Index Catalog // ScholarsArchive@OSU

Creator:: Kuebel Cervantes, B. T., Allen, J. S., and Samelson, R. M.
Abstract:: The effects of wind-forced upwelling and downwelling on the continental shelf off Duck, North Carolina, are studied through experiments with a two-dimensional numerical primitive equation model. Moored and shipboard measurements obtained during August–November 1994 as part of the Coastal Ocean Processes (CoOP) Inner Shelf Study (ISS) are used for model–data...
Resource Type:: Article
Full Text:: Lagrangian Aspects of Shelf Circulation off Duck, North Carolina B. T. KUEBEL CERVANTES, J. S. ALLEN, AND R

Creator:: Perlin, N., Samelson, R. M., and Chelton, D. B.
Abstract:: Measurements of surface wind stress by the SeaWinds scatterometer on NASA's Quick Scatterometer (QuikSCAT) satellite are analyzed and compared with several different atmospheric model products, from an operational model and two high-resolution nested regional models, during two summer periods, June through September 2000 and 2001, in the coastal region west...
Resource Type:: Article
Full Text:: the Oregon–Northern California Coastal Zone N. PERLIN, R. M. SAMELSON, AND D. B. CHELTON College of

Creator:: Bennett, A. F., Chua, B. S., Pflaum, B. L., Erwig, M., Fu, Z., Loft, R. D., and Muccino, J. C.
Abstract:: The Inverse Ocean Modeling (IOM) system constructs and runs weak-constraint, four-dimensional variational data assimilation (W4DVAR) for any dynamical model and any observing array. The dynamics and the observing algorithms may be nonlinear but must be functionally smooth. The user need only provide the model and the observing algorithms, together with...
Resource Type:: Article
Full Text:: . BENNETT, B. S. CHUA, AND B. L. PFLAUM College of Oceanic and Atmospheric Sciences, Oregon State

Creator:: Ruessink, B. G., Wijnberg, K. M., Holman, R. A., Kuriyama, Y., and van Enckevort, I. M. J.
Abstract:: Long-term (>years) bathymetric data sets collected in six multiple near-shore sandbar systems were analyzed with complex empirical orthogonal function analysis to quantify intersite differences and similarities in cyclic offshore progressive bar behavior. The observations came from a 37-year annually sampled data set of four regions along the Dutch coast (spanning...
Resource Type:: Article
Full Text:: behavior B. G. Ruessink,1 K. M. Wijnberg,2 R. A. Holman,3 Y. Kuriyama,4 and I. M. J. van Enckevort1

Creator:: Wingenter, Oliver W., Haase, Karl B., Strutton, Peter, Friederich, Gernot, Meinardi, Simone, Blake, Donald R., and Rowland, F. Sherwood
Abstract:: Oceanic iron (Fe) fertilization experiments have advanced the understanding of how Fe regulates biological productivity and air–sea carbon dioxide (CO₂) exchange. However, little is known about the production and consumption of halocarbons and other gases as a result of Fe addition. Besides metabolizing inorganic carbon, marine microorganisms produce and consume...
Resource Type:: Article
Full Text:: , J. J., Swanson, A. L., Meinardi, S., Sive, B. C., Blake, D. R. & Rowland, F. S. (2001) Anal. Chem

Creator:: Rosell-Melé, A., Bard, E., Emeis, K.-C., Grimalt, J. O., Muller, P., Schneider, R., Bouloubassi, I., Epstein, B., Fahl, K., Fluegge, A., Freeman, K., Goñi, M., Güntner, U., Hartz, D., Hellebust, S., Herbert, T., Ikehara, M., Ishiwatari, R., Kawamura, K., Kenig, F., de Leeuw, J., Lehman, S., Mejanelle, L., Ohkouchi, N., Pancost, R. D., Pelejero, C., Prahl, Fredrick, Quinn, J., Rontani, J.-F., Rostek, F., Rullkötter, J., Sachs, J., Blanz, T., Sawada, K., Schulz-Bull, D., Sikes, E., Sonzogni, C., Ternois, Y., Versteegh, G., Volkman, J. K., and Wakeham, S.
Abstract:: Measurements of the U₃₇ K’ index and the absolute abundance of alkenones in marine sediments are increasingly used in paleoceanographic research as proxies of past sea surface temperature and haptophyte (mainly coccolith-bearing species) primary productivity, respectively. An important aspect of these studies is to be able to compare reliably data...
Resource Type:: Article
Full Text:: e n o n e s in t e r l a b o r a t o r y c o m pa r iso n 2 0 0 0 G C 0 0 0 1 4 1 to be

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