The Rhines effect on the geographical characteristics of altimeter-observed eddies
-
摘要: Rhines效应是指Rossby波和大湍流(中尺度涡)相互作用,将涡动能量以波的形式传播出去,从而使中尺度涡发生形变,最终消亡的一种动力学机制。本文通过比较海洋里涡特征速度和Rossby长波波速的方法,研究了一种广义的Rhines效应对高度计观测的海洋中尺度涡空间分布特征的影响。结果显示,广义Rhines效应比只考虑行星涡度梯度的传统形式对中尺度涡的分布具有更显著的影响。大部分中尺度涡分布在涡特征速度(Ue)大于由广义Beta值计算的Rossby长波波速(Ucg)的区域。这些涡可以由动能反向串级过程获取能量,成长为振幅和空间尺度较大的涡。热带海域以外的“涡旋沙漠”区域,中尺度涡的数量稀少,强度很弱,大都分布于Uecg的海域。广义Rhines效应可能是这些海域中尺度涡难以成长的动力学机制。Abstract: The Rhines effect may be regarded as an interaction between Rossby waves and turbulence, in which the Rossby waves may radiate away eddy energy when their frequencies are equal or larger than those of the turbulence, thereby deforming and eventually destroying the existing eddies. Through comparing eddy-scale velocity and long Rossby wave phase speed in the oceans, a generalized form of the Rhines effect is examined on the geographical characteristics of altimeter-observed eddies. The results show that the generalized Rhines effect has a much greater influence on eddy characteristics than its classical form, which only considers the simple beta effect due to the meridional gradient of planetary vorticity. The largest amount of eddies are detected in regions where eddy-scale velocity is larger than the critical Rossby-wave phase speed considering a generalized beta effect. The eddies in those regions can grow via an inverse kinetic energy cascade and have much larger amplitudes and sizes. The "eddy desert" regions outside of the tropical oceans, which have far fewer detected eddies and much weaker eddy amplitudes, lie in areas where the eddy-scale velocity is less than the critical Rossby-wave phase speed. In those regions, the generalized Rhines effect may be a possible mechanism of suppressing eddy growth.
-
Key words:
- Rhines effect /
- mesoscale eddy /
- Rossby wave /
- energy cascade /
- eddy desert
-
Charney J G. 1947. The dynamics of long waves in a baroclinic westerly current. Journal of Meteorology, 4(5):135-162 Chelton D B, deSzoeke R A, Schlax M G, et al. 1998. Geographical variability of the first baroclinic rossby radius of deformation. Journal of Physical Oceanography, 28(3):433-460 Chelton D B, Schlax M G, Samelson R M, et al. 2007. Global observations of large oceanic eddies. Geophysical Research Letters, 34(15):L15606 Chelton D B, Schlax M G, Samelson R M. 2011. Global observations of nonlinear mesoscale eddies. Progress in Oceanography, 91(2):167-216 Chemke R, Kaspi Y. 2015. The latitudinal dependence of atmospheric jet scales and macroturbulent energy cascades. Journal of the Atmospheric Sciences, 72(10):3891-3907 Chemke R, Kaspi Y. 2016. The latitudinal dependence of the oceanic barotropic eddy kinetic energy and macroturbulence energy transport. Geophysical Research Letters, 43(6):2723-2731 Eady E. 1949. Long waves and cyclone waves. Tellus, 1(3):33-52 Ferrari R, Wunsch C. 2009. Ocean circulation kinetic energy:reservoirs, sources, and sinks. Annual Review of Fluid Mechanics, 41(1):253-282 Galperin B, Sukoriansky S, Dikovskaya N, et al. 2006. Anisotropic turbulence and zonal jets in rotating flows with a β-effect. Nonlinear Processes in Geophysics, 13(1):83-98 Galperin B, Sukoriansky S, Dikovskaya N. 2010. Geophysical flows with anisotropic turbulence and dispersive waves:flows with a β-effect. Ocean Dynamics, 60(2):427-441 Gill A E, Green J S A, Simmons A J. 1974. Energy partition in the large-scale ocean circulation and the production of mid-ocean eddies. Deep Sea Research and Oceanographic Abstracts, 