未來工作

當黑潮受到暖渦影響時，黑潮的傳輸量增強，同時也有向東偏移的現象發 生。而黑潮產生偏移雖然和風應力旋度及熱通量有關，那麼和渦漩的相關性又 是如何呢?此外，本研究定義的 Eddy-Poor Year 還是會有渦漩產生，並且通過觀 察中的測線，若是能夠建立一個理想的實驗模式，能夠分別探討有渦漩以及沒 有渦漩的情況，首先觀察只有黑潮本來就有的傳輸量大小變化及主軸路徑的改 變，再加入自訂的渦漩來探討渦漩對黑潮的影響，如此一來，我們能夠更深入 了解副熱帶反流區的渦漩對黑潮的傳輸量，以及黑潮主軸的影響。

70

參考文獻

Chang, Y.-L. and L.-Y. Oey (2011), Interannual and seasonal variations of Kuroshio transport east of Taiwan inferred from 29 years of tide-gauge data. Geophysical Research Letters, doi:10.1029/2011GL047062

Chang, Y.-L., and L.-Y. Oey (2014), Analysis of STCC eddies using the Okubo–Weiss parameter on model and satellite data, Ocean Dynamics, 64(2), 259-271, doi:10.1007/s10236-013-0680-7.

Chang, Y.-L., Y. Miyazawa and X. Guo (2015), Effects of the STCC eddies on the Kuroshio based on the 20-years JCOPE2 reanalysis result., Prog. Oceanogr., http://dx.doi.org/10.1016/j.pocean.2015.04.006

Chao, S.-Y. (1991), Circulation of the East China Sea, a numerical study, Journal of the Oceanographical Society of Japan, 46(6), 273-295, doi:10.1007/BF02123503.

Chelton, D. B., M. G. Schlax, R. M. Samelson, and R. A. de Szoeke (2007), Global observations of large oceanic eddies, Geophysical Research Letters, 34(15), L15606, doi:10.1029/2007GL030812.

Chelton, D. B., M. G. Schlax, and R. M. Samelson (2011), Global observations of nonlinear mesoscale eddies, Progress in Oceanography, 91(2), 167-216, doi:http://dx.doi.org/10.1016/j.pocean.2011.01.002.

Gawarkiewicz, G., S. Jan, P.F.J. Lermusiaux, J.L. McClean, L. Centurioni, K. Taylor, B. Cornuelle, T.F. Duda, J. Wang, Y.J. Yang, T. Sanford, R.-C. Lien, C. Lee, M.-A.

Lee, W. Leslie, P.J. Haley Jr., P.P. Niiler, G. Gopalakrishnan, P. Velez-Belchi, D.-K. Lee, and Y.Y. Kim. “Circulation and Intrusions Northeast of Taiwan: Chasing and Predicting Uncertainty in the Cold Dome.” Oceanography 24.4 (2011): 110–

121. Web. © 2011 The Oceanography Society, Inc.

71

Guo, X., H. Hukuda, Y. Miyazawa, and T. Yamagata (2003), A Triply Nested Ocean Model for Simulating the Kuroshio—Roles of Horizontal Resolution on JEBAR, Journal of Physical Oceanography, 33(1), 146-169,

doi:10.1175/1520-0485(2003)033<0146:ATNOMF>2.0.CO;2.

Hwang, C., C.-R. Wu, and R. Kao (2004), TOPEX/Poseidon observations of mesoscale eddies over the Subtropical Countercurrent: Kinematic characteristics of an anticyclonic eddy and a cyclonic eddy, Journal of Geophysical Research: Oceans, 109(C8), C08013, doi:10.1029/2003JC002026.

Ichikawa, K. (2001), Variation of the Kuroshio in the Tokara Strait Induced by Meso-Scale Eddies, Journal of Oceanography, 57(1), 55-68, doi:10.1023/A:1011174720390.

Ichikawa, K., R. Tokeshi, M. Kashima, K. Sato, T. Matsuoka, S. Kojima, and S. Fujii (2008), Kuroshio variations in the upstream region as seen by HF radar and satellite altimetry data, International Journal of Remote Sensing, 29(21), 6417-6426, doi:10.1080/01431160802175454.

