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  • Waves  (12)
  • Adaptation
  • Climate
  • Soc. Explorat. Geophys.  (5)
  • Air Force Geophysics Laboratory  (4)
  • Annual Reviews  (3)
  • Massachusetts Institute of Technology and Woods Hole Oceanographic Institution  (3)
  • 2020-2023  (2)
  • 2005-2009  (4)
  • 1990-1994  (3)
  • 1985-1989  (5)
  • 1980-1984  (1)
  • 1955-1959
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Years
Year
  • 1
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    Soc. Explorat. Geophys.
    In:  60th Annual Meeting of SEG, Cambridge, MA, USA, Soc. Explorat. Geophys., vol. 10, no. 18, pp. 1400-1403
    Publication Date: 1990
    Keywords: Inversion ; Waves ; AnisotropyS ; cracks and fractures (.NE. fracturing)
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  • 2
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    Soc. Explorat. Geophys.
    In:  56th Annual Meeting of SEG, Harwell, Berkshire, Soc. Explorat. Geophys., vol. 10, no. AFGL-TR-88-0315, pp. 563-565, (ISBN 3-933346-037)
    Publication Date: 1986
    Keywords: Vertical seismic profiling ; Waves ; Wave propagation
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  • 3
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    Soc. Explorat. Geophys.
    In:  Expanded abstracts of the technical program with authors' biographies of the 54th SEG International Meeting, Atlanta, Soc. Explorat. Geophys., vol. C 560, 183 pp., no. 51, 52 and 53, pp. 742-744, (ISBN 3-933346-037)
    Publication Date: 1984
    Keywords: Reflection seismics ; Seismics (controlled source seismology) ; Waves ; Reflectivity ; Conference abstr.
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  • 4
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    Soc. Explorat. Geophys.
    In:  60th Annual Meeting of SEG, Hannover, Soc. Explorat. Geophys., vol. C 560, 183 pp., no. 83-179, pp. 1410-1412, (ISBN 3-933346-037)
    Publication Date: 1990
    Keywords: cracks and fractures (.NE. fracturing) ; Anisotropy ; Waves
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  • 5
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    Air Force Geophysics Laboratory
    In:  Technical Report, San Francisco, Air Force Geophysics Laboratory, vol. C 560, 183 pp., no. AFGL-TR-88-0025, pp. 1680-1682, (ISBN 3-933346-037)
    Publication Date: 1988
    Keywords: Nuclear explosion ; Waves ; SEModelling ; Finite difference method ; Lg-waves ; SV waves ; Inhomogeneity ; Two-dimensional
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  • 6
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    Soc. Explorat. Geophys.
    In:  60th Annual Meeting of SEG, Washington, D.C., Soc. Explorat. Geophys., vol. C 560, 183 pp., no. 57, pp. 1388-1391, (ISBN 3-933346-037)
    Publication Date: 1990
    Keywords: Wave propagation ; Waves
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  • 7
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    Air Force Geophysics Laboratory
    In:  Technical Report, Mexico, Air Force Geophysics Laboratory, vol. C 560, 183 pp., no. AFGL-TR-87-0106, pp. 1015-1021, (ISBN 3-933346-037)
    Publication Date: 1987
    Keywords: Nuclear explosion ; Finite difference method ; Seismology ; Magnitude ; Waves ; Source ; Body waves ; Surface waves
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  • 8
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    Air Force Geophysics Laboratory
    In:  Technical Report, Mexico, Air Force Geophysics Laboratory, vol. C 560, 183 pp., no. AFGL-TR-88-0314, pp. 1015-1021, (ISBN 3-933346-037)
    Publication Date: 1988
    Keywords: Nuclear explosion ; Anisotropy ; Waves ; Seismology ; Teleseismic events ; Hypocentral depth ; Seismicity
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  • 9
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    Air Force Geophysics Laboratory
    In:  Technical Report, Kiel, Air Force Geophysics Laboratory, vol. C 560, 183 pp., no. AFGL-TR-88-0149, pp. 267-278, (ISBN 3-933346-037)
    Publication Date: 1988
    Keywords: Nuclear explosion ; Waves ; Synthetic seismograms
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  • 10
    Publication Date: 2022-05-25
    Description: Author Posting. © Annual Reviews, 2003. This article is posted here by permission of Annual Reviews for personal use, not for redistribution. The definitive version was published in Annual Review of Environment and Resources 28 (2003): 521-558, doi:10.1146/annurev.energy.28.011503.163443.
