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1    
2    <ul><li>
3    R. Abernathey, J. Marshall, and D. Ferreira, 2011: The dependence of Southern
4    Ocean meridional overturning on wind stress. J. Phys. Oceanogr., 41,
5    2261-2278.
6    </li></ul>
7    
8  <ul><li>  <ul><li>
9  J. Campin, C. Hill, H. Jones, and J. Marshall, 2011:  J. Campin, C. Hill, H. Jones, and J. Marshall, 2011:
10  <a href="http://www-paoc.mit.edu/paoc/papers/superparam.pdf">  <a href="http://www-paoc.mit.edu/paoc/papers/superparam.pdf">
11  Superparameterization in ocean modeling: application to deep  Super-parameterization in ocean modeling: Application to deep
12  convection.</a> Ocean Modeling, in press.  convection.</a> Ocean Modelling, 36, 90-101.
13  </li></ul>  </li></ul>
14    
15  <ul><li>  <ul><li>
# Line 34  J. Phys. Oceanogr., 41(2), 269-286, doi: Line 41  J. Phys. Oceanogr., 41(2), 269-286, doi:
41  </li></ul>  </li></ul>
42    
43  <ul><li>  <ul><li>
44    H. Gennerich and H. Villinger, 2011:
45    <a href="http://ecco2.org/manuscripts/2011/Gennerich_2011.pdf">
46    Deciphering the ocean bottom pressure variation in the Logatchev
47    hydrothermal field at the eastern flank of the Mid-Atlantic Ridge.</a>
48    Geochemistry Geophysics Geosystems, 12, doi:10.1029/2010GC003441.
49    </li></ul>
50    
51    <ul><li>
52  P. Heimbach, C. Wunsch, R. Ponte, G. Forget, C. Hill, and J. Utke, 2011:  P. Heimbach, C. Wunsch, R. Ponte, G. Forget, C. Hill, and J. Utke, 2011:
53  Timescales and Regions of the Sensitivity of Atlantic Meridional Volume and  Timescales and Regions of the Sensitivity of Atlantic Meridional Volume and
54  Heat Transport Magnitudes: Toward Observing System Design. Deep Sea Res. II  Heat Transport Magnitudes: Toward Observing System Design. Deep Sea Res. II
55  (special issue on the AMOC), in press, doi:10.1016/j.dsr2.2010.10.065  (Topical issue on "Climate and the AMOC"), 58(17-18), 1858-1879, doi:10.1016/j.dsr2.2010.10.065.
56  </li></ul>  </li></ul>
57    
58  <ul><li>  <ul><li>
# Line 45  M. Manizza, M. Follows, S. Dutkiewicz, D Line 60  M. Manizza, M. Follows, S. Dutkiewicz, D
60  C. Hill, B. Peterson, R. Key, 2011:  C. Hill, B. Peterson, R. Key, 2011:
61  <a href="http://ecco2.org/manuscripts/2011/Manizza2011.pdf">  <a href="http://ecco2.org/manuscripts/2011/Manizza2011.pdf">
62  A model of the Arctic Ocean carbon cycle.</a>  A model of the Arctic Ocean carbon cycle.</a>
63  J. Geophys. Res., in press.  J. Geophys. Res., 116, C12020, doi:10.1029/2011JC006998.
64    </li></ul>
65    
66    <ul><li>
67    I. Cerovecki, L.D. Talley, and M.R. Mazloff, 2011:
68    A Comparison of Southern Ocean Air-Sea Buoyancy Flux from an Ocean State Estimate with Five Other Products.
69    J. Clim., 24(24), 6283-6306, <a href="http://dx.doi.org/10.1175/2011JCLI3858.1">doi:10.1175/2011JCLI3858.1</a>
70  </li></ul>  </li></ul>
71    
72  <ul><li>  <ul><li>
# Line 57  doi:10.1029/2010JC006573 Line 78  doi:10.1029/2010JC006573
78  </li></ul>  </li></ul>
79    
80  <ul><li>  <ul><li>
81    Piecuch, C. G., and R. M. Ponte, 2011: Mechanisms of interannual steric sea level variability, Geophys. Res. Lett., 38, L15605, doi:10.1029/2011GL048440.
82    </li></ul>
83    
84    <ul><li>
85    Rampal, P., J. Weiss, C. Dubois & J.-M. Campin 2011: IPCC climate models do not capture Arctic sea ice drift acceleration: Consequences in terms of projected sea ice thinning and decline, J. Geophys. Res., vol. 116, C00D07, doi:10.1029/2011JC007110.
86    </li></ul>
87    
88    <ul><li>
89    Roquet, F., C. Wunsch, and G. Madec, 2011: On the patterns of wind-power input to the ocean circulation. J. Phys. Oceanogr., 41, 2328-2342, <a href="http://dx.doi.org/10.1175/JPO-D-11-024.1">doi:10.1175/JPO-D-11-024.1</a>.
