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Browsing Faculty Research Publications (College of Earth, Ocean, and Atmospheric Sciences) by Title

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Browsing Faculty Research Publications (College of Earth, Ocean, and Atmospheric Sciences) by Title

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  • Schofield, Oscar; Arnone, Robert A.; Bissett, W. Paul; Dickey, Tommy D.; Davis, Curtiss O.; Finkel, Zoe; Oliver, Matthew; Moline, Mark A. (Oceanography Society, 2004-06)
    See article for abstract.
  • Sallenger, Asbury H. Jr.; Holman, Robert A. (American Geophysical Union, 1985-11-20)
    Time series of flow were measured across the inner surf zone during a storm. These data were used to quantify the dependence of wave height (transformed from measured flow) and velocity on local slope and depth. Similar ...
  • Ruggiero, Peter; Holman, Robert A.; Beach, R. A. (American Geophysical Union, 2004)
    Because of highly dissipative conditions and strong alongshore gradients in foreshore beach morphology, wave run-up data collected along the central Oregon coast during February 1996 stand in contrast to run-up data cu ...
  • Senechal, Nadia; Coco, Giovanni; Bryan, Karin R.; Holman, Rob A. (American Geophysical Union, 2011-07-30)
    Video measurements of wave runup were collected during extreme storm conditions characterized by energetic long swells (peak period of 16.4 s and offshore height up to 6.4 m) impinging on steep foreshore beach slopes (0. ...
  • Howd, Peter A.; Oltman-Shay, Joan; Holman, Robert A. (American Geophysical Union, 1991)
    The wave-induced velocity field in the nearshore is composed of contributions from incident wind waves (f > 0.05 Hz), surface infragravity waves (f < 0.05 Hz, lkl < (σ²/gβ) and shear waves (f < 0.05 Hz, lkl > σ²/gβ), ...
  • Kirincich, Anthony R.; Lentz, Steven J.; Barth, John A. (American Meteorological Society, 2009-11)
    Recent work by S. Lentz et al. documents offshore transport in the inner shelf due to a wave-driven return flow associated with the Hasselmann wave stress (the Stokes–Coriolis force). This analysis is extended using ob ...
  • Freilich, M. H.; Chelton, D. B. (American Meteorological Society, 1986-04)
    Vector winds measured by the Seasat-A Satellite Scatterometer (SASS) are analyzed to determine the spatial structure of oceanic surface winds over wavelengths from 200 to 2200 km. The analysis is performed in four latitu ...
  • Holland, K. T.; Holman, Robert A. (American Geophysical Union, 1999-06-15)
    Alongshore-separated time series of natural swash motions were obtained over a range of environmental conditions using a video technique. Although the frequency spectra and normalized wavenumber spectra for these motions ...
  • Durland, Theodore S.; Farrar, J. Thomas (American Meteorological Society, 2012-11)
    The theoretical resonant excitation of equatorial inertia–gravity waves and mixed Rossby–gravity waves is examined. Contrary to occasionally published expectations, solutions show that winds that are broadband in both zo ...
  • Farrar, J. Thomas; Durland, Theodore S. (American Meteorological Society, 2012-11)
    In the 1970s and 1980s, there was considerable interest in near-equatorial variability at periods of days to weeks associated with oceanic equatorial inertia–gravity waves and mixed Rossby–gravity waves. At that time, th ...
  • Haller, Merrick C.; Ozkan-Hollar, Tuba (American Institute of Physics, 2007-12-03)
    Models for surface gravity wave propagation in the presence of currents often assume the current field to be quasi-stationary, which implies that the absolute wave frequency is time invariant. However, in the presence ...
  • Bennett, Andrew F.; Miller, Robert N. (American Meteorological Society, 1991-04)
    An analysis of variational data assimilation schemes for linear dynamical forecast models shows that the penalty functional must include an explicit contribution from the initial conditions in order to ensure a unique, l ...
  • Zhao, Liuzhi; Chen, Changsheng; Vallino, Joe; Hopkinson, Charles; Beardsley, Robert C.; Lin, Huichan; Lerczak, Jim (American Geophysical Union, 2010-10-16)
    Wetland‐estuarine‐shelf interaction processes in the Plum Island Sound and Merrimack River system in the Massachusetts coast are examined using the high‐resolution unstructured grid, finite volume, primitive equations, ...
  • Haggerty, Roy; Harvey, Charles F.; von Schwerin, Claudius Freiherr; Meigs, Lucy C. (American Geophysical Union, 2004)
    Estimates of mass transfer timescales from 316 solute transport experiments reported in 35 publications are compared to the pore-water velocities and residence times, as well as the experimental durations. New tracer exp ...
  • Goes, Marlos; Urban, Nathan M.; Tonkonojenkov, Roman; Haran, Murali; Schmittner, Andreas; Keller, Klaus (American Geophysical Union, 2010-12-02)
    Current projections of the oceanic response to anthropogenic climate forcings are uncertain. Two key sources of these uncertainties are (1) structural errors in current Earth system models and (2) imperfect knowledge of ...
  • de Szoeke, Simon P.; Xie, Shang-Ping; Miyama, Toru; Richards, Kelvin J.; Small, R. Justin O. (American Meteorological Society, 2007-06)
    A coupled ocean–atmosphere regional model suggests a mechanism for formation of a sharp sea surface temperature (SST) front north of the equator in the eastern Pacific Ocean in boreal summer and fall. Meridional converge ...
  • Strom, Suzanne L.; Miller, Charles B.; Frost, Bruce W. (Inter Research, 2000-02-28)
    Phytoplankton biomass in high-nitrate, low-chlorophyll (HNLC) ocean regions exhibits a pronounced stability: variation occurs only within a narrow range of values. The magnitude of this variation has profound ecological ...
  • Fischer, H.; Severinghaus, J.; Brook, E.; Wolff, E.; Albert, M.; Alemany, O.; Arthern, R.; Bentley, C.; Blankenship, D.; Chappellaz, J.; Creyts, T.; Dahl-Jensen, D.; Dinn, M.; Frezzotti, M.; Fujita, S.; Gallee, H.; Hindmarsh, R.; Hudspeth, D.; Jugie, G.; Kawamura, K.; Lipenkov, V.; Miller, H.; Mulvaney, R.; Parrenin, F.; Pattyn, F.; Ritz, C.; Schwander, J.; Steinhage, D.; van Ommen, T.; Wilhelms, F. (Copernicus Publications, 2013)
    The recovery of a 1.5 million yr long ice core from Antarctica represents a keystone of our understanding of Quaternary climate, the progression of glaciation over this time period and the role of greenhouse gas cycle ...
  • O'Neill, Larry W. (American Meteorological Society, 2012-03-01)
    The surface wind and stress responses to sea surface temperature (SST) are examined using collocated moored buoy and satellite observations in the Gulf Stream and the eastern equatorial Pacific. Using 17 buoy pairs, diff ...
  • Kirincich, Anthony R.; Barth, John A.; Grantham, Brian A.; Menge, Bruce A.; Lubchenco, Jane (American Geophysical Union, 2005)
    Velocity measurements from 17 deployments of moored acoustic Doppler current profilers obtained during four summer upwelling seasons are used to describe the crossshelf divergence of Ekman transport in the inner shelf ...

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