    Description: Agriculture and industrial development have led to inadvertent changes in the natural carbon cycle. As a consequence, concentrations of carbon dioxide and other greenhouse gases have increased in the atmosphere and may lead to changes in climate. The current challenge facing society is to develop options for future management of the carbon cycle. A variety of approaches has been suggested: direct reduction of emissions, deliberate manipulation of the natural carbon cycle to enhance sequestration, and capture and isolation of carbon from fossil fuel use. Policy development to date has laid out some of the general principles to which carbon management should adhere. These are summarized as: how much carbon is stored, by what means, and for how long. To successfully manage carbon for climate purposes requires increased understanding of carbon cycle dynamics and improvement in the scientific capabilities available for measurement as well as for policy needs. The specific needs for scientific information to underpin carbon cycle management decisions are not yet broadly known. A stronger dialogue between decision makers and scientists must be developed to foster improved application of scientific knowledge to decisions. This review focuses on the current knowledge of the carbon cycle, carbon measurement capabilities (with an emphasis on the continental scale) and the relevance of carbon cycle science to carbon sequestration goals.
    Description: The National Center for Atmospheric Research is supported by the National Science Foundation.
    Keywords: Carbon sequestration ; Measurement techniques ; Climate ; Kyoto protocol
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 11
    Publication Date: 2022-05-25
    Description: First published online as a Review in Advance on October 24, 2005. (Some corrections may occur before final publication online and in print)
    Description: Author Posting. © Annual Reviews, 2005. This article is posted here by permission of Annual Reviews for personal use, not for redistribution. The definitive version was published in Annual Review of Physiology 68 (2006): 22.1-22.29, doi:10.1146/annurev.physiol.68.040104.105418.
    Description: Superfast muscles of vertebrates power sound production. The fastest, the swimbladder muscle of toadfish, generates mechanical power at frequencies in excess of 200 Hz. To operate at these frequencies, the speed of relaxation has had to increase approximately 50-fold. This increase is accomplished by modifications of three kinetic traits: (a) a fast calcium transient due to extremely high concentration of sarcoplasmic reticulum (SR)-Ca2+ pumps and parvalbumin, (b) fast off-rate of Ca2+ from troponin C due to an alteration in troponin, and (c) fast cross-bridge detachment rate constant (g, 50 times faster than that in rabbit fast-twitch muscle) due to an alteration in myosin. Although these three modifications permit swimbladder muscle to generate mechanical work at high frequencies (where locomotor muscles cannot), it comes with a cost: The high g causes a large reduction in attached force-generating cross-bridges, making the swimbladder incapable of powering low-frequency locomotory movements. Hence the locomotory and sound-producing muscles have mutually exclusive designs.
    Description: This work was made possible by support from NIH grants AR38404 and AR46125 as well as the University of Pennsylvania Research Foundation.
    Keywords: Parvalbumin ; Ca2+ release ; Ca2+ uptake ; Cross-bridges ; Adaptation ; Sound production ; Whitman Center
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 12
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    Massachusetts Institute of Technology and Woods Hole Oceanographic Institution
    Publication Date: 2022-05-25
    Description: Submitted to the Joint Program in Physical Oceanography in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution September 2006
    Description: Ocean surface infragravity waves (periods from 20 to 200 s) observed along the southern California coast are shown to be sensitive to the bottom topography of the shelf region, where propagation is linear, and of the nearshore region, where nonlinearity is important. Infragravity waves exchange energy with swell and wind waves (periods from 5 to 20 s) via conservative nonlinear interactions that approach resonance with decreasing water depth. Consistent with previous results, it is shown here that as waves shoal into water less than a few meters deep, energy is transfered from swell to infragravity waves. In addition, it is shown here that the apparent dissipation of infragravity energy observed in the surfzone is the result of nonlinear energy transfers from infragravity waves back to swell and wind waves. The energy transfers are sensitive to the shallow water bottom topography. On nonplanar beach profiles the transfers, and thus the amount of infragravity energy available for reflection from the shoreline, change with the tide, resulting in the tidal modulation of infragravity energy observed in bottom-pressure records on the continental shelf. The observed wave propagation over the shelf topography is dominated by refraction, and the observed partial reflection from, and transmission across, a steep-walled submarine canyon is consistent with long-wave theory. A generalized regional model incorporating these results predicts the observed infragravity wave amplitudes over variable bottom topography.
