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Woods Hole Coastal and Marine Science Center

2022 Annual Report

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Mapping methane reduction potential of tidal wetland restoration in the United States

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Opportunities to improve alignment with the FAIR Principles for U.S. Geological Survey data

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

Featured Journal Article

Herring River, Wellfleet, MA

Calibrating optical turbidity measurements with suspended-sediment concentrations from the Herring River in Wellfleet, Massachusetts, from November 2018 to November 2019

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Featured USGS Series

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Woods Hole Coastal and Marine Science Center—2022 Annual Report.  The 2022 annual report highlights accomplishments, includes a list of publications, and summarizes the work of the center and each of the science groups.

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Sound Waves

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Coastal and Marine Research News from Across the USGS

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Filter Total Items: 1691

Shallow geology, sea-floor texture, and physiographic zones of Buzzards Bay, Massachusetts

Geologic, sediment texture, and physiographic zone maps characterize the sea floor of Buzzards Bay, Massachusetts. These maps were derived from interpretations of seismic-reflection profiles, high-resolution bathymetry, acoustic-backscatter intensity, bottom photographs, and surficial sediment samples. The interpretation of the seismic stratigraphy and mapping of glacial and Holocene marine units
Authors
David S. Foster, Wayne E. Baldwin, Walter A. Barnhardt, William C. Schwab, Seth D. Ackerman, Brian D. Andrews, Elizabeth A. Pendleton
By
Natural Hazards Mission Area, Coastal and Marine Hazards and Resources Program, Woods Hole Coastal and Marine Science Center

Substantial nitrous oxide emissions from intertidal sediments and groundwater in anthropogenically-impacted West Falmouth Harbor, Massachusetts

Large N2O emissions were observed from intertidal sediments in a coastal estuary, West Falmouth Harbor, MA, USA. Average N2O emission rates from 41 chambers during summer 2008 were 10.7 mol N2O m(-2) h(-1)±4.43 μmol N2O m(-2) h(-1) (standard error). Emissions were highest from sediments within a known wastewater plume, where a maximum N2O emission rate was 155 μmol N2O m(-2) h(-1). Intertidal N2O
Authors
Serena Moseman-Valtierra, Kevin D. Kroeger, John Crusius, Sandy Baldwin, Adrian G. Mann, Thomas W. Brooks, E. Pugh
By
Woods Hole Coastal and Marine Science Center

Bottom stress measurements on the inner shelf

Bottom stress shapes the mean circulation patterns, controls sediment transport, and influences benthic habitat in the coastal ocean. Accurate and precise measurements of bottom stress have proved elusive, in part because of the difficulty in separating the turbulent eddies that transport momentum from inviscid wave-induced motions. Direct covariance measurements from a pair of acoustic Doppler ve
Authors
Christopher R. Sherwood, Malcolm Scully, John Trowbridge
By
Woods Hole Coastal and Marine Science Center

National Oceanic and Atmospheric Administration hydrographic survey data used in a U.S. Geological Survey regional geologic framework study along the Delmarva Peninsula

The U.S. Geological Survey initiated a research effort in 2014 to define the geologic framework of the Delmarva Peninsula inner continental shelf, which included new data collection and assembly of relevant extant datasets. Between 2006 and 2011, Science Applications International Corporation, under contract to the National Oceanic and Atmospheric Administration National Ocean Service, carried out
Authors
Elizabeth A. Pendleton, Laura L. Brothers, E. Robert Thieler, William W. Danforth, Castle E. Parker
By
Woods Hole Coastal and Marine Science Center

Maps showing bathymetry and modern sediment thickness on the inner continental shelf offshore of Fire Island, New York, pre-Hurricane Sandy

The U.S. Geological Survey mapped approximately 336 square kilometers of the lower shoreface and inner continental shelf offshore of Fire Island, New York, in 2011 by using interferometric sonar and high-resolution chirp seismic-reflection systems. This report presents maps of bathymetry, acoustic backscatter, the coastal plain unconformity, the Holocene marine transgressive surface, and modern se
Authors
William C. Schwab, Jane F. Denny, Wayne E. Baldwin
By
Woods Hole Coastal and Marine Science Center, Hurricane Sandy

