PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

The response of cyclonic eddies to typhoons based on satellite remote sensing data for 2001-2014 from the South China Sea

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Eddies are known to be affected by typhoons, and in recent years, the general three-dimensional structure, as well as features of the spatial and temporal distributions of eddies have been determined. However, the type of eddy that is most likely to be affected by a typhoon remains unclear. In this paper, quantitative and qualitative methods were used to study the eddies that are most sensitive to upper-ocean tropical cyclones (TCs) from the perspective of eddy characteristics, and the quantitative results showed that not all eddies were enhanced under the influence of typhoons. Enhancement of the eddy amplitude (Amp), radius (Rad), area (A), or eddy kinetic energy (EKE) accounted for 92.3% of the total eddy within the radius of the typhoon. Qualitative analyses showed the following: First, eddies located on different sides of the typhoon tracks were differently affected, as eddies on the left side were more intensely affected by the typhoon than eddies on the right side, and second, eddies with short lifespans or small radii were more susceptible to the TCs.
Czasopismo
Rocznik
Strony
265--275
Opis fizyczny
Bibliogr. 35 poz., tab., wykr.
Twórcy
autor
  • College of Information Science and Engineering, Ocean University of China, Qingdao, China
  • Laboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China
  • College of Information Science and Engineering, Ocean University of China, Qingdao, China
autor
  • College of Information Science and Engineering, Ocean University of China, Qingdao, China
  • Laboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China
autor
  • College of Information Science and Engineering, Ocean University of China, Qingdao, China
Bibliografia
  • [1] Chelton, D. B., Gaube, P., Schlax, M. G., Early, J. J., Samelson, R. M., 2011a. The influence of nonlinear mesoscale eddies on near-surface oceanic chlorophyll. Science 334 (6054), 328-332, http://dx.doi.org/10.1126/science.1208897.
  • [2] Chelton, D. B., Schlax, M. G., Samelson, R. M., 2011b. Global observations of nonlinear mesoscale eddies. Prog. Oceanogr. 91 (2), 167-216, http://dx.doi.org/10.1016/j.pocean.2011.01.002.
  • [3] Chen, G., Gan, J., Xie, Q., Chu, X., Wang, D., Hou, Y., 2012. Eddy heat and salt transports in the South China Sea and their seasonal modulations. J. Geophys. Res.-Oceans. 117 (C5), http://dx.doi. org/10.1029/2011JC007724.
  • [4] Chiang, T., Wu, C., Oey, L., 2011. Typhoon Kai-Tak: an ocean's perfect storm. J. Phys. Oceanogr. 41 (1), 221-233, http://dx.doi.org/10.1175/2010JPO4518.1.
  • [5] Chow, C., Hu, J., Centurioni, L. R., Niiler, P. P., 2008. Mesoscale Dongsha Cyclonic Eddy in the northern South China Sea by drifter and satellite observations. J. Geophys. Res. 113 (C4), http://dx.doi.org/10.1029/2007JC004542.
  • [6] Du, Y., Wu, D., Liang, F., Yi, J., Mo, Y., He, Z., Pei, T., 2016. Major migration corridors of mesoscale ocean eddies in the South China Sea from 1992 to 2012. J. Mar. Syst. 158, 173-181, http://dx.doi.org/10.1016/j.jmarsys.2016.01.013.
  • [7] Gordon, A. L., Shroyer, E., Murty, V. S. N., 2017. An intrathermocline Eddy and a tropical cyclone in the Bay of Bengal. Sci Rep.-UK 7, 46218, http://dx.doi.org/10.1038/srep46218.
  • [8] Guan, S., Zhao, W., Huthnance, J., Tian, J., Wang, J., 2014. Observed upper ocean response to typhoon Megi (2010) in the Northern South China Sea. J. Geophys. Res.-Oceans. 119 (5), 3134-3157, http://dx.doi.org/10.1002/2013JC009661.
  • [9] Hisaki, Y., 2003. Horizontal variability of near-inertial oscillations associated with the passage of a typhoon. J. Geophys. Res. 108 (C12), 12 pp., http://dx.doi.org/10.1029/2002JC001683.
