Now showing items 1-8 of 8

  • Assimilating long-term hydrographic information into an eddy-permitting model of the North Atlantic 

    Wright, D. G., K. R. Thompson, and Y. Lu. 2006. "Assimilating long-term hydrographic information into an eddy-permitting model of the North Atlantic." Journal of Geophysical Research 111(C9): 09022-C09022. DOI: 10.1029/2005JC003200
    No abstract available.
  • Calculation of UV attenuation and colored dissolved organic matter absorption spectra from measurements of ocean color 

    This article first appeared in: Johannessen, S. C., W. L. Miller, and J. J. Cullen. 2003. "Calculation of UV attenuation and colored dissolved organic matter absorption spectra from measurements of ocean color." Journal of Geophysical Research 108(C9): 13-13. DOI: 10.1029/2000JC000514
    No abstract available.
  • Carbon disulfide in the North Atlantic and Pacific Oceans 

    Xie, Huixiang, and Robert M. Moore. 1999. "Carbon disulfide in the North Atlantic and Pacific Oceans." Journal of Geophysical Research 104(C3): 5393-5402. DOI: 10.1029/1998JC900074
    No abstract available.
  • Methyl iodide in the NW Atlantic; spatial and seasonal variation 

    This article first appeared in: Wang, Lu, Robert M. Moore, and John J. Cullen. 2009. "Methyl iodide in the NW Atlantic; spatial and seasonal variation." Journal of Geophysical Research 114(C7): 07007-Citation C07007. DOI: 10.1029/2007JC004626
    While the global ocean is an important source of atmospheric methyl iodide (CH (sub 3) I), the major producers of CH (sub 3) I within the ocean remain unclear. During a seasonal study in the NW Atlantic, the relationship ...
  • Rate of growth of isolated bubbles in sediments with a diagenetic source of methane 

    Boudreau, Bernard P., Bruce S. Gardiner, and Bruce D. Johnson. 2001. "Rate of growth of isolated bubbles in sediments with a diagenetic source of methane." Limnology and Oceanography 46(3): 616-622.
    Observation of bubbles in estuarine and coastal sediments indicates that bubbles at or below 10 cm depth grow on seasonal time scales (May-October). In order to determine the controls on this growth rate, we have constructed ...
  • Return periods of extreme sea levels from short records 

    Middleton, J. F., and K. R. Thompson. 1986. "Return periods of extreme sea levels from short records." Journal of Geophysical Research 91: 11707-16. DOI: 10.1029/JC091iC10p11707
    Extreme sea levels usually arise from a combination of the tides (assumed here to be deterministic) and storm surges (assumed stochastic). The authors show how tide and surge statistics derived from short (~1 year) records ...
  • Sea level and circulation variability of the Gulf of Carpentaria; influence of the Madden-Julian Oscillation and the adjacent deep ocean 

    Oliver, E. C. J., and K. R. Thompson. 2011. "Sea level and circulation variability of the Gulf of Carpentaria; influence of the Madden-Julian Oscillation and the adjacent deep ocean." Journal of Geophysical Research 116(C2): 02019-Citation C02019. DOI: 10.1029/2010JC006596
    The Madden-Julian Oscillation (MJO) is a significant contributing factor to intraseasonal variability in both the tropical and extratropical atmosphere and ocean. Sea level and circulation variations in the Gulf of Carpentaria ...
  • Trichloroethylene and tetrachlorethylene in Atlantic waters 

    Moore, Robert M.. 2001. "Trichloroethylene and tetrachlorethylene in Atlantic waters." Journal of Geophysical Research 106(C11): 27-27,143. DOII: 10.1029/2000JC000374
    No abstract available.