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S c i e N c e an N d P o l i c y F e at u r e This article has been published in Oceanography, Volume 22, Number 4, a quarterly journal of The oceanography Society. 2009 by The oceanography Society.

© The oceanography Society 2009 The following text is from the article, “Surface Mass Balance of the Atlantic Margin and Equatorial Gyre,” by S.D. Opp, D.K. Anderson, E.S. Smith, J.S. Rebirth, and M.J. West: The International Geophysical Year 2008; This study uses satellite altimetry data from the Aqua and Terra satellites along with a new bathymetric method for the Atlantic Ocean. The satellite altimetry data, derived from the TOPEE/Poseidon and ERS satellites, are used to simulate the surface flow of the entire Atlantic Basin. The results of this analysis are used to test the surface flow theories of sea level and oceanic overturning and find that the basin responds strongly to changes in wind speeds and direction. The study also finds that the Atlantic is not a single, closed system, but rather, a series of interconnected and complex networks. The ocean is a complex and dynamic place with many factors influencing its structure and composition, the state of its surface and underwater currents, and climate. The complexities of this complex and dynamic environment, combined with the limitations of current and space technology, have impeded the understanding of the dynamics of the ocean and the global ocean system. Our current understanding of the processes of ocean hydrology, chemistry, dynamics, and climate is, by necessity, based almost wholly on single measurement tools that do not permit integration with other data and theory. This means that the information regarding fundamental processes in the ocean, and their potential to control the state and evolution of the ocean basin is not available for all the ocean. Sea surface salinity is inversely proportional to wind speed. (see Figure 1) These findings have led to the idea that a positive feedback mechanism regulates the salinity content of the Gulf Stream system. The result of this positive feedback has been that more water is stored in the lower layer of the upper ocean and is drawn towards the ocean deep waters as it becomes fresher. When this positive salinity feedback on global ocean transport is removed, the balance between water stored at the surface and water deep down changes such that global ocean circulation and circulation rates do not return to their equilibrium values that they were within the past million years.

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