90    </ul></li>
91    
92    <ul><li>
93  G. Spreen, R. Kwok, and D. Menemenlis, 2011:  G. Spreen, R. Kwok, and D. Menemenlis, 2011:
94  <a href="http://ecco2.org/manuscripts/2011/Spreen2011.pdf">  <a href="http://ecco2.org/manuscripts/2011/Spreen2011.pdf">
95  Trends in Arctic sea ice drift and role of wind forcing:  Trends in Arctic sea ice drift and role of wind forcing:
# Line 71  Ocean.</a> Estuaries and Coasts, doi:10. Line 104  Ocean.</a> Estuaries and Coasts, doi:10.
104  </li></ul>  </li></ul>
105    
106  <ul><li>  <ul><li>
107    R. Tulloch, C. Hill, and O. Jahn, 2011:
108    <a href="http://ocean.mit.edu/~tulloch/Publications/tulloch_etalagu11.pdf">
109    Possible spreadings of buoyant plumes and local coastline
110    sensitivities using flow syntheses from 1992 to 2007.</a> Geophysical
111    Monograph Series, 195, 245-255.
112    </li></ul>
113    
114    <ul><li>
115  R. Tulloch, J. Marshall, C. Hill, and K. Smith, 2011:  R. Tulloch, J. Marshall, C. Hill, and K. Smith, 2011:
116  <a href="http://ocean.mit.edu/~tulloch/Publications/tulloch_etaljpo10.pdf">  <a href="http://ocean.mit.edu/~tulloch/Publications/tulloch_etaljpo11.pdf">
117  Scales, growth rates and spectral fluxes of baroclinic instability in  Scales, growth rates and spectral fluxes of baroclinic instability in
118  the ocean.</a> J. Phys. Oceanogr., in press.  the ocean.</a> J. Phys. Oceanogr., 41, 1057-1076.
119  </li></ul>  </li></ul>
120    
121  <ul><li>  <ul><li>
122  C. Ubelmann and L. Fu, 2011:  C. Ubelmann and L. Fu, 2011:
123  <a href="http://ecco2.org/manuscripts/2011/UbelmannFu2011.pdf">  <a href="http://ecco2.org/manuscripts/2011/UbelmannFu2011a.pdf">
124  Vorticity structures in the tropical Pacific from a numerical simulation.</a>  Vorticity structures in the Tropical Pacific from a numerical simulation.</a>
125  J. Phys. Oceanogr., submitted.  J. Phys. Oceanogr., 41, 1455.
126  </li></ul>  </li></ul>
127    
128  <ul><li>  <ul><li>
129  N. Vinogradova, R. Ponte, and P. Heimbach, 2011: Dynamics and forcing of sea  C. Ubelmann and L. Fu, 2011:
130  surface temperature variability on climate time scales. J. Clim., submitted.  <a href="http://ecco2.org/manuscripts/2011/UbelmannFu2011b.pdf">
131    Cyclonic eddies formed at the Pacific tropical instability wave fronts.</a>
132    J. Geophys. Res., 116, C12021.
133  </li></ul>  </li></ul>
134    
135  <ul><li>  <ul><li>
136  D. Volkov and L. Fu, 2011: Mechanism for the interannual variability of the  D. Volkov and L. Fu, 2011:
137  Azores Current eddy energy. Geophys. Res. Lett., submitted.  <a href="http://ecco2.org/manuscripts/2011/VolkovFu2011.pdf">
138    Interannual variability of the Azores Current strength and eddy energy
139    in relation to atmospheric forcing.</a> J. Geophys. Res., 116, C11011.
140  </li></ul>  </li></ul>
141    
   
142  <ul><li>  <ul><li>
143  Wunsch, C., 2011: Covariances and linear predictability of the North Atlantic Ocean. submitted.  Wunsch, C., 2011:
144    The decadal mean circulation and Sverdrup balance.
145    J. Marine Res., 69, 417-434.
146  </li></ul>  </li></ul>
147    
148  <ul><li>  <ul><li>
149  Wunsch, C., 2011:  Y. Xu and L. Fu, 2011:
150  The decadal mean circulation and Sverdrup balance.  <a href="http://ecco2.org/manuscripts/2011/XuFu2011.pdf">
151  J. Marine Res., in press.  Global variability of the wavenumber spectrum of
152    oceanic mesoscale turbulence.</a> J. Phys. Oceanogr., 41, 802-809.
153  </li></ul>  </li></ul>
154    
155  <ul><li>  <ul><li>
156  Y. Xu and L. Fu, 2011: Global variability of the wavenumber spectrum of  Y. Xu, L. Fu, and R. Tulloch, 2011: The global characteristics of the
157  oceanic mesoscale turbulence. J. Phys. Oceanogr., in press,  wavenumber spectrum of ocean surface wind. J. Phys. Oceanogr., 41,
158  doi:10.1175/2010JPO4558.1.  1576-1582.
159  </li></ul>  </li></ul>
160    
161  <ul><li>  <ul><li>
162  L. Zanna, P. Heimbach, A. Moore, and E. Tziperman, 2011: Optimal  L. Zanna, P. Heimbach, A. Moore, and E. Tziperman, 2011: Optimal
163  excitation of interannual Atlantic meridional overturning circulation  excitation of interannual Atlantic meridional overturning circulation
164  variability. J. Climate, in press, doi:10.1175/2010JCLI3610.1.  variability. J. Climate, 24(2), 413-423, doi:10.1175/2010JCLI3610.1.
165  </li></ul>  </li></ul>
166    
 <ul><li>  
 L. Zanna, P. Heimbach, A. Moore and E. Tziperman, 2011. Analysis of the  
 predictability and variability of the Atlantic ocean in response to optimal  
 surface excitation.  Quart. J. Roy. Met. Soc., submitted.  
 </li></ul>  

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