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Coupling alongshore variations in wave energy to beach morphologic change using the SWAN wave model at Ocean Beach, San Francisco, CA Coupling alongshore variations in wave energy to beach morphologic change using the SWAN wave model at Ocean Beach, San Francisco, CA

Coastal managers have faced increasing pressure to manage their resources wisely over the last century as a result of heightened development and changing environmental forcing. It is crucial to understand seasonal changes in beach volume and shape in order to identify areas vulnerable to accelerated erosion. Shepard (1950) was among the first to quantify seasonal beach cycles. Sonu and...
Authors
Jodi L. Eshleman, Patrick L. Barnard, Li H. Erikson, Daniel M. Hanes

Model scenarios of shoreline change at Kaanapali Beach, Maui, Hawaii: Seasonal and extreme events Model scenarios of shoreline change at Kaanapali Beach, Maui, Hawaii: Seasonal and extreme events

Kaanapali beach is a well-defined littoral cell of carbonate sand extending 2 km south from Black Rock (a basalt headland) to Hanakao'o Point. The beach experiences dynamic seasonal shoreline change forced by longshore transport from two dominant swell regimes. In summer, south swells (Hs = 1–2 m Tp = 14–25 s) drive sand to the north, while in winter, north swells (Hs = 5–8 m Tp = 14–20...
Authors
Sean Vitousek, Charles H. Fletcher, Mark A. Merrifield, Geno Pawlak, Curt D. Storlazzi

Pliocene environments Pliocene environments

The Pliocene spans the interval of Earth history from ca. 5.3 to 1.8 million years ago (Ma). Although details are still debated there is much evidence from continental and oceanic locations indicating that conditions from 5.3 to about 3.0 Ma were often warmer than in modern times in mid- and high latitudes and that climate variability was subdued compared to the Pleistocene. Millennial...
Authors
R.Z. Poore

Swash zone characteristics at Ocean Beach, San Francisco, CA Swash zone characteristics at Ocean Beach, San Francisco, CA

Runup data collected during the summer of 2005 at Ocean Beach, San Francisco, CA are analyzed and considered to be typical summer swash characteristics at this site. Analysis shows that the beach was dissipative with Iribarren numbers between 0.05 and 0.4 and that infragravity energy dominated. Foreshore slopes were mild between 0.01 and 0.05 with swash periods on the order of a minute...
Authors
L. H. Erikson, D.M. Hanes, P.L. Barnard, A. E. Gibbs

Glacial landforms on German Bank, Scotian Shelf: evidence for Late Wisconsinan ice-sheet dynamics and implications for the formation of De Geer moraines Glacial landforms on German Bank, Scotian Shelf: evidence for Late Wisconsinan ice-sheet dynamics and implications for the formation of De Geer moraines

The extent and behaviour of the southeast margin of the Laurentide Ice Sheet in Atlantic Canada is of significance in the study of Late Wisconsinan ice sheet-ocean interactions. Multibeam sonar imagery of subglacial, ice-marginal and glaciomarine landforms on German Bank, Scotian Shelf, provides evidence of the pattern of glacial-dynamic events in the eastern Gulf of Maine. Northwest...
Authors
Brian J. Todd, Page C. Valentine, Oddvar Longva, John Shaw

Spatially continuous interpolation of water stage and water depths using the Everglades depth estimation network (EDEN) Spatially continuous interpolation of water stage and water depths using the Everglades depth estimation network (EDEN)

The Everglades Depth Estimation Network (EDEN) is an integrated network of real-time water-level monitoring, ground-elevation modeling, and water-surface modeling that provides scientists and managers with current (2000-present), online water-stage and water-depth information for the entire freshwater portion of the Greater Everglades. Continuous daily spatial interpolations of the EDEN...
Authors
Leonard Pearlstine, Aaron Higer, Monica Palaseanu, Ikuko Fujisaki, Frank Mazzotti

Comparison of flood lavas on Earth and Mars Comparison of flood lavas on Earth and Mars

Flood lavas, by definition, cover vast areas in great sheets of lava, without the construction of major edifices (e.g., Geikie, 1880; Washington, 1922; Tyrrell, 1937; Self et al., 1997). The flat terrain that flood lavas produce has led to the term “plateau volcanism” to be used as a synonym for flood volcanism. In addition, the classic erosion pattern of flood lavas leaves a series of...
Authors
Laszlo P. Keszthelyi, Alfred S. McEwen

Tampa Bay as a model estuary for examining the impact of human activities on biogeochemical processes: an introduction Tampa Bay as a model estuary for examining the impact of human activities on biogeochemical processes: an introduction

Tampa Bay is a shallow, Y-shaped coastal embayment that is located along the center of the Florida Platform – an expansive accumulation of Cretaceous–Tertiary shallow-water carbonates and evaporites that were periodically exposed during glacio–eustatic sea level fluctuations. As a consequence, extensive karstification likely had a controlling impact on the geologic evolution of Tampa Bay...
Authors
Peter W. Swarzenski, Mark Baskaran, Carl S. Henderson, Kim Yates

Continental margin sedimentation: From sediment transport to sequence stratigraphy Continental margin sedimentation: From sediment transport to sequence stratigraphy

This volume on continental margin sedimentation brings together an expert editorial and contributor team to create a state-of-the-art resource. Taking a global perspective, the book spans a range of timescales and content, ranging from how oceans transport particles, to how thick rock sequences are formed on continental margins. - Summarizes and integrates our understanding of...

The need for sustained and integrated high-resolution mapping of dynamic coastal environments The need for sustained and integrated high-resolution mapping of dynamic coastal environments

The coastal zone of the United States is a dynamic environment evolving in response to both natural processes and human activities. In order to protect coastal populations and resources, a detailed understanding of the physical setting and of the processes responsible for change is required. A sustained program of mapping coastal areas provides a means to establish baseline conditions...
Authors
Hilary F. Stockdon, Jeff W. Lillycrop, Peter A. Howd, Jennifer M. Wozencraft

Southern California Bight 2003 Regional Monitoring Program: V. water quality Southern California Bight 2003 Regional Monitoring Program: V. water quality

More than $30 million is expended annually on environmental monitoring in the Southern California Bight (SCB), yet only 5% of the Bight is monitored on an ongoing basis. Therefore, environmental managers in the SCB decided to expand their monitoring program and, starting in 1994, decided to conduct periodic regional assessments of ecosystem condition and assess the overall health of the...
Authors
Nikolay P. Nezlin, Paul M. DiGiacomo, Stephen B. Weisberg, Dario W. Diehl, Jonathan A. Warrick, Michael J. Mengel, Burton H. Jones, Kristen M. Reifel, Scott C. Johnson, J. Carter Ohlmann, Libe Washburn, Eric J. Terrill
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