H. T. Perkins, D. K. Lee, D. R. Watts, Y. B. Kim, D. A. Mitchell, C. M. Lee, and K. Kim, 2004. Circulation and currents in the southwestern East/Japan Sea: Overview and review. Progress in Oceanography, 61: 105-156
DOI
ScienceOn
|
31 |
Kim, Y-G and K. Kim,1999. Intermediate waters in the East/Japan Sea. J. Oceanography, 55: 123-132
DOI
|
32 |
Kang, D. J., S. C. Chang, H. K. Suk, K. R. Kim, H. H. Gi, 1997. Distribution of 137Cs and 239, 240Pu in the Surface Waters of the East Sea (Sea of Japan). Marine Pollution Bulletin, 35: 305-312
DOI
ScienceOn
|
33 |
오경희, 박영규, 석문식, 2004.자동수직물성관측뜰개(ARGO)로 얻은 수온과 염분의 정확도와 안정도.한국해양학회지-바다, 9: 204-211
|
34 |
Durand, F.,and G Reverdin, 2005. A Statistical Method for Correcting Salinity Observations from Autonomous Profiling Floats: An ARGO Perspective. J. Atmospheric and Oceanic Technology, 22: 292-301
DOI
ScienceOn
|
35 |
Ohno, Y, Y Sato, and N. Iwasaka, 2004. The mixed layer depth in the North Pacific as detected by the ARGO floats. OCEANS '04. MTTSIIEEE TECHNO-OCEAN '04, 1491-1495
|