Publications
Scientific literature and information products produced by Woods Hole Coastal and Marine Science Center staff.
Filter Total Items: 1739
Coupled atmosphere-ocean-wave simulations of a storm event over the Gulf of Lion and Balearic Sea Coupled atmosphere-ocean-wave simulations of a storm event over the Gulf of Lion and Balearic Sea
The coastal areas of the North-Western Mediterranean Sea are one of the most challenging places for ocean forecasting. This region is exposed to severe storms events that are of short duration. During these events, significant air-sea interactions, strong winds and large sea-state can have catastrophic consequences in the coastal areas. To investigate these air-sea interactions and the...
Authors
Lionel Renault, Jacopo Chiggiato, John C. Warner, Marta Gomez, Guillermo Vizoso, Joaquin Tintore
Profile measurements and data from the 2011 Optics, Acoustics, and Stress In Situ (OASIS) project at the Martha's Vineyard Coastal Observatory Profile measurements and data from the 2011 Optics, Acoustics, and Stress In Situ (OASIS) project at the Martha's Vineyard Coastal Observatory
This report documents data collected by the U.S. Geological Survey (USGS) for the Coastal Model Applications and Field Measurements project under the auspices of the U.S. Navy Office of Naval Research Optics, Acoustics, and Stress In Situ (OASIS) Project. The objective of the measurements was to relate optical and acoustic properties of suspended particles to changes in particle size
Authors
Christopher R. Sherwood, Patrick J. Dickhudt, Marinna A. Martini, Ellyn T. Montgomery, Emmanuel S. Boss
Tidal and groundwater fluxes to a shallow, microtidal estuary: Constraining inputs through field observations and hydrodynamic modeling Tidal and groundwater fluxes to a shallow, microtidal estuary: Constraining inputs through field observations and hydrodynamic modeling
Increased nutrient loading to estuaries has led to eutrophication, degraded water quality, and ecological transformations. Quantifying nutrient loads in systems with significant groundwater input can be difficult due to the challenge of measuring groundwater fluxes. We quantified tidal and freshwater fluxes over an 8-week period at the entrance of West Falmouth Harbor, Massachusetts, a...
Authors
Neil K. Ganju, Melanie Hayn, Shih-Nan Chen, Robert W. Howarth, Patrick J. Dickhudt, Alfredo L. Aretxabaleta, Roxanne Marino
Foraminiferal repopulation of the late Eocene Chesapeake Bay impact crater Foraminiferal repopulation of the late Eocene Chesapeake Bay impact crater
The Chickahominy Formation is the initial postimpact deposit in the 85km-diameter Chesapeake Bay impact crater, which is centered under the town of Cape Charles, Virginia, USA. The formation comprises dominantly microfossil-rich, silty, marine clay, which accumulated during the final ~1.6myr of late Eocene time. At cored sites, the Chickahominy Formation is 16.8-93.7m thick, and fills a...
Authors
C. Wylie Poag
Sea-floor geology in central Rhode Island Sound south of Sakonnet Point, Rhode Island Sea-floor geology in central Rhode Island Sound south of Sakonnet Point, Rhode Island
The U.S. Geological Survey (USGS) and the National Oceanic and Atmospheric Administration (NOAA) are working together to study the sea floor along the northeastern coast of the United States. NOAA collected multibeam-echosounder data during hydrographic survey H11995 in a 63-square-kilometer area in central Rhode Island Sound, south of Sakonnet Point, Rhode Island. The USGS collected...
Authors
K.Y. McMullen, L.J. Poppe, S.D. Ackerman, C.R. Worley, M.A. Nadeau, M. V. Van Hoy
Sea-floor character and sedimentary processes of Block Island Sound, offshore Rhode Island Sea-floor character and sedimentary processes of Block Island Sound, offshore Rhode Island
Gridded multibeam bathymetry covers approximately 634 square kilometers of sea floor in Block Island Sound. Although originally collected for charting purposes during National Oceanic and Atmospheric Administration hydrographic surveys H12009, H12010, H12011, H12015, H12033, H12137, and H12139, these combined acoustic data and the sea-floor sediment sampling and photography stations...
