<div dir="ltr"><div><a href="http://www.ncl.ucar.edu/">http://www.ncl.ucar.edu/</a><br><br>Click "Examples" ===> <a href="http://www.ncl.ucar.edu/Applications/">http://www.ncl.ucar.edu/Applications/</a><br><br>on right hand side, Under "Data Analysis", click "Eliassen-Palm flux; Brunt/Ri/Eady"<br><br>See the 6.4.0 text box. See: "...can be downloaded from <b>here</b> " ..... Click on <b>here</b><br></div><div><br>;-------------------------------<br>undef("eady_growth_rate")<br>function eady_growth_rate(th:numeric, u:numeric, z:numeric, lat:numeric, opt[1]:integer, ndimz[1]:integer)<br>;<br>; Maximum Eady Growth Rate <br>;<br>; Reference:<br>; R. S. Lindzen and Brian Farrell, 1980:<br>; A Simple Approximate Result for the Maximum Growth Rate of Baroclinic Instabilities.<br>; J. Atmos. Sci., 37, 1648–1654.<br>; <a href="http://dx.doi.org/10.1175/1520-0469(1980)037">http://dx.doi.org/10.1175/1520-0469(1980)037</a><1648:ASARFT><a href="http://2.0.CO">2.0.CO</a>;2<br>;<br>; Simmonds, I., and E.-P. Lim (2009):<br>; Biases in the calculation of Southern Hemisphere mean baroclinic eddy growth rate<br>; Geophys. Res. Lett., 36, L01707<br>; doi:10.1029/2008GL036320<br>;<br>; Vallis, G.K. (2006)<br>; Atmospheric and Oceanic Dynamics: Fundamentals and Large-Scale Circulation<br>; Cambridge Univ. Press, New York.<br><br>[SNIP]<br><br></div><div>Cheers ... <br></div></div><div class="gmail_extra"><br><div class="gmail_quote">On Mon, Jan 25, 2016 at 1:57 PM, Xi Chang <span dir="ltr"><<a href="mailto:xi.chang01@gmail.com" target="_blank">xi.chang01@gmail.com</a>></span> wrote:<br><blockquote class="gmail_quote" style="margin:0 0 0 .8ex;border-left:1px #ccc solid;padding-left:1ex"><div dir="ltr">Hallo NCL developer,<div><br></div><div>Could I have a new contributed subroutines that contain</div><div>this function?</div><div>Thanks</div><span class="HOEnZb"><font color="#888888"><div><br></div><div>Chang.</div></font></span></div>
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