Carolyn Ruppel, PhD
I lead the USGS Gas Hydrates Project, which is jointly funded by the Coastal and Marine Hazards and Resources Program and the Energy Resources Program. Project scientists in Woods Hole and Denver study the resource and climate aspects of natural hydrates. My work also focuses on methane seeps, hydroacoustics, marine environmental compliance, and subsea permafrost on the Arctic coast.
Research
Highlighted Journal Articles, Data Releases, and Geonarratives
- Gas Hydrate in Nature
- Hydrate formation on marine seep bubbles and the implications for water column…
- Elevated levels of radiocarbon in methane dissolved in seawater reveal likely l…
- Preliminary global database of known and inferred gas hydrate locations
- Post-expedition report for USGS T-3 ice island heat flow measurements in the Hi…
- Thermal Data and Navigation for T-3 (Fletcher's) Ice Island Arctic Ocean Heat F…
My primary research focus is on the interaction between methane hydrates (and methane seeps) on one hand and the ocean-atmosphere system on the other. I focus particularly on the US Atlantic and US Pacific margins, as well as Arctic Ocean margins (US Beaufort Sea and Svalbard). I also work on energy issues related to gas hydrates (including delineating their distribution in marine sediments; 2018 MATRIX seismic program on US Atlantic margin), the coexistence of permafrost (including subsea) and hydrates (Beaufort Sea), and reservoir properties of hydrate-bearing sediments. As a side specialty, I assist with programmatic environmental compliance for USGS marine acoustics surveys. During my career, I have also worked on marine heat flow data acquisition and analysis, other aspects of the hydrogeology of gas hydrate systems, and coastal zone hydrogeophysics (particularly tidal pumping, inductive EM data, and saline intrusion in surficial aquifers). My earliest work focused on numerical modeling of large scale tectonic processes and associated particle tracking, continental rifting, and marine analogs for continental tectonic processes.
Professional Experience
July 2023 - present: Supervisory Research Geophysicist, U.S. Geological Survey
Feb 2023 - present: Part-Time Acting Senior Science Advisor to the USGS Chief Scientist
July 2022 - Feb 2023: Acting Senior Science Advisor to the USGS Chief Scientist (detail)
2010-present: Chief, USGS Gas Hydrates Project
2006-2023: Research Geophysicist, U.S. Geological Survey
2006-2019: Visiting Scientist, MIT, Dept. of Earth, Atmospheric & Planetary Sciences
2003-2006: Program manager (faculty rotater), National Science Foundation, Ocean Sciences (MG&G and Ocean Drilling Program)
2000-2002: Coordinator, Georgia Tech Focused Research Program on Methane Hydrates
2000-2006: Associate Professor (tenured) of Geophysics, Georgia Tech
1994-2000: Assistant Professor of Geophysics, Georgia Tech
1992-1993: Postdoctoral Scholar and Postdoctoral Research, Woods Hole Oceanographic Institution
Education and Certifications
Massachusetts Institute of Technology, Ph.D., 1992, Geophysics and Geology (with Marcia McNutt)
Massachusetts Institute of Technology, M.S., 1986, Earth sciences (with Leigh Royden and Kip Hodges)
Affiliations and Memberships*
Panel member, National Academy of Sciences, Community on Ocean Acoustics Education and Expertise (study completion in 2024)
Member, Science Advisory Board, University of Tromso, Centre of Excellence for Ice, Cryosphere, Carbon and Climate, 2023-
Member, Arctic Icebreaker Coordinating Committee (UNOLS), 2015-2020
Chief Scientist, 8 research cruises (3 Arctic), 2010-2019
Member, Advisory Board, University of Tromso, Centre of Excellence for Arctic Gas Hydrate, Environment and Climate (CAGE) 2014-present
Strategic Plan Committee, Coastal & Marine Geology Program, USGS, 2014-2019
Arctic subgroup (appointed CMGP representative), Subcommittee on Ocean Science and Technology (SOST), OSTP, 2015-16
Mentor, Graduate Women at MIT (GWAMIT), 2013-2016
USGS Technical lead, NSF-USGS Programmatic Environmental Impact Statement for Marine Seismics, 2008-2012
Lead organizer, Catching climate change in progress, circum-Arctic Ocean drilling workshop, December 2011 (sponsored by US Science Support Program for IODP)
Lead proponent, IODP Pre-Proposal 797, Late Pleistocene to contemporary climate change on the Alaskan Beaufort Margin (ABM)
Organizer and convener, USGS-DOE Climate-Hydrates workshop, Boston, MA, March 2011
Originator and Chair, Gordon Research Conference on Natural Gas Hydrates, inaugural conference held June 2010.
