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Scientific literature and information products produced by Woods Hole Coastal and Marine Science Center staff.

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Using the Model Coupling Toolkit to couple earth system models Using the Model Coupling Toolkit to couple earth system models

Continued advances in computational resources are providing the opportunity to operate more sophisticated numerical models. Additionally, there is an increasing demand for multidisciplinary studies that include interactions between different physical processes. Therefore there is a strong desire to develop coupled modeling systems that utilize existing models and allow efficient data...
Authors
J.C. Warner, N. Perlin, E.D. Skyllingstad

Chapter 31 Sensitivity and spin-up times of cohesive sediment transport models used to simulate bathymetric change Chapter 31 Sensitivity and spin-up times of cohesive sediment transport models used to simulate bathymetric change

Bathymetric change in tidal environments is modulated by watershed sediment yield, hydrodynamic processes, benthic composition, and anthropogenic activities. These multiple forcings combine to complicate simple prediction of bathymetric change; therefore, numerical models are necessary to simulate sediment transport. Errors arise from these simulations, due to inaccurate initial...
Authors
D. H. Schoellhamer, N. K. Ganju, P. R. Mineart, M. A. Lionberger

Comparison of two U.S. power-plant carbon dioxide emissions data sets Comparison of two U.S. power-plant carbon dioxide emissions data sets

Estimates of fossil-fuel CO2 emissions are needed to address a variety of climate-change mitigation concerns over a broad range of spatial and temporal scales. We compared two data sets that report power-plant CO 2 emissions in the conterminous U.S. for 2004, the most recent year reported in both data sets. The data sets were obtained from the Department of Energy's Energy Information
Authors
K.V. Ackerman, E.T. Sundquist

Workshop summary: Physical properties of gas hydrate-bearing sediment Workshop summary: Physical properties of gas hydrate-bearing sediment

A wide range of particle and pore scale phenomena, often coupled, determines the macro-scale response of gas-hydrate bearing sediment to changes in mechanical, thermal, or chemical conditions. Predicting this macro-scale response is critical for applications such as optimizing the production of methane from gas-hydrate deposits, or determining the role of gas hydrates in global carbon...
Authors
William F. Waite, J.C. Santamarina

Investigating gas hydrate as a factor in accretionary margin frontal ridge slope failures and cold seep biogeochemistry Investigating gas hydrate as a factor in accretionary margin frontal ridge slope failures and cold seep biogeochemistry

During August 2008, a research expedition (2008-007-PGC) was carried out offshore Vancouver Island on the northern Cascadia Margin (Figure 1) to study the role of gas hydrate in slope stability and cold seep biogeochemistry. The cruise was organized by the Geological Survey of Canada (GSC) as part of the Earth Science Sector, Natural Gas Hydrate Program, Natural Resources Canada (NRCan)...
Authors
R. Enkin, L. Esteban, R. Haacke, T.S. Hamilton, M. Hogg, L. Lapham, G. Middleton, P. Neelands, John W. Pohlman, M Riedel, K. Rose, A. Schlesinger, G. Standen, A. Stephenson, S. Taylor, W. Waite, X. Wang

Climate change and global carbon cycle: Perspectives and opportunities Climate change and global carbon cycle: Perspectives and opportunities

The relevance of methane hydrates research to broader societal themes is often framed in terms of methane’s role in the global carbon cycle and its potential contribution to future climate change. To date, investigations of these fundamental issues have remained largely disconnected from applied studies focused on locating natural gas hydrate deposits, developing production technologies...
Authors
Carolyn D. Ruppel, John W. Pohlman

Application of RHIZON samplers to obtain high-resolution pore-fluid records during geochemical investigations of gas hydrate systems Application of RHIZON samplers to obtain high-resolution pore-fluid records during geochemical investigations of gas hydrate systems

Obtaining accurate, high-resolution profiles of pore fluid constituents is critical for characterizing the subsurface geochemistry of hydrate-bearing sediments. Tightly-constrained downcore profiles provide clues about fluid sources, fluid flow, and the milieu of chemical and diagenetic reactions, all of which are used to interpret where and why gas and gas hydrate occur in the natural...
Authors
John W. Pohlman, M Riedel, William F. Waite, K. Rose, L. Lapham

Collaboration tools and techniques for large model datasets Collaboration tools and techniques for large model datasets

In MREA and many other marine applications, it is common to have multiple models running with different grids, run by different institutions. Techniques and tools are described for low-bandwidth delivery of data from large multidimensional datasets, such as those from meteorological and oceanographic models, directly into generic analysis and visualization tools. Output is stored using...
Authors
R. P. Signell, S. Carniel, J. Chiggiato, I. Janekovic, J. Pullen, C. R. Sherwood

Shoaling of nonlinear internal waves in Massachusetts Bay Shoaling of nonlinear internal waves in Massachusetts Bay

The shoaling of the nonlinear internal tide in Massachusetts Bay is studied with a fully nonlinear and nonhydrostatic model. The results are compared with current and temperature observations obtained during the August 1998 Massachusetts Bay Internal Wave Experiment and observations from a shorter experiment which took place in September 2001. The model shows how the approaching...
Authors
A. Scotti, R.C. Beardsley, B. Butman, J. Pineda

Quaternary geology and sedimentary processes in the vicinity of Six Mile Reef, eastern Long Island Sound Quaternary geology and sedimentary processes in the vicinity of Six Mile Reef, eastern Long Island Sound

Six Mile Reef, a sandy, 22-m-high shoal trending east-west and located about 7.8 km off the Connecticut coast, has a core of postglacial marine deltaic deposits mantled by tidally reworked modern sediments. Sedimentary environments off the eastern end of the shoal are characterized by processes associated with long-term erosion or nondeposition, a mobile-sediment-limited seafloor armored...
Authors
L. J. Poppe, S.J. Williams, M. S. Moser, N.A. Forfinski, H.F. Stewart, E. F. Doran

Nitrogen biogeochemistry of submarine groundwater discharge Nitrogen biogeochemistry of submarine groundwater discharge

To investigate the role of the seepage zone in transport, chemical speciation, and attenuation of nitrogen loads carried by submarine groundwater discharge, we collected nearshore groundwater samples (n = 328) and examined the distribution and isotopic signature (δ15N) of nitrate and ammonium. In addition, we estimated nutrient fluxes from terrestrial and marine groundwater sources. We...
Authors
K.D. Kroeger, M.A. Charette

Sediment dispersal in the northwestern Adriatic Sea Sediment dispersal in the northwestern Adriatic Sea

Sediment dispersal in the Adriatic Sea was evaluated using coupled three-dimensional circulation and sediment transport models, representing conditions from autumn 2002 through spring 2003. The calculations accounted for fluvial sources, resuspension by waves and currents, and suspended transport. Sediment fluxes peaked during southwestward Bora wind conditions that produced energetic...
Authors
C. K. Harris, C. R. Sherwood, R. P. Signell, A.J. Bever, J.C. Warner
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