Skip to main content
U.S. flag

An official website of the United States government

Publications

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

Filter Total Items: 1749

Modeling sulfate reduction in methane hydrate-bearing continental margin sediments: Does a sulfate-methane transition require anaerobic oxidation of methane? Modeling sulfate reduction in methane hydrate-bearing continental margin sediments: Does a sulfate-methane transition require anaerobic oxidation of methane?

The sulfate‐methane transition (SMT), a biogeochemical zone where sulfate and methane are metabolized, is commonly observed at shallow depths (1–30 mbsf) in methane‐bearing marine sediments. Two processes consume sulfate at and above the SMT, anaerobic oxidation of methane (AOM) and organoclastic sulfate reduction (OSR). Differentiating the relative contribution of each process is...
Authors
A. Malinverno, John W. Pohlman

Barriers on the brink? The complex intertwined roles of geologic framework, sediment availability and sea-level rise in island evolution Barriers on the brink? The complex intertwined roles of geologic framework, sediment availability and sea-level rise in island evolution

Sensitivity experiments in the North Carolina Outer Banks (OBX) have previously revealed that substrate sand proportion, followed by substrate slope, sea-level rise rate and sediment-loss rate are the most important factors in determining how barrier islands respond to sea-level rise. High sediment-loss rates and low substrate sand proportions cause barriers to be smaller and more deeply...
Authors
Laura Moore, Jeffrey H. List, S. Jeffress Williams, Kiki Patsch

Documenting channel features associated with gas hydrates in the Krishna-Godavari Basin, offshore India Documenting channel features associated with gas hydrates in the Krishna-Godavari Basin, offshore India

During the India National Gas Hydrate Program (NGHP) Expedition 01 in 2006 significant sand and gas hydrate were recovered at Site NGHP-01-15 within the Krishna–Godavari Basin, East Coast off India. At the drill site NGHP-01-15, a 5–8 m thick interval was found that is characterized by higher sand content than anywhere else at the site and within the KG Basin. Gas hydrate concentrations...
Authors
M. Riedel, Timothy S. Collett, Ude Shankar

Implementation and modification of a three-dimensional radiation stress formulation for surf zone and rip-current applications Implementation and modification of a three-dimensional radiation stress formulation for surf zone and rip-current applications

Regional Ocean Modeling System (ROMS v 3.0), a three-dimensional numerical ocean model, was previously enhanced for shallow water applications by including wave-induced radiation stress forcing provided through coupling to wave propagation models (SWAN, REF/DIF). This enhancement made it suitable for surf zone applications as demonstrated using examples of obliquely incident waves on a...
Authors
N. Kumar, G. Voulgaris, John C. Warner

Strong atmospheric chemistry feedback to climate warming from Arctic methane emissions Strong atmospheric chemistry feedback to climate warming from Arctic methane emissions

The magnitude and feedbacks of future methane release from the Arctic region are unknown. Despite limited documentation of potential future releases associated with thawing permafrost and degassing methane hydrates, the large potential for future methane releases calls for improved understanding of the interaction of a changing climate with processes in the Arctic and chemical feedbacks...
Authors
Ivar Isaksen, Michael Gauss, Gunnar Myhre, Katey M. Walter Anthony, Carolyn Ruppel

Downhole well log and core montages from the Mount Elbert Gas Hydrate Stratigraphic Test Well, Alaska North Slope Downhole well log and core montages from the Mount Elbert Gas Hydrate Stratigraphic Test Well, Alaska North Slope

The BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well was an integral part of an ongoing project to determine the future energy resource potential of gas hydrates on the Alaska North Slope. As part of this effort, the Mount Elbert well included an advanced downhole geophysical logging program. Because gas hydrate is unstable at ground surface pressure and temperature...
Authors
Timothy S. Collett, R.E. Lewis, William J. Winters, Myung W. Lee, K.K. Rose, R.M. Boswell

Wave-current interaction in Willapa Bay Wave-current interaction in Willapa Bay

This paper describes the importance of wave-current interaction in an inlet-estuary system. The three-dimensional, fully coupled, Coupled Ocean-Atmosphere-Wave-Sediment Transport (COAWST) modeling system was applied in Willapa Bay (Washington State) from 22 to 29 October 1998 that included a large storm event. To represent the interaction between waves and currents, the vortex-force...
Authors
Maitane Olabarrieta, John C. Warner, Nirnimesh Kumar

A nearshore processes field experiment at Cape Hatteras, North Carolina, U.S.A. A nearshore processes field experiment at Cape Hatteras, North Carolina, U.S.A.

A month-long field experiment focused on the nearshore hydrodynamics of Diamond Shoals adjacent to Cape Hatteras Point, North Carolina, was conducted in February 2010. The objectives of this multi-institutional experiment were to test hypotheses related to Diamond Shoals as a sink in the regional sediment budget and to provide data for evaluating numerical models. The experiment included...
Authors
Jeffrey H. List, John C. Warner, E. Robert Thieler, Kevin Haas, George Voulgaris, Jesse E. McNinch, Katherine L. Brodie

Character of shell beds flanking Herod Point Shoal, southeastern Long Island Sound, New York Character of shell beds flanking Herod Point Shoal, southeastern Long Island Sound, New York

High biogenic productivity, strong tidal currents, shoal topography, and short transport distances combine to favor shell-bed formation along the lower flanks of a cape-associated shoal off Herod Point on Long Island, New York. This shell bed has a densely packed, clast-supported fabric composed largely of undegraded surf clam (Spisula solidissima) valves. It is widest along the central...
Authors
Lawrence J. Poppe, S. Jeffress Williams, Ivar G. Babb

2-D inner-shelf current observations from a single VHF WEllen RAdar (WERA) station 2-D inner-shelf current observations from a single VHF WEllen RAdar (WERA) station

The majority of High Frequency (HF) radars used worldwide operate at medium to high frequencies (8 to 30 MHz) providing spatial resolutions ranging from 3 to 1.5 km and ranges from 150 to 50 km. This paper presents results from the deployment of a single Very High Frequency (VHF, 48 MHz) WEllen RAdar (WERA) radar with spatial resolution of 150 m and range 10-15 km, used in the nearshore...
Authors
G. Voulgaris, N. Kumar, K.-W. Gurgel, John C. Warner, Jeffrey H. List

Glacial flour dust storms in the Gulf of Alaska: hydrologic and meteorological controls and their importance as a source of bioavailable iron Glacial flour dust storms in the Gulf of Alaska: hydrologic and meteorological controls and their importance as a source of bioavailable iron

Iron is an essential micronutrient that limits primary productivity in much of the ocean, including the Gulf of Alaska (GoA). However, the processes that transport iron to the ocean surface are poorly quantified. We combine satellite and meteorological data to provide the first description of widespread dust transport from coastal Alaska into the GoA. Dust is frequently transported from...
Authors
John Crusius, A.W. Schroth, S. Gasso, C.M. Moy, R.C. Levy, M. Gatica

Methane hydrates and the future of natural gas Methane hydrates and the future of natural gas

For decades, gas hydrates have been discussed as a potential resource, particularly for countries with limited access to conventional hydrocarbons or a strategic interest in establishing alternative, unconventional gas reserves. Methane has never been produced from gas hydrates at a commercial scale and, barring major changes in the economics of natural gas supply and demand, commercial
Authors
Carolyn Ruppel
Was this page helpful?