Now showing items 33-52 of 151

  • Deep structure of the ocean-continent transition in the southern Iberia Abyssal Plain from seismic refraction profiles: Ocean Drilling Program (Legs 149 and 173) transect 

    Chian, DP, KE Louden, TA Minshull, and RB Whitmarsh. 1999. "Deep structure of the ocean-continent transition in the southern Iberia Abyssal Plain from seismic refraction profiles: Ocean Drilling Program (Legs 149 and 173) transect." Journal of Geophysical Research-Solid Earth 104(B4): 7443-7462. DOI:10.1029/1999JB900004
    We present a wide-angle seismic refraction study of an 80x40 km region of the southern Iberia Abyssal Plain, south of Galicia Bank. An intersecting grid of two E-W and four NS wide-angle reflection/refraction profiles is ...
  • Deep structure of the ocean-continent transition in the southern Iberia Abyssal Plain from seismic refraction profiles: The IAM-9 transect at 40 degrees 20 ' N 

    Dean, SM, TA Minshull, RB Whitmarsh, and KE Louden. 2000. "Deep structure of the ocean-continent transition in the southern Iberia Abyssal Plain from seismic refraction profiles: The IAM-9 transect at 40 degrees 20 ' N." Journal of Geophysical Research-Solid Earth 105(B3): 5859-5885. DOI:10.1029/1999JB900301
    We present a crust and mantle velocity structure for the West Iberia passive continental margin derived from a 320-km-long wide-angle seismic profile acquired in the southern Iberia Abyssal Plain. We observe a 170-km-wide ...
  • A description of water types on the Mackenzie Shelf of the Beaufort Sea during winter 

    Moore, R. M., H. Melling, and K. R. Thompson. 1992. "A description of water types on the Mackenzie Shelf of the Beaufort Sea during winter." Journal of Geophysical Research.C.Oceans 97(C8): 12607-12618. DOI:10.1029/92JC00842
    For a number of years during the 1980s, observations of the physical and chemical properties of seawater in the southeastern Beaufort Sea have been acquired in late winter. The most complete data set, from 1987, has been ...
  • A description of water types on the Mackenzie Shelf of the Beaufort Sea during winter 

    Moore, R. M., H. Melling, and K. R. Thompson. 1992. "A description of water types on the Mackenzie Shelf of the Beaufort Sea during winter." Journal of Geophysical Research.C.Oceans 97(C8): 12607-12618. DOI:10.1029/92JC00842
    For a number of years during the 1980s, observations of the physical and chemical properties of seawater in the southeastern Beaufort Sea have been acquired in late winter. The most complete data set, from 1987, has been ...
  • The detection of coastal-trapped waves 

    Haines, J. W., K. R. Thompson, and D. P. Wiens. 1991. "The detection of coastal-trapped waves." Journal of Geophysical Research 96: 2593-7. DOI:10.1029/90JC02218
    The authors outline a simple method for estimating the cross-spectral matrix of coastal-trapped wave amplitudes, A, from a set of oceanographic observations. Specifically, they propose that A may be estimated by ...
  • Dichloromethane in North Atlantic waters 

    Moore, RM. 2004. "Dichloromethane in North Atlantic waters." Journal of Geophysical Research-Oceans 109(C9): 09004-C09004. DOI:10.1029/2004JC002397
    [1] Dichloromethane is an atmospheric trace gas that has a tropospheric lifetime on the order of 5 months and has major anthropogenic sources. Evidence has been presented for an oceanic source. This paper reports measurements ...
  • Direct observations of diel biological CO2 fixation on the Scotian Shelf, northwestern Atlantic Ocean 

    Thomas, H., S. E. Craig, B. J. W. Greenan, W. Burt, et al. 2012. "Direct observations of diel biological CO2 fixation on the Scotian Shelf, northwestern Atlantic Ocean." Biogeosciences 9(6): 2301-2309.
    Much of the variability in the surface ocean's carbon cycle can be attributed to the availability of sunlight, triggering surface heat flux and photosynthesis, which in turn regulate the biogeochemical cycling of carbon ...
  • Dissolved organic phosphorus concentrations in the northeast subarctic Pacific Ocean 

    Ridal, J. J., and R. M. Moore. 1992. "Dissolved organic phosphorus concentrations in the northeast subarctic Pacific Ocean." Limnology and Oceanography 37(5): 1067-1075. DOI:10.4319/lo.1992.37.5.1067
    Shipboard determinations of dissolved organic P (DOP) concentrations were made for NE subarctic Pacific Ocean samples with three different oxidation-hydrolysis methods: UV irradiation, acid persulfate digestion, and a ...
  • Distribution of N2O in the Baltic Sea during transition from anoxic to oxic conditions 

    Walter, S., U. Breitenbach, H. W. Bange, G. Nausch, et al. 2006. "Distribution of N2O in the Baltic Sea during transition from anoxic to oxic conditions." Biogeosciences 3(4): 557-570.
    In January 2003, a major inflow of cold and oxygen-rich North Sea Water terminated an ongoing stagnation period in parts of the central Baltic Sea. In order to investigate the role of North Sea Water inflow in the production ...
  • Distributions and Photosynthesis of Phototrophs in Sea-Surface Films 

    CULLEN, JJ, HL MACINTYRE, and DJ CARLSON. 1989. "Distributions and Photosynthesis of Phototrophs in Sea-Surface Films." Marine Ecology Progress Series 55(2-3): 271-278. doi:10.3354/meps055271
    No abstract available.
  • Distributions of Pigments and Primary Production in a Gulf-Stream Meander 

