By Thomas ( Ed. ) Abbondi

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The atmospheric pressure ionization mass spectrometer laboratory container is in the foreground. Credit: Barry Huebert, University of Hawaii 33 This project is an innovative step toward a better understanding of air-sea interaction, in particular, gas fluxes between the ocean and atmosphere. The investigators have modified the newly developed atmospheric pressure ionization mass spectrometer (APIMS) for shipboard applications for measuring airsea exchange of trace gas species important to global climate.

Earlier models had suggested that the North Pole enjoyed a subtropical climate during this period; this has been confirmed by carbon isotopic analyses of ACEX sediment cores. The cores also challenge conventional wisdom about the opening of the Arctic Ocean basin, suggesting that the basin is older than predicted by plate tectonic reconstructions. A surprising discovery was more than 140 meters of laminated, organic-rich sediment that could indicate conditions conducive to oil formation in adjacent, 34 deeper basins.

Htm 27 Top image credit: © 2009 Digital Vision, Gety Images force behind ocean current patterns. Temperature and salinity are the key variables affecting seawater density and drive vertical ocean circulation; density increases with increasing salinity or decreasing temperature. 1 The warming or cooling of the ocean’s surface can have far-reaching effects on the atmosphere. 2 Researchers use the CCSM and other global climate models to predict El Niño events, which can have profound impacts on human activities.

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Advanced Techniques: Painting and Weathering Military Vehicles by Thomas ( Ed. ) Abbondi

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