Johns, W. E., T. N. Lee, D. Zhang, R. Zantopp, C.-T. Liu, and Y. Yang (2001), The Kuroshio East of Taiwan: Moored Transport Observations from the WOCE PCM-1 Array, Journal of Physical Oceanography, 3PCM-1(4), PCM-103PCM-1-PCM-1053, doi:PCM-10.PCM-1PCM-175/PCM-1520- doi:10.1175/1520-0485(2001)031<1031:TKEOTM>2.0.CO;2.

Miyazawa, Y., R. Zhang, X. Guo, H. Tamura, D. Ambe, J.-S. Lee, A. Okuno, H.

Yoshinari, T. Setou, and K. Komatsu (2009), Water mass variability in the western North Pacific detected in a 15-year eddy resolving ocean reanalysis, Journal of Oceanography, 65(6), 737-756, doi:10.1007/s10872-009-0063-3.

72

Okubo, A. (1970), Horizontal dispersion of floatable particles in the vicinity of velocity singularities such as convergences, Deep Sea Research and Oceanographic Abstracts, 17(3), 445-454, doi:http://dx.doi.org/10.1016/0011-7471(70)90059-8.

Qiu, B., K. A. Kelly, and T. M. Joyce (1991), Mean flow and variability in the Kuroshio Extension from Geosat altimetry data, Journal of Geophysical Research: Oceans, 96(C10), 18491-18507, doi:10.1029/91JC01834.

Qiu, B., R. B. Scott, and S. Chen (2008), Length Scales of Eddy Generation and Nonlinear Evolution of the Seasonally Modulated South Pacific Subtropical Countercurrent, Journal of Physical Oceanography, 38(7), 1515-1528, doi:10.1175/2007JPO3856.1.

Qiu, B., and S. Chen (2010), Interannual Variability of the North Pacific Subtropical Countercurrent and Its Associated Mesoscale Eddy Field, Journal of Physical Oceanography, 40, 213–225.

doi: http://dx.doi.org/10.1175/2009JPO4285.1

Qiu, B., and S. Chen (2011), Effect of Decadal Kuroshio Extension Jet and Eddy Variability on the Modification of North Pacific Intermediate Water, Journal of Physical Oceanography, 41(3), 503-515, doi:10.1175/2010JPO4575.1.

Robinson, A. R. (Ed.) (1983), Eddies in Marine Science, 609 pp., Springer, New York.

Soeyanto, E., X. Guo, J. Ono, and Y. Miyazawa (2014), Interannual variations of Kuroshio transport in the East China Sea and its relation to the Pacific Decadal Oscillation and mesoscale eddies, J. Geophys. Res. Oceans, 119, 3595–3616, doi:10.1002/2013JC009529.

Sverdrup, H. U. (1947), Wind-Driven Currents in a Baroclinic Ocean; with Application to the Equatorial Currents of the Eastern Pacific, Proceedings of the National Academy of Sciences of the United States of America, 33(11), 318-326.

73

Wang, J., and L.-Y. Oey (2014), Inter-annual and decadal fluctuations of the Kuroshio in East China Sea and connection with surface fluxes of momentum and heat, Geophys. Res. Lett., 41, 8538–8546, doi:10.1002/2014GL062118.

Weiss, J. (1991), The dynamics of enstrophy transfer in two-dimensional hydrodynamics, Physica D: Nonlinear Phenomena, 48(2–3), 273-294, doi:http://dx.doi.org/10.1016/0167-2789(91)90088-Q.

Yang, Y., C.-T. Liu, J.-H. Hu, and M. Koga (1999), Taiwan Current (Kuroshio) and Impinging Eddies, Journal of Oceanography, 55(5), 609-617, doi:10.1023/A:1007892819134.

Zhang, D., T. N. Lee, W. E. Johns, C.-T. Liu, and R. Zantopp (2001), The Kuroshio East of Taiwan: Modes of Variability and Relationship to Interior Ocean Mesoscale Eddies, Journal of Physical Oceanography, 31(4), 1054-1074, doi:10.1175/1520-0485(2001)031<1054:TKEOTM>2.0.CO;2.