Inner-shelf circulation and sediment dynamics on a series of shoreface connected ridges offshore of Fire Island, NY

Locations along the inner-continental shelf offshore of Fire Island, NY, are characterized by a series of shoreface-connected ridges (SFCRs). These sand ridges have approximate dimensions of 10 km in length, 3 km spacing, and up to ∼8 m ridge to trough relief and are oriented obliquely at approximately 30° clockwise from the coastline. Stability analysis from previous studies explains how sand rid
Authors
John C. Warner, Jeffrey H. List, William C. Schwab, George Voulgaris, Brandy N. Armstrong, N Marshall
By
Woods Hole Coastal and Marine Science Center, Hurricane Sandy

Widespread gas hydrate instability on the upper U.S. Beaufort margin

The most climate-sensitive methane hydrate deposits occur on upper continental slopes at depths close to the minimum pressure and maximum temperature for gas hydrate stability. At these water depths, small perturbations in intermediate ocean water temperatures can lead to gas hydrate dissociation. The Arctic Ocean has experienced more dramatic warming than lower latitudes, but observational data h
Authors
Benjamin J. Phrampus, Matthew J. Hornbach, Carolyn D. Ruppel, Patrick E. Hart
By
Woods Hole Coastal and Marine Science Center

Comparison of the physical and geotechnical properties of gas-hydrate-bearing sediments from offshore India and other gas-hydrate-reservoir systems

The sediment characteristics of hydrate-bearing reservoirs profoundly affect the formation, distribution, and morphology of gas hydrate. The presence and type of gas, porewater chemistry, fluid migration, and subbottom temperature may govern the hydrate formation process, but it is the host sediment that commonly dictates final hydrate habit, and whether hydrate may be economically developed.In th
Authors
William J. Winters, R.W. Wilcox-Cline, P. Long, S.K. Dewri, P. Kumar, Laura A. Stern, Laura A. Kerr
By
Woods Hole Coastal and Marine Science Center

Core data from offshore Puerto Rico and the U.S. Virgin Islands

In 2008, as a collaborative effort between Woods Hole Oceanographic Institution and the U.S. Geological Survey, 20 giant gravity cores were collected from areas surrounding Puerto Rico and the U.S. Virgin Islands. The regions sampled have had many large earthquake and landslide events, some of which are believed to have triggered tsunamis. The objective of this coring cruise, carried out aboard th

Authors
Shannon K. Hoy, Jason D. Chaytor, Uri S. ten Brink
By
Woods Hole Coastal and Marine Science Center, 2020 Puerto Rico Earthquakes

Character, distribution, and ecological significance of storm wave-induced scour in Rhode Island Sound, USA

Multibeam bathymetry, collected during NOAA hydrographic surveys in 2008 and 2009, is coupled with USGS data from sampling and photographic stations to map the seabed morphology and composition of Rhode Island Sound along the US Atlantic coast, and to provide information on sediment transport and benthic habitats. Patchworks of scour depressions cover large areas on seaward-facing slopes and bathy
Authors
Katherine Y. McMullen, Lawrence J. Poppe, Castle E. Parker
By
Woods Hole Coastal and Marine Science Center

Permafrost-associated gas hydrate: is it really approximately 1% of the global system?

Permafrost-associated gas hydrates are often assumed to contain ∼1 % of the global gas-in-place in gas hydrates based on a study26 published over three decades ago. As knowledge of permafrost-associated gas hydrates has grown, it has become clear that many permafrost-associated gas hydrates are inextricably linked to an associated conventional petroleum system, and that their formation history (tr
Authors
Carolyn Ruppel
By
Woods Hole Coastal and Marine Science Center

The potential for sea-level-rise-induced barrier island loss: Insights from the Chandeleur Islands, Louisiana, USA

As sea level rises and hurricanes become more intense, barrier islands around the world become increasingly vulnerable to conversion from self-sustaining migrating landforms to submerging or subaqueous sand bodies. To explore the mechanism by which such state changes occur and to assess the factors leading to island disintegration, we develop a suite of numerical simulations for the Chandeleur Isl
Authors
Laura J. Moore, Kiki Patsch, Jeffrey H. List, S. Jeffress Williams
By
Woods Hole Coastal and Marine Science Center