Winter mixed layer (ML) characteristics in the North Pacific Ocean are examined and compared between Argo floats in 2004 and 2005 and the World Ocean Atlas 2001 (WOA01) climatology for a series of named water masses, North Pacific Tropical Water, Eastern Subtropical Mode Water (ESTMW), North Pacific Subtropical Mode Water, and Light and dense Central Mode Water (DCMW). The WOA01 is found to be in good agreement with Argo in terms of water mass volumes, average temperature-salinity (T-S) properties, and outcrop areas. The exception to this is for the central mode waters, especially DCMW, whose outcropping is shown to be much more intermittent than is apparent in the WOA01 and whose T-S properties are vary from what is shown in the WOA01. Distributions of ML T-S properties measured by floats are examined within the outcropping areas defined by the WOA01 and show some shifting of T-S characteristics. In 2005, all the water masses were warmer than climatology on average, with DCMW being highest at about 1oC. Similar results were found for the 2004 Argo data except ESTMW and DCMW which were slightly cooler than climatology. Differences between float data and climatology were also examined for the entire North Pacific. This analysis showed the winter North Pacific ML to be fresher and warmer than climatology in both 2004 and 2005, with magnitudes of 0.3-0.4 degC and 0.06-0.07. This warming and freshening was apparent throughout a large area of the tropics and northeastern North Pacific, but in the mode water formation areas the trends were less clear.