Hurricane Gilbert
Some figures from Shay et al. 1998.
Figure 2. Three-dimensional view of the velocity vectors and temperature structure in the upper 750 m observed from the deployment of AXCPs from NOAA WP-3D in the western Gulf of Mexico during Wake 1 experiment one day after the passage of Hurricane Gilbert (17 Sept 1988). Temperature bar (°C) is located in the lower left, the velocity scale in lower right, and the best track of Gilbert is depicted by the black line.
Figure 8. Isotherm depths for yeardays 200 (left panels) and 300 (right panels) for 18°C, 15°C, 8°C and error levels based on objective analysis of the MMS survey data acquired from research vessels and aircraft (SAIC 1989).
Figure 9. Objectively-analyzed temperatures (°C), and the geostrophic current vectors re: 750 m (cm s-1) (left panels) and the stream function (ψ) (dyn-m) (right panels) superposed on the normalized relative vorticity field (% of f) at 30, 50, 80 and 200 m on yearday 300 based upon survey data acquired as part of the MMS sponsored program in the western Gulf of Mexico shown (SAIC 1989).
Figure 10. As in Fig. 9 except for yearday 200.
Figure 11. Geostrophic vectors (cm s-1) re: 750 m superposed on the normalized relative vorticities (% of f) from objectively analyzing the Wake 1 (Yearday 262) of hurricane Gilbert AXCP data at a) 30 m, b) 50 m c) 80 m and d) 200 m in the western Gulf of Mexico. Normalized relative vorticity field above and below f are depicted by the red and purple on the color bar for each panel.
ReferencesL.K. Shay, A.J. Mariano, S.D. Jacob, E.H. Ryan, Mean and Near-Inertial Ocean Current Responce to Hurricane Gilbert J. Physical Oceanography, Vol. 28, No. 5, pp. 858-889, May 1998. ( doi:10.1175/1520-0485(1998)028<0858:MANIOC>2.0.CO;2)