Publications
Scientific literature and information products produced by Woods Hole Coastal and Marine Science Center staff.
Filter Total Items: 1739
Short-term nitrogen additions can shift a coastal wetland from a sink to a source of N2O Short-term nitrogen additions can shift a coastal wetland from a sink to a source of N2O
Coastal salt marshes sequester carbon at high rates relative to other ecosystems and emit relatively little methane particularly compared to freshwater wetlands. However, fluxes of all major greenhouse gases (N2O, CH4, and CO2) need to be quantified for accurate assessment of the climatic roles of these ecosystems. Anthropogenic nitrogen inputs (via run-off, atmospheric deposition, and...
Authors
Serena Moseman-Valtierra, Rosalinda Gonzalez, Kevin D. Kroeger, Jianwu Tang, Wei Chun Chao, John Crusius, John F. Bratton, Adrian G. Mann, James Shelton
A conduit dilation model of methane venting from lake sediments A conduit dilation model of methane venting from lake sediments
Methane is a potent greenhouse gas, but its effects on Earth's climate remain poorly constrained, in part due to uncertainties in global methane fluxes to the atmosphere. An important source of atmospheric methane is the methane generated in organic-rich sediments underlying surface water bodies, including lakes, wetlands, and the ocean. The fraction of the methane that reaches the...
Authors
B.P. Scandella, C. Varadharajan, Harold F. Hemond, C. Ruppel, R. Juanes
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
Methane hydrates and contemporary climate change Methane hydrates and contemporary climate change
As the evidence for warming climate became better established in the latter part of the 20th century (IPCC 2001), some scientists raised the alarm that large quantities of methane (CH4) might be liberated by widespread destabilization of climate-sensitive gas hydrate deposits trapped in marine and permafrost-associated sediments (Bohannon 2008, Krey et al. 2009, Mascarelli 2009). Even if...
Authors
Carolyn D. Ruppel
High-resolution geophysical data from the sea floor surrounding the Western Elizabeth Islands, Massachusetts High-resolution geophysical data from the sea floor surrounding the Western Elizabeth Islands, Massachusetts
Geophysical and geospatial data were collected in the nearshore area surrounding the western Elizabeth Islands, Massachusetts on the U.S. Geological Survey research vessel Rafael during September 2010 in a collaborative effort between the U.S. Geological Survey and the Massachusetts, Office of Coastal Zone Management. This report describes the results of the short-term goals of this...
Authors
Elizabeth A. Pendleton, David C. Twichell, David S. Foster, Charles R. Worley, Barry J. Irwin, William W. Danforth
Duration and severity of Medieval drought in the Lake Tahoe Basin Duration and severity of Medieval drought in the Lake Tahoe Basin
Droughts in the western U.S. in the past 200 years are small compared to several megadroughts that occurred during Medieval times. We reconstruct duration and magnitude of extreme droughts in the northern Sierra Nevada from hydroclimatic conditions in Fallen Leaf Lake, California. Stands of submerged trees rooted in situ below the lake surface were imaged with sidescan sonar and...
Authors
J.A. Kleppe, D.S. Brothers, G.M. Kent, F. Biondi, S. Jensen, N. W. Driscoll
Groupers on the edge: Shelf edge spawning habitat in and around marine reserves of the northeastern Gulf of Mexico Groupers on the edge: Shelf edge spawning habitat in and around marine reserves of the northeastern Gulf of Mexico
The northeastern Gulf of Mexico contains some of the most diverse and productive marine habitat in the United States. Much of this habitat, located on the shelf edge in depths of 50 to 120 m, supports spawning for many economically important species, including groupers. Here, we couple acoustic surveys with georeferenced videography to describe the primary spatial and geologic features...
Authors
Felicia C. Coleman, Kathryn M. Scanlon, Christopher C. Koenig