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Chaudhuri, A.H., R.M. Ponte, G. Forget, and P. Heimbach, 2012: A comparison of atmospheric re- analysis products over the ocean and implications for uncertainties in air-sea boundary forcing. J. Climate, submitted. |
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Heimbach, P. and M. Losch, 2012: Adjoint sensitivities of sub-ice shelf melt rates to ocean circulation under Pine Island Ice Shelf, West Antarctica. Annals of Glaciology, in press. |
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A. Nguyen, R. Kwok, and D. Menemenlis, 2012: |
A. Nguyen, R. Kwok, and D. Menemenlis, 2012: |
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<a href="http://ecco2.org/manuscripts/2012/NguyenJPO2012.pdf"> |
<a href="http://ecco2.org/manuscripts/2012/NguyenJPO2012.pdf"> |
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Source and pathway of the Western Arctic upper halocline in a data-constrained |
Source and pathway of the Western Arctic upper halocline in a data-constrained |
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coupled ocean and sea ice model.</a> J. Phys. Oceanogr., in press. |
coupled ocean and sea ice model.</a> J. Phys. Oceanogr., in press. |
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Piecuch, C. G., and R. M. Ponte, 2012: Importance of Circulation Changes to Atlantic Heat Storage Rates on Seasonal and Interannual Time Scales. J. Climate, 25, 350-362. |
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Ponte, R. M., 2012: An assessment of deep steric height variability over the global ocean. Geophys. Res. Lett., in press, doi:10.1029/2011GL050681. |
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M. Schodlok, D. Menemenlis, E. Rignot, and M. Studinger, 2012: |
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<a href="http://ecco2.org/manuscripts/2012/Schodlok2012.pdf"> |
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Sensitivity of the ice shelf ocean system to the sub-ice shelf cavity |
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shape measured by NASA IceBridge in Pine Island Glacier, West |
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Antarctica.</a> Annals of Glaciology, in press. |
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N. Vinogradova, R. Ponte, and P. Heimbach, 2011: Dynamics and forcing of sea |
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surface temperature variability on climate time scales. J. Clim., submitted. |
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Wunsch, C., 2012: Covariances and linear predictability of the North Atlantic Ocean. Deep Sea Res., in press. |
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Zanna L., P. Heimbach, A.M. Moore and E. Tziperman, 2012: Upper-ocean singular vectors of the North Atlantic climate with implications for linear predictability and variability. Quart. J. Roy. Met. Soc., in press, doi:10.1002/qj.937. |
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