21(7):499-528 Holloway G, Hendershott M C. 1977. Stochastic closure for nonlinear Rossby waves. Journal of Fluid Mechanics, 82(4):747-765 Pascual A, Faugère Y, Larnicol G, et al. 2006. Improved description of the ocean mesoscale variability by combining four satellite altimeters. Geophysical Research Letters, 33(2):L02611 Phillips N A. 1954. Energy transformations and meridional circulations associated with simple baroclinic waves in a two-level, quasi-geostrophic model. Tellus, 6(3):273-286 Qiu Bo, Chen Shuiming, Klein P, et al. 2014. Seasonal mesoscale and submesoscale eddy variability along the North Pacific Subtropical Countercurrent. Journal of Physical Oceanography, 44(12):3079-3098 Luo D, Zhong L, Franzke C. 2015. Inverse Energy Cascades in an Eddy-Induced NAO-Type Flow:Scale Interaction Mechanism. Journal of the Atmospheric Sciences, 72(9):3417-3448 Rhines P B. 1975. Waves and turbulence on a beta-plane. Journal of Fluid Mechanics, 69(3):417-443 Sasaki H, Klein P, Qiu Bo, et al. 2014. Impact of oceanic-scale interactions on the seasonal modulation of ocean dynamics by the atmosphere. Nature Communications, 5:5636, doi: 10.1038/ncomms6636 Scott R B, Wang Faming. 2005. Direct evidence of an oceanic inverse kinetic energy cascade from satellite altimetry. Journal of Physical Oceanography, 35(9):1650-1666 Smith K S. 2004. A local model for planetary atmospheres forced by small-scale convection. Journal of Atmospheric Sciences, 61(12):1420-1433 Smith K S. 2007. The geography of linear baroclinic instability in Earth's oceans. Journal of Marine Research, 65(5):655-683 Stammer D. 1997. Global characteristics of ocean variability estimated from regional TOPEX/POSEIDON altimeter measurements. Journal of Physical Oceanography, 27(8):1743-1769 Stammer D, Wunsch C. 1999. Temporal changes in eddy energy of the oceans. Deep Sea Research Part Ⅱ:Topical Studies in Oceanography, 46(1-2):77-108 Sukoriansky S, Dikovskaya N, and Galperin B. 2007. On the arrest of inverse energy cascade and the Rhines scale. Journal of the Atmospheric Sciences, 64(9):3312-3326 Theiss J. 2004. Equatorward energy cascade, critical latitude, and the predominance of cyclonic vortices in geostrophic turbulence. Journal of Physical Oceanography, 34(7):1663-1678 Theiss J. 2006. A generalized Rhines effect and storms on Jupiter. Geophysical Research Letters, 33(8):L08809 Tulloch R, Marshall J, Smith K S. 2009. Interpretation of the propagation of surface altimetric observations in terms of planetary waves and geostrophic turbulence. Journal of Geophysical Research:Oceans, 114(C2):C02005, doi: 10.1029/2008JC005055 Tulloch R, Marshall J, Hill C, et al. 2011. Scales, growth rates, and spectral fluxes of baroclinic instability in the ocean. Journal of Physical Oceanography, 41(6):1057-1076 Vallis G K, Maltrud M E. 1993. Generation of mean flows and jets on a beta plane and over topography. Journal of Physical Oceanography, 23(7):1346-1362 Wang shihong, Liu Zhiliang, Pang Chongguang. 2015. Geographical distribution and anisotropy of the inverse kinetic energy cascade, and its role in the eddy equilibrium processes. Journal of Geophysical Research:Oceans, 120(7):4891-4906 Williams G P. 1978. Planetary circulations. I-Barotropic representation of Jovian and terrestrial turbulence. Journal of the Atmospheric Sciences, 35(8):1399-1426 Wunsch C. 1997. The vertical partition of oceanic horizontal kinetic energy. Journal of Physical Oceanography, 27(8):1770-1794
点击查看大图
计量
- 文章访问数: 1120
- HTML全文浏览量: 47
- PDF下载量: 867
- 被引次数: 0