Authors
L.J. Poppe, W. W. Danforth, K.Y. McMullen, M.A. Blankenship, K.A. Glomb, D.B. Wright, S. M. Smith
Diversity of active aerobic methanotrophs along depth profiles of arctic and subarctic lake water column and sediments Diversity of active aerobic methanotrophs along depth profiles of arctic and subarctic lake water column and sediments
Methane (CH4) emitted from high-latitude lakes accounts for 2–6% of the global atmospheric CH4 budget. Methanotrophs in lake sediments and water columns mitigate the amount of CH4 that enters the atmosphere, yet their identity and activity in arctic and subarctic lakes are poorly understood. We used stable isotope probing (SIP), quantitative PCR (Q-PCR), pyrosequencing and enrichment...
Authors
Ruo He, Matthew J. Wooller, John W. Pohlman, John Quensen, James M. Tiedje, Mary Beth Leigh
Documentation of the U.S. Geological Survey sea floor stress and sediment mobility database Documentation of the U.S. Geological Survey sea floor stress and sediment mobility database
The U.S. Geological Survey Sea Floor Stress and Sediment Mobility Database contains estimates of bottom stress and sediment mobility for the U.S. continental shelf. This U.S. Geological Survey database provides information that is needed to characterize sea floor ecosystems and evaluate areas for human use. The estimates contained in the database are designed to spatially and seasonally...
Authors
P. Soupy Dalyander, Bradford Butman, Christopher R. Sherwood, Richard P. Signell
Identification of functionally active aerobic methanotrophs in sediments from an arctic lake using stable isotope probing Identification of functionally active aerobic methanotrophs in sediments from an arctic lake using stable isotope probing
Arctic lakes are a significant source of the greenhouse gas methane (CH4), but the role that methane oxidizing bacteria (methanotrophs) play in limiting the overall CH4 flux is poorly understood. Here, we used stable isotope probing (SIP) techniques to identify the metabolically active aerobic methanotrophs in upper sediments (0–1 cm) from an arctic lake in northern Alaska sampled during...
Authors
Ruo He, Matthew J. Wooller, John W. Pohlman, Catharine Catranis, John Quensen, James M. Tiedje, Mary Beth Leigh
Apalachicola Bay interpreted seismic horizons and updated IRIS chirp seismic-reflection data Apalachicola Bay interpreted seismic horizons and updated IRIS chirp seismic-reflection data
Apalachicola Bay and St. George Sound contain the largest oyster fishery in Florida, and the growth and distribution of the numerous oyster reefs here are the combined product of modern estuarine conditions and the late Holocene evolution of the bay. A suite of geophysical data and cores were collected during a cooperative study by the U.S. Geological Survey, the National Oceanic and...
Authors
V.A. Cross, D.C. Twichell, D.S. Foster, T.F. O’Brien
Plate interaction in the NE Caribbean subduction zone from continuous GPS observations Plate interaction in the NE Caribbean subduction zone from continuous GPS observations
Kinematic similarities between the Sumatra and Puerto Rico Trenches highlight the potential for a mega-earthquake along the Puerto Rico Trench and the generation of local and trans-Atlantic tsunamis. We used the horizontal components of continuous GPS (cGPS) measurements from 10 sites on NE Caribbean islands to evaluate strain accumulation along the North American (NA) - Caribbean (CA)...
Authors
Uri S. ten Brink, Alberto M. Lopez-Vegas
High-resolution geophysical data collected within Red Brook Harbor, Buzzards Bay, Massachusetts, in 2009 High-resolution geophysical data collected within Red Brook Harbor, Buzzards Bay, Massachusetts, in 2009
The U.S. Geological Survey conducted a high-resolution geophysical survey within Red Brook Harbor, Massachusetts, from September 28 through November 17, 2009. Red Brook Harbor is located on the eastern edge of Buzzards Bay, south of the Cape Cod Canal. The survey area was approximately 7 square kilometers, with depths ranging from 0 to approximately 10 meters. Data were collected aboard...
Authors
Aaron M. Turecek, William W. Danforth, Wayne E. Baldwin, Walter A. Barnhardt