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revision 1.21 by dimitri, Sat Mar 16 22:05:04 2013 UTC revision 1.23 by dimitri, Tue Jul 23 01:28:38 2013 UTC
# Line 19  Meltwater routing and the Younger Dryas. Line 19  Meltwater routing and the Younger Dryas.
19  </li></ul>  </li></ul>
20    
21  <ul><li>  <ul><li>
22    V. Dansereau, 2012: Ice shelf-ocean interactions in a general circulation model:
23    melt-rate modulation due to mean flow and tidal currents. M.Sc. Thesis, MIT-WHOI Joint Program, Cambridge, MA.
24    </li></ul>
25    
26    <ul><li>
27  M. Granskog, C. Stedmon, P. Dodd, R. Amon, A. Pavlov, L. de Steur, and  M. Granskog, C. Stedmon, P. Dodd, R. Amon, A. Pavlov, L. de Steur, and
28  E. Hansen, 2012: Characteristics of colored dissolved organic matter (CDOM) in  E. Hansen, 2012: Characteristics of colored dissolved organic matter (CDOM) in
29  the Arctic outflow in the Fram Strait: Assessing the changes and fate of  the Arctic outflow in the Fram Strait: Assessing the changes and fate of
# Line 28  terrigenous CDOM in the Arctic Ocean, J. Line 33  terrigenous CDOM in the Arctic Ocean, J.
33  <ul><li>  <ul><li>
34  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
35  rates to ocean circulation under Pine Island Ice Shelf, West  rates to ocean circulation under Pine Island Ice Shelf, West
36  Antarctica. Annals of Glaciology, 54, 59-69.  Antarctica. Annals of Glaciology, 54, 59-69, doi:10.3189/2012/AoG60A025.
37  </li></ul>  </li></ul>
38    
39  <ul><li>  <ul><li>
# Line 106  discharge.</a> Annals of Glaciology, 53, Line 111  discharge.</a> Annals of Glaciology, 53,
111  L. Zanna, P. Heimbach, A. Moore, and E. Tziperman, 2012: Upper-ocean  L. Zanna, P. Heimbach, A. Moore, and E. Tziperman, 2012: Upper-ocean
112  singular vectors of the North Atlantic climate with implications for  singular vectors of the North Atlantic climate with implications for
113  linear predictability and variability. Quart. J. Roy. Met. Soc., 138,  linear predictability and variability. Quart. J. Roy. Met. Soc., 138,
114  500-513.  500-513, doi:10.1002/qj.937.
115  </li></ul>  </li></ul>
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