  • [10] Hu, J. Y., Kawamura, H., 2004. Detection of cyclonic eddy generated by looping tropical cyclone in the northern South China Sea: a case study. Acta Oceanol. Sin. 23 (2), 213-224.
  • [11] Jaimes, B., Shay, L. K., Halliwell, G. R., 2011. The response of quasigeostrophic oceanic vortices to tropical cyclone forcing. J. Phys. Oceanogr. 41 (10), 1965-1985, http://dx.doi.org/10.1175/JPO-D-11-06.1.
  • [12] Knaff, J. A., DeMaria, M., Sampson, C. R., Peak, J. E., Cummings, J., Schubert, W. H., 2013. Upper oceanic energy response to tropical cyclone passage. J. Clim. 26 (8), 2631-2650, http://dx.doi.org/10.1175/JCLI-D-12-00038.1.
  • [13] Lin, I. I., Wu, C. C., Emanuel, K. A., Lee, I. H., Wu, C. R., Pun, I. F., 2005. The interaction of Supertyphoon Maemi (2003) with a warm ocean eddy. Mon. Weather Rev. 133 (9), 2635-2649, http://dx.doi.org/10.1175/MWR3005.1.
  • [14] Lin, S., Zhang, W., Shang, S., Hong, H., 2017. Ocean response to typhoons in the western North Pacific: composite results from Argo data. Deep-Sea Res. Pt. I 123, 62-74, http://dx.doi.org/10.1016/j.dsr.2017.03.007.
  • [15] Liu, W. T., Xie, X. S., 1999. Spacebased observations of the seasonal changes of South Asian monsoons and oceanic responses. Geophys. Res. Lett. 26 (10), 1473-1476, http://dx.doi.org/10.1029/1999GL900289.
  • [16] Liu, Y., Chen, G., Sun, M., Liu, S., Tian, F., 2016. A parallel SLA-based algorithm for global mesoscale Eddy identification. J. Atmos. Ocean. Tech. 33 (12), 2743-2754, http://dx.doi.org/10.1175/JTECH-D-16-0033.1.
  • [17] Liu, S., Sun, L., Wu, Q., Yang, Y., 2017. The responses of cyclonic and anticyclonic eddies to typhoon forcing: the vertical temperature-salinity structure changes associated with the horizontal convergence/divergence. J. Geophys. Res.-Oceans. 122 (6), 4974-4989, http://dx.doi.org/10.1002/2017JC012814.
  • [18] Lu, Z., Wang, G., Shang, X., 2016. Response of a preexisting cyclonic ocean Eddy to a Typhoon. J. Phys. Oceanogr. 46 (8), 2403-2410, http://dx.doi.org/10.1175/JPO-D-16-0040.1.
  • [19] Mahadevan, A., Thomas, L. N., Tandon, A., 2008. Comment on “eddy/wind interactions stimulate extraordinary mid-ocean plankton blooms”. Science 320 (5875), 448, http://dx.doi.org/10.1126/science.1152111.
  • [20] Patnaik, K. V. K. R., Maneesha, K., Sadhuram, Y., Prasad, K. V. S. R., Murty, T. V. R., Brahmananda Rao, V., 2014. East India Coastal Current induced eddies and their interaction with tropical storms over Bay of Bengal. J. Oper. Oceanogr. 7 (1), 58-68, http://dx.doi.org/10.1080/1755876X.2014.11020153.
  • [21] Potter, H., Drennan, W. M., Graber, H. C., 2017. Upper ocean cooling and air-sea fluxes under typhoons: a case study. J. Geophys. Res.- Oceans. 122 (9), 7237-7252, http://dx.doi.org/10.1002/2017JC012954.
  • [22] Price, J. F., 1981. Upper ocean response to a hurricane. J. Phys. Oceanogr. 11 (2), 153-175, http://dx.doi.org/10.1175/1520-0485(1981)011<0153:UORTAH>2.0.CO;2.