Interagency Technical Coordinating Committee, DOE Methane Hydrates R&D Program, 2010-present
The Future of Natural Gas, MIT Energy Initiative, affiliated author (methane hydrates), 2008-2011
National Research Council, Scientific Ocean Drilling (SOD) review, presentation on Gas Hydrates and SOD, 2010
IODP Operations Task Force, 2008-2009
IODP Science Planning Committee (SPC), 2006-2009
Organizer, DOE-USGS Symposium/Meeting on Gas Hydrates and Climate Change (held at MIT), February 2008
Honors and Awards
National Science Foundation, Director's Award for Program Management, 2005 (Chixulub seismic program)
JOI/USSAC Distinguished Lecturer, Ocean Drilling Program, 1999-2000
Science and Products
Evidence for extensive methane venting on the southeastern U.S. Atlantic margin
Mass fractionation of noble gases in synthetic methane hydrate: Implications for naturally occurring gas hydrate dissociation
Minimum distribution of subsea ice-bearing permafrost on the US Beaufort Sea continental shelf
Observations of mass fractionation of noble gases in synthetic methane hydrate
Strong atmospheric chemistry feedback to climate warming from Arctic methane emissions
Methane hydrates and the future of natural gas
Methane hydrates and contemporary climate change
The impact of hydrate saturation on the mechanical, electrical, and thermal properties of hydrate-bearing sand, silts, and clay
Parametric study of the physical properties of hydrate-bearing sand, silt, and clay sediments: 1. Electromagnetic properties
Parametric study of the physical properties of hydrate‐bearing sand, silt, and clay sediments: 2. Small‐strain mechanical properties
Permafrost gas hydrates and climate change: Lake-based seep studies on the Alaskan north slope
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
USGS scientists contribute to new gas hydrates monograph
The recently-published monograph entitled World Atlas of Submarine Gas Hydrates on Continental Margins compiles findings about gas hydrates offshore all of Earth’s continents and also onshore in selected permafrost regions.
Science and Products
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Filter Total Items: 64
Evidence for extensive methane venting on the southeastern U.S. Atlantic margin
We present the first evidence for widespread seabed methane venting along the southeastern United States Atlantic margin beyond the well-known Blake Ridge diapir seep. Recent ship- and autonomous underwater vehicle (AUV)–collected data resolve multiple water-column anomalies (>1000 m height) and extensive new chemosynthetic seep communities at the Blake Ridge and Cape Fear diapirs. These results iAuthorsL.L. Brothers, C.L. Van Dover, C.R. German, C.L. Kaiser, D.R. Yoerger, C.D. Ruppel, E. Lobecker, A.D. Skarke, J.K.S. WagnerMass fractionation of noble gases in synthetic methane hydrate: Implications for naturally occurring gas hydrate dissociation
As a consequence of contemporary or longer term (since 15 ka) climate warming, gas hydrates in some settings may presently be dissociating and releasing methane and other gases to the ocean-atmosphere system. A key challenge in assessing the impact of dissociating gas hydrates on global atmospheric methane is the lack of a technique able to distinguish between methane recently released from gas hyAuthorsAndrew G. Hunt, Laura Stern, John W. Pohlman, Carolyn Ruppel, Richard J. Moscati, Gary P. LandisMinimum distribution of subsea ice-bearing permafrost on the US Beaufort Sea continental shelf
Starting in Late Pleistocene time (~19 ka), sea level rise inundated coastal zones worldwide. On some parts of the present-day circum-Arctic continental shelf, this led to flooding and thawing of formerly subaerial permafrost and probable dissociation of associated gas hydrates. Relict permafrost has never been systematically mapped along the 700-km-long U.S. Beaufort Sea continental shelf and isAuthorsLaura L. Brothers, Patrick E. Hart, Carolyn D. RuppelObservations of mass fractionation of noble gases in synthetic methane hydrate
