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revision 1.20 by dimitri, Sat Mar 16 20:09:05 2013 UTC revision 1.22 by heimbach, Sun Mar 17 00:50:05 2013 UTC
# Line 6  calving law. Geophys. Res. Lett., 39, L1 Line 6  calving law. Geophys. Res. Lett., 39, L1
6  </li></ul>  </li></ul>
7    
8  <ul><li>  <ul><li>
9    A. Condron and I. Renfrew,
10    2012: <a href="http://www.nature.com/ngeo/journal/v6/n1/full/ngeo1661.html">
11    The impact of polar mesoscale storms on northeast Atlantic Ocean
12    circulation.</a> Nature Geoscience, 6, 34-37.
13    </li></ul>
14    
15    <ul><li>
16  A. Condron and P. Winsor,  A. Condron and P. Winsor,
17  2012: <a href="http://ecco2.org/manuscripts/2012/CondronWinsor2012.pdf">  2012: <a href="http://ecco2.org/manuscripts/2012/CondronWinsor2012.pdf">
18  Meltwater routing and the Younger Dryas.</a> PNAS 1207381109.  Meltwater routing and the Younger Dryas.</a> PNAS 1207381109.
# Line 21  terrigenous CDOM in the Arctic Ocean, J. Line 28  terrigenous CDOM in the Arctic Ocean, J.
28  <ul><li>  <ul><li>
29  P. Heimbach and M. Losch, 2012: Adjoint sensitivities of sub-ice shelf melt  P. Heimbach and M. Losch, 2012: Adjoint sensitivities of sub-ice shelf melt
30  rates to ocean circulation under Pine Island Ice Shelf, West  rates to ocean circulation under Pine Island Ice Shelf, West
31  Antarctica. Annals of Glaciology, 54, 59-69.  Antarctica. Annals of Glaciology, 54, 59-69, doi:10.3189/2012/AoG60A025.
32  </li></ul>  </li></ul>
33    
34  <ul><li>  <ul><li>
# Line 99  discharge.</a> Annals of Glaciology, 53, Line 106  discharge.</a> Annals of Glaciology, 53,
106  L. Zanna, P. Heimbach, A. Moore, and E. Tziperman, 2012: Upper-ocean  L. Zanna, P. Heimbach, A. Moore, and E. Tziperman, 2012: Upper-ocean
107  singular vectors of the North Atlantic climate with implications for  singular vectors of the North Atlantic climate with implications for
108  linear predictability and variability. Quart. J. Roy. Met. Soc., 138,  linear predictability and variability. Quart. J. Roy. Met. Soc., 138,
109  500-513.  500-513, doi:10.1002/qj.937.
110  </li></ul>  </li></ul>
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