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Ocean Science An interactive open-access journal of the European Geosciences Union
Ocean Sci., 6, 775-787, 2010
https://doi.org/10.5194/os-6-775-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
 
24 Aug 2010
Seasonal cycles of surface layer salinity in the Pacific Ocean
F. M. Bingham1, G. R. Foltz2, and M. J. McPhaden3 1Center for Marine Science, Univ. of North Carolina Wilmington, 601 S. College Rd., Wilmington, NC 28403-5928, USA
2Joint Institute for the Study of Atmosphere and Ocean, Univ. of Washington, 3737 Brooklyn Ave NE, P.O. Box 355672, Seattle, WA 98105-5672, USA
3NOAA/Pacific Marine Environmental Laboratory, 7600 Sand Point Way NE, Seattle, WA 98115, USA
Abstract. The seasonal variability of surface layer salinity (SLS) is examined in the Pacific Ocean between 40° S and 60° N using a variety of data sources. Significant seasonal cycles were found in 5 regions: 1) The western North Pacific, 2) The northeastern North Pacific and Alaska gyre, 3) the intertropical convergence zone (ITCZ), 4) an area of the central North Pacific north of the Hawaiian Islands, 5) the central South Pacific along 10–20° S. Amplitudes range from 0.1 to > 0.5. The largest amplitudes are in the tropical band and the western North Pacific. Maximum salinity is obtained in late (northern) winter in the western North Pacific, late winter and early spring in the northeastern North Pacific, early summer in the ITCZ area, late summer and early fall in the central North Pacific area and (austral) winter in the central South Pacific. Large areas of the Pacific have no significant seasonal variation in SLS.

Seasonal variability of evaporation rate, precipitation rate and the difference between them (E-P) were calculated from the OAFlux and Global Precipitation Climatology Project datasets. Typical amplitudes of E-P are 0.1–1 × 10−4 kg m−2 s−1. The seasonal variability of E-P is largely dominated by variability in evaporation in the western North Pacific and precipitation elsewhere. The largest amplitudes are in areas along the edge of the western North Pacific and in the far eastern tropical Pacific around 10° N. Phases in these areas indicate maximum E-P in mid- to late winter in these areas of large amplitude. The closest correspondence between E-P and SLS is in the ITCZ. E-P was combined with seasonal variation of the mixed-layer depth to calculate the freshwater flux forcing term of the SLS balance equation. The term was found to be similar in magnitude and distribution to E-P. Some other terms of the SLS balance were calculated. Horizontal advection was found to have seasonal cycles in a region near the equator. Entrainment was found to be mostly not significant except for a small region along 2.5–7.5° N in the eastern Pacific.

Averaged spatially over large areas in the western North Pacific, ITCZ, South Pacific and northern North Pacific, the seasonal cycle is mostly a balance between changes in SLS and E-P, with entrainment and advection playing relatively minor roles.

This work highlights the potentially significant role of surface salinity in the hydrologic cycle and in subtropical mode water formation. It can also help to interpret measurements that will soon be available from the Aquarius and SMOS (Soil Moisture and Ocean Salinity) satellite missions.


Citation: Bingham, F. M., Foltz, G. R., and McPhaden, M. J.: Seasonal cycles of surface layer salinity in the Pacific Ocean, Ocean Sci., 6, 775-787, https://doi.org/10.5194/os-6-775-2010, 2010.
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