As a consequence of contemporary or longer term (since 15 ka) climate warming, gas hydrates in some settings are presently dissociating and releasing methane and other gases to the oceanatmosphere system. A key challenge in assessing the susceptibility of gas hydrates to warming climate is the lack of a technique able to distinguish between methane recently released from gas hydrates and methane eAuthorsAndrew G. Hunt, John W. Pohlman, Laura A. Stern, Carolyn D. Ruppel, Richard J. Moscati, Gary P. Landis, John C. PinkstonStrong 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 in the atmAuthorsIvar S.A. Isaksen, Michael Gauss, Gunnar Myhre, Katey M. Walter Anthony, Carolyn RuppelMethane 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 productiAuthorsCarolyn RuppelMethane 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 only a frAuthorsCarolyn D. RuppelThe impact of hydrate saturation on the mechanical, electrical, and thermal properties of hydrate-bearing sand, silts, and clay
Proper understanding of the physical properties of hydrate-bearing sediments is required for interpretation of borehole logs and exploration geophysical data, the analysis of borehole and submarine slope stability, and the formulation of reservoir simulation and production models. Yet current knowledge of geophysical and geotechnical properties of hydrate-bearing sediments is still largely derivedAuthorsJ. Carlos Santamarina, Carolyn D. RuppelParametric study of the physical properties of hydrate-bearing sand, silt, and clay sediments: 1. Electromagnetic properties
The marked decrease in bulk electrical conductivity of sediments in the presence of gas hydrates has been used to interpret borehole electrical resistivity logs and, to a lesser extent, the results of controlled source electromagnetic surveys to constrain the spatial distribution and predicted concentration of gas hydrate in natural settings. Until now, an exhaustive laboratory data set that couldAuthorsJ.Y. Lee, J.C. Santamarina, C. RuppelParametric study of the physical properties of hydrate‐bearing sand, silt, and clay sediments: 2. Small‐strain mechanical properties
The small‐strain mechanical properties (e.g., seismic velocities) of hydrate‐bearing sediments measured under laboratory conditions provide reference values for calibration of logging and seismic exploration results acquired in hydrate‐bearing formations. Instrumented cells were designed for measuring the compressional (P) and shear (S) velocities of sand, silts, and clay with and without hydrateAuthorsJ.Y. Lee, F.M. Francisca, J.C. Santamarina, C. RuppelPermafrost gas hydrates and climate change: Lake-based seep studies on the Alaskan north slope
The potential interactions between climate change and methane hydrate destabilization are among the most societally-relevant aspects of gas hydrates research. Massive dissociation of deep marine methane hydrates following rapid Earth warming is the most plausible explanation for carbon isotopic data that imply widespread release of microbial methane during the Late Paleocene Thermal Maximum (~55 mAuthorsM.J. Wooller, Carolyn D. Ruppel, John W. Pohlman, M.B. Leigh, M. Heintz, K. Walter AnthonyNon-USGS Publications**