    LOHRENZ, SE, JJ CULLEN, DA PHINNEY, DB OLSON, et al. 1993. "Distributions of Pigments and Primary Production in a Gulf-Stream Meander." Journal of Geophysical Research-Oceans 98(C8): 14545-14560. DOI:10.1029/93JC00678
    An investigation was made of physical effects of Gulf Stream meandering on the vertical and horizontal distributions of photosynthetic pigments and primary production. Cruises were conducted in the vicinity of a meander ...
  • Early diagenesis in a marine sapropel, Mangrove Lake, Bermuda 

    Boudreau, Bernard P., Donald E. Canfield, and Alfonso Mucci. 1992. "Early diagenesis in a marine sapropel, Mangrove Lake, Bermuda." Limnology and Oceanography 37(8): 1738-1753.
    No abstract available.
  • Effect of the nonlinearity of the carbonate system on partial pressure of carbon dioxide in the oceans 

    Trela, P., S. Sathyendranath, R. M. Moore, and DE Kelley. 1995. "Effect of the nonlinearity of the carbonate system on partial pressure of carbon dioxide in the oceans." Journal of Geophysical Research.C.Oceans 100(C4): 6829-6844. DOI:10.1029/94JC02573
    Partial pressure of CO sub(2) is a nonlinear function of several seawater properties. Due to the nonlinearity in this relationship, the partial pressure of a uniform ocean would be different from that of a nonuniform ocean ...
  • Effect of Uv-Radiation on Phytoplankton 

    SMITH, RC, and JJ CULLEN. 1995. "Effect of Uv-Radiation on Phytoplankton." Reviews of Geophysics 33: 1211-1223. doi:10.1029/95RG00801
    No abstract available.
  • Effects of temperature and circulation on the population dynamics of Calanus finmarchicus in the Gulf of St. Lawrence and Scotian Shelf: Study with a coupled, three-dimensional hydrodynamic, stage-based life history model 

    Zakardjian, BA, JY Sheng, JA Runge, I. McLaren, et al. 2003. "Effects of temperature and circulation on the population dynamics of Calanus finmarchicus in the Gulf of St. Lawrence and Scotian Shelf: Study with a coupled, three-dimensional hydrodynamic, stage-based life history model." Journal of Geophysical Research-Oceans 108(C11): 8016-8016. DOI:10.1029/2002JC001410
    We developed a physical-biological model for the Gulf of St. Lawrence (GSL) and Scotian Shelf (SS) by coupling a stage-based life-history model of the planktonic copepod Calanus finmarchicus to a three-dimensional ocean ...
  • Enhanced ocean carbon storage from anaerobic alkalinity generation in coastal sediments 

    Thomas, H., L-S Schiettecatte, K. Suykens, YJ M Kone, et al. 2008. "Enhanced ocean carbon storage from anaerobic alkalinity generation in coastal sediments." Biogeosciences Discussions 5(4): 3575-3591.
    The coastal ocean constitutes the crucial link between land, the open ocean and the atmosphere. Furthermore, its shallow water column permits close interactions between the sedimentary and atmospheric compartments, which ...
  • Estimating mixed layer nitrate in the North Atlantic Ocean 

    Steinhoff, T., T. Friedrich, S. E. Hartman, A. Oschlies, et al. 2010. "Estimating mixed layer nitrate in the North Atlantic Ocean." Biogeosciences 7(3): 795-807.
    Here we present an equation for the estimation of nitrate in surface waters of the North Atlantic Ocean (40 degrees N to 52 degrees N, 10 degrees W to 60 degrees W). The equation was derived by multiple linear regression ...
  • Estimating the monthly pCO(2) distribution in the North Atlantic using a self-organizing neural network 

    Telszewski, M., A. Chazottes, U. Schuster, A. J. Watson, et al. 2009. "Estimating the monthly pCO(2) distribution in the North Atlantic using a self-organizing neural network." Biogeosciences 6(8): 1405-1421.
    Here we present monthly, basin-wide maps of the partial pressure of carbon dioxide (pCO(2)) for the North Atlantic on a 1 degrees latitude by 1 degrees longitude grid for years 2004 through 2006 inclusive. The maps have ...
  • Estimation of Low-Frequency Wind Stress Fluctuations Over the Open Ocean 

    THOMPSON, KR, RF MARSDEN, and DG WRIGHT. 1983. "Estimation of Low-Frequency Wind Stress Fluctuations Over the Open Ocean." Journal of Physical Oceanography 13(6): 1003-1011. © Copyright 1983 American Meteorological Society (AMS)
    No abstract available.
  • Evidence for asymmetric nonvolcanic rifting and slow incipient oceanic accretion from seismic reflection data on the Newfoundland margin 

    Shillington, Donna J., W. Steven Holbrook, Harm J. A. Van Avendonk, Brian E. Tucholke, et al. 2006. "Evidence for asymmetric nonvolcanic rifting and slow incipient oceanic accretion from seismic reflection data on the Newfoundland margin." Journal of Geophysical Research-Solid Earth 111(B9): 09402-B09402. DOI:10.1029/2005JB003981
    [ 1] Prestack depth migrations of seismic reflection data collected around the Ocean Drilling Program (ODP) Leg 210 transect on the Newfoundland nonvolcanic margin delineate three domains: ( 1) extended continental crust, ...