  • [23] Shang, S., Li, L., Sun, F., Wu, J., Hu, C., Chen, D., Ning, X., Qiu, Y., Zhang, C., Shang, S., 2008. Changes of temperature and biooptical properties in the South China Sea in response to Typhoon Lingling, 2001. Geophys. Res. Lett. 35 (10), 6 pp., http://dx.doi.org/10.1029/2008GL033502.
  • [24] Shang, X., Zhu, H., Chen, G., Xu, C., Yang, Q., 2015. Research on cold core eddy change and phytoplankton bloom induced by typhoons: case studies in the South China Sea. Adv. Meteorol. 2015, 1-19, http://dx.doi.org/10.1155/2015/340432.
  • [25] Shay, L. K., Goni, G. J., Black, P. G., 2000. Effects of a warm oceanic feature on hurricane opal. Mon. Weather. Rev. 128 (5), 1366-1383, http://dx.doi.org/10.1175/1520-0493(2000)128<1366:EOAWOF>2.0.CO;2.
  • [26] Sun, L., Li, Y., Yang, Y., Wu, Q., Chen, X., Li, Q., Li, Y., Xian, T., 2014. Effects of super typhoons on cyclonic ocean eddies in the western North Pacific: a satellite data-based evaluation between 2000 and 2008. J. Geophys. Res.-Oceans. 119 (9), 5585-5598, http://dx.doi.org/10.1002/2013JC009575.
  • [27] Sun, J., Oey, L., Chang, R., Xu, F., Huang, S., 2015. Ocean response to typhoon Nuri (2008) in western Pacific and South China Sea. Ocean Dynam. 65 (5), 735-749, http://dx.doi.org/10.1007/s10236-015-0823-0.
  • [28] Sun, M., Tian, F., Liu, Y., Chen, G., 2017. An improved automatic algorithm for global eddy tracking using satellite altimeter data. Remote Sens.-Basel. 9 (3), 206, http://dx.doi.org/10.3390/rs9030206.
  • [29] Wang, G., 2003. Mesoscale eddies in the South China Sea observed with altimeter data. Geophys. Res. Lett. 30 (21), 6 pp., http://dx.doi.org/10.1029/2003GL018532.
  • [30] Wang, G., Ling, Z., Wang, C., 2009. Influence of tropical cyclones on seasonal ocean circulation in the South China Sea. J. Geophys. Res. 114 (C10), http://dx.doi.org/10.1029/2009JC005302 11 pp.
  • [31] Wang, H., Wang, D., Liu, G., Wu, H., Li, M., 2012. Seasonal variation of eddy kinetic energy in the South China Sea. Acta Oceanol. Sin. 31 (1), 1-15, http://dx.doi.org/10.1007/s13131-012-0170-7.
  • [32] Xiu, P., Chai, F., Shi, L., Xue, H., Chao, Y., 2010. A census of eddy activities in the South China Sea during 1993-2007. J. Geophys. Res. 115 (C3), http://dx.doi.org/10.1029/2009JC005657 15 pp.
  • [33] Xu, C., Shang, X., Huang, R. X., 2011. Estimate of eddy energy generation/dissipation rate in the world ocean from altimetry data. Ocean Dynam. 61 (4), 525-541, http://dx.doi.org/10.1007/s10236-011-0377-8.
  • [34] Zhang, Z., Tian, J., Qiu, B., Zhao, W., Chang, P., Wu, D., Wan, X., 2016. Observed 3D structure, generation, and dissipation of oceanic mesoscale eddies in the South China Sea. Sci. Rep.-UK 6 (1), 11 pp., http://dx.doi.org/10.1038/srep24349.
  • [35] Zheng, Z., Ho, C., Zheng, Q., Lo, Y., Kuo, N., Gopalakrishnan, G., 2010. Effects of preexisting cyclonic eddies on upper ocean responses to Category 5 typhoons in the western North Pacific. J. Geophys. Res. 115 (C9), 11 pp., http://dx.doi.org/10.1029/ 2009JC005562.
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-6dc5ff54-3c7e-4993-a9cd-bbaa5dedebc9
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.