Tréhu, A.M., C. Ruppel, M. Holland, G.R. Dickens, M.E. Torres, T.S. Collett, D. Goldberg, M. Riedel, and P. Schultheiss. 2006. Gas hydrates in marine sediments: Lessons from scientific ocean drilling. Oceanography 19(4):124–142, https://doi.org/10.5670/oceanog.2006.11.Nimblett, J. and C. Ruppel, 2003, Permeability evolution during formation of gas hydrates in marine sediments, Journal of Geophysical Research, 108, 2420, doi: 10.1029/2001JB001650.Ruppel, C., Thermal state of the gas hydrate reservoir, 2000, in: Max, M. editor, Natural Gas Hydrate in Oceanic and Permafrost Environments, Kluwer Academic Publishers, 29-42, 2000. https://doi.org/10.1007/978-94-011-4387-5_4Nimblett, J. and C. Ruppel, 2003, Permeability evolution during formation of gas hydrates in marine sediments, Journal of Geophysical Research, 108, 2420, doi: 10.1029/2001JB001650.Ruppel, C., 1997, Anomalously cold temperatures observed at the base of the gas hydrate stability zone, U.S. Atlantic passive margin, Geology, 25, 699-702. Doi: 10.1130/0091-7613(1997)025<0699:ACTOAT>2.3.CO;2Wood, W.T., and Ruppel, C., 2000. Seismic and thermal investigations of the Blake Ridge gas hydrate area: a synthesis. In Paull, C.K., Matsumoto, R., Wallace, P.J., and Dillon, W.P. (Eds.), Proc. ODP, Sci. Results, 164: College Station, TX (Ocean Drilling Program), 253–264. doi:10.2973/odp.proc.sr.164.203.2000Xu, W. and C. Ruppel, 1999, Predicting the occurrence, distribution, and evolution of methane gas hydrate in porous marine sediments from analytical models, Journal of Geophysical Research, 104, ,5081-5096. 10.1029/1998JB900092Paull, C.K., Matsumoto, R., Wallace, P.J., et al., 1996. Proc. ODP, Init. Repts., 164: College Station, TX (Ocean Drilling Program). doi:10.2973/odp.proc.ir.164.1996Ruppel, C., R.P. Von Herzen, and A. Bonneville, 1995, Heat flux through an old (~175 Ma) passive margin: offshore southeastern USA, Journal of Geophysical Research, 100,20,037-20,058. Doi: 10.1029/95JB01860Santamarina, J.C. and C. Ruppel, 2010, The impact of hydrate saturation on the mechanical, electrical, and thermal properties of hydrate-bearing sand, silts, and clay (Chapter 26), In: Riedel, Willoughby, Chopra (eds), Geophysical Characterization of Gas Hydrates, Society of Exploration Geophysicists Geophysical Developments, vol. 14, 373-384Trehu, A.M., C. Ruppel, J. Dickens, D. Goldberg, M. Holland, M. Riedel, P. Schultheiss, and M. Torres, 2006, Gas hydrates in marine sediments: lessons from ocean drilling, Oceanography, 19, 124-143, 2006.Yun, T.S., G. Narsilio, J.C. Santamarina, and C. Ruppel, 2006, Instrumented pressure testing chamber for characterizing sediment cores recovered at in situ hydrostatic pressure, Marine Geology, 229, 285-293. doi: 10.1016/j.margeo.2006.03.012.Yun, T.S., F. Francisca, J.C. Santamarina, and C. Ruppel, 2005, Compressional and shear wave velocities of uncemented sediment containing gas hydrate, Geophysical Research Letters, 32, L10609. doi: 10.1029/2005GL022607.Nimblett, J. and C. Ruppel, 2003, Permeability evolution during formation of gas hydrates in marine sediments, Journal of Geophysical Research, 108, 2420, doi: 10.1029/2001JB001650.Waite, W.F, deMartin, B.J, Kirby, S.H., Pinkston, J., Ruppel, C.D., 2002, Thermal conductivity measurements in porous mixtures of methane hydrate and quartz sand, Geophysical Research Letters. doi: 10.1029/2002GL015988Ruppel C. (2000) Thermal State of the Gas Hydrate Reservoir. In: Max M.D. (eds) Natural Gas Hydrate. Coastal Systems and Continental Margins, vol 5. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-4387-5_4Xu, W. and C. Ruppel, 1999, Predicting the occurrence, distribution, and evolution of methane gas hydrate in porous marine sediments from analytical models, Journal of Geophysical Research, 104, ,5081-5096**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
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USGS scientists contribute to new gas hydrates monograph
The recently-published monograph entitled World Atlas of Submarine Gas Hydrates on Continental Margins compiles findings about gas hydrates offshore all of Earth’s continents and also onshore in selected permafrost regions.
Filter Total Items: 13
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government