Model constraints on the anthropogenic carbon budget of the Arctic Ocean

For the TrOCA method we identified low inventory estimates in the South Atlantic (Fig. 3b) due to the relatively large amount of negative C ant estimates in deep waters (Fig. The

(1997) iceberg model, devel- oped by MA10, is coupled to an eddy-permitting global im- plementation of the Nucleus for European Modelling of the Ocean (NEMO) (Madec, 2008), to

In this study, the WOCE current meter database and the 1/6
-resolution CLIPPER velocity fields were processed identically to provide 806 comparable pairs of synoptic,

In the same way, unresolved spatial correlations between tempera- ture and horizontal velocity will contribute horizontal density fluxes that should be included in ocean models

TABLE 4-7: DENSITIES AND EXCESS MOLAR VOLUMES OF AQUEOUS N-EPD SOLUTION AND PURE LIQUID AT ATMOSPHERIC PRESSURE... TABLE 4-8: TEMPERATURE DEPENDENT REDLICH-KISHTER PARAMETERS FOR

In summary, this work introduces ion mobility spectrometry coupled with mass spectrometry analysis for the structural study of soluble organic matter by presenting

model results using ship emission inventories A, B and C, as well as the model sim- ulation without ship emissions and the satellite data from MODIS and AMSR-E for average cloud