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$\begin{figure} \par\includegraphics[width=8.8cm,clip]{3170fig1.eps} \end{figure}$ Figure 1: Tilting and break-up of (isotropic) turbulent eddy due to the shearing by shear flow ${\vec u} = U_0(x) {\hat y} = -x {{\cal A}} {\hat y}$ . The wavenumber in the x direction increases as $k_y {\cal A}t$ , linearly proportional to time t.
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In the text

$\begin{figure} \par\includegraphics[width=8.8cm,clip]{3170fig2.eps} \end{figure}$ Figure 2: Tilting and break-up of turbulent eddy driven by plumes due to the shearing by radial differential rotation ${\vec u} = U_0(x) {\hat y} = -{\cal A}x {\hat y}$ . The wavenumber in the x direction again increases as $k_y {\cal A}t$ , linearly proportional to time t. The turbulent eddy is almost uniform in x with $k_x/k_y \ll 1$ initially at t=0, but gradually develops radial dependences as the shearing continues.
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In the text

$\begin{figure} \par\includegraphics[width=8.8cm,clip]{3170fig1.eps} \end{figure}$	Figure 1: Tilting and break-up of (isotropic) turbulent eddy due to the shearing by shear flow ${\vec u} = U_0(x) {\hat y} = -x {{\cal A}} {\hat y}$ . The wavenumber in the x direction increases as $k_y {\cal A}t$ , linearly proportional to time t.
Open with DEXTER