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revision 1.2 by dimitri, Mon Jan 17 22:50:33 2011 UTC revision 1.5 by dimitri, Tue Jan 18 04:27:15 2011 UTC
# Line 14  climate variability.</a> J. Clim., in pr Line 14  climate variability.</a> J. Clim., in pr
14  </li></ul>  </li></ul>
15    
16  <ul><li>  <ul><li>
17    G. Forget, G. Maze, M. Buckley, and J. Marshall, 2011:
18    Estimated Seasonal Cycle of North Atlantic Eighteen Degree Water Volume.
19    J. Phys. Oceanogr., in press.
20    </li></ul>
21    
22    <ul><li>
23    P. Heimbach, C. Wunsch, R. Ponte, G. Forget, C. Hill, and J. Utke, 2011:
24    Timescales and Regions of the Sensitivity of Atlantic Meridional Volume and
25    Heat Transport Magnitudes: Toward Observing System Design. Deep Sea Res. II
26    (special issue on the AMOC), in press.
27    </li></ul>
28    
29    <ul><li>
30  E. Hill, D. Enderton, P. Heimbach, and C. Hill, 2011: SPGrid: A  E. Hill, D. Enderton, P. Heimbach, and C. Hill, 2011: SPGrid: A
31  numerical grid generation program for domain decomposed geophysical  numerical grid generation program for domain decomposed geophysical
32  fluid dynamics models. Mon. Weather Rev., submitted.  fluid dynamics models. Unpublished manuscript.
33  </li></ul>  </li></ul>
34    
35  <ul><li>  <ul><li>
# Line 73  Azores Current eddy energy. Geophys. Res Line 86  Azores Current eddy energy. Geophys. Res
86  </li></ul>  </li></ul>
87    
88  <ul><li>  <ul><li>
89    Y. Xu and L. Fu, 2011: Global variability of the wavenumber spectrum of
90    oceanic mesoscale turbulence. J. Phys. Oceanogr., in press,
91    doi:10.1175/2010JPO4558.1.
92    </li></ul>
93    
94    <ul><li>
95    L. Zanna, P. Heimbach, A. Moore, and E. Tziperman, 2011: Optimal
96    excitation of interannual Atlantic meridional overturning circulation
97    variability. J. Climate, in press, doi:10.1175/2010JCLI3610.1.
98    </li></ul>
99    
100    <ul><li>
101  L. Zanna, P. Heimbach, A. Moore and E. Tziperman, 2011. Analysis of the  L. Zanna, P. Heimbach, A. Moore and E. Tziperman, 2011. Analysis of the
102  predictability and variability of the Atlantic ocean in response to optimal  predictability and variability of the Atlantic ocean in response to optimal
103  surface excitation.  Quart. J. Roy. Met. Soc., submitted.  surface excitation.  Quart. J. Roy. Met. Soc., submitted.
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