    Description: Support from the Office of Naval Research (Coastal Geosciences Program, N00014-02-10145), the National Science Foundation (Physical Oceanography, OCE-0115850),
    Keywords: Waves ; Ocean bottom
    Repository Name: Woods Hole Open Access Server
    Type: Thesis
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  • 13
    Publication Date: 2022-10-27
    Description: This paper is not subject to U.S. copyright. The definitive version was published in Sherwood, C. R., van Dongeren, A., Doyle, J., Hegermiller, C. A., Hsu, T.-J., Kalra, T. S., Olabarrieta, M., Penko, A. M., Rafati, Y., Roelvink, D., van der Lugt, M., Veeramony, J., & Warner, J. C. Modeling the morphodynamics of coastal responses to extreme events: what shape are we in? Annual Review of Marine Science, 14, (2022): 457–492, https://doi.org/10.1146/annurev-marine-032221-090215.
    Description: This review focuses on recent advances in process-based numerical models of the impact of extreme storms on sandy coasts. Driven by larger-scale models of meteorology and hydrodynamics, these models simulate morphodynamics across the Sallenger storm-impact scale, including swash,collision, overwash, and inundation. Models are becoming both wider (as more processes are added) and deeper (as detailed physics replaces earlier parameterizations). Algorithms for wave-induced flows and sediment transport under shoaling waves are among the recent developments. Community and open-source models have become the norm. Observations of initial conditions (topography, land cover, and sediment characteristics) have become more detailed, and improvements in tropical cyclone and wave models provide forcing (winds, waves, surge, and upland flow) that is better resolved and more accurate, yielding commensurate improvements in model skill. We foresee that future storm-impact models will increasingly resolve individual waves, apply data assimilation, and be used in ensemble modeling modes to predict uncertainties.
    Description: All authors except D.R. were partially supported by the IFMSIP project, funded by US Office of Naval Research grant PE 0601153N under contracts N00014-17-1-2459 (Deltares), N00014-18-1-2785 (University of Delaware), N0001419WX00733 (US Naval Research Laboratory, Monterey), N0001418WX01447 (US Naval Research Laboratory, Stennis Space Center), and N0001418IP00016 (US Geological Survey). C.R.S., C.A.H., T.S.K., and J.C.W. were supported by the US Geological Survey Coastal/Marine Hazards and Resources Program. A.v.D. and M.v.d.L. were supported by the Deltares Strategic Research project Quantifying Flood Hazards and Impacts. M.O. acknowledges support from National Science Foundation project OCE-1554892.
    Keywords: Coastal morphodynamics ; Extreme storms ; Coastal modeling ; Sandy coasts ; Waves ; Sediment transport
    Repository Name: Woods Hole Open Access Server
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  • 14
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    Massachusetts Institute of Technology and Woods Hole Oceanographic Institution
    Publication Date: 2022-10-20
    Description: Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Oceanography at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution February 2021.
    Description: Anthropogenic emissions of greenhouse gases are driving rapid changes in ocean conditions. Shallow-water coral reefs are experiencing the brunt of these changes, including intensifying marine heatwaves (MHWs) and rapid ocean acidification (OA). Consequently, coral reefs are in broad-scale decline, threatening the livelihoods of hundreds of millions of people. Ensuring survival of coral reefs in the 21st century will thus require a new management approach that incorporates robust understanding of reef-scale climate change, the mechanisms by which these changes impact corals, and their potential for adaptation. In this thesis, I extract information from within coral skeletons to 1) Quantify the climate changes occurring on coral reefs and the effects on coral growth, 2) Identify differences in the sensitivity of coral reefs to these changes, and 3) Evaluate the adaptation potential of the keystone reef-building coral, Porites. First, I develop a mechanistic Porites growth model and reveal the physicochemical link between OA and skeletal formation. I show that the thickening (densification) of coral skeletal framework is most vulnerable to OA and that, under 21st century climate model projections, OA will reduce Porites skeletal density globally, with greatest impact in the Coral Triangle. Second, I develop an improved metric of thermal stress, and use a skeletal bleaching proxy to quantify coral responses to intensifying heatwaves in the central equatorial Pacific (CEP) since 1982. My work reveals a long history of bleaching in the CEP, and reef-specific differences in thermal tolerance linked to past heatwave exposure implying that, over time, reef communities have adapted to tolerate their unique thermal regimes. Third, I refine the Sr-U paleo-thermometer to enable monthly-resolved sea surface temperatures (SST) generation using laser ablation ICPMS. I show that laser Sr-U accurately captures CEP SST, including the frequency and amplitude of MHWs. Finally, I apply laser Sr-U to reconstruct the past 100 years of SST at Jarvis Island in the CEP, and evaluate my proxy record of bleaching severity in this context. I determine that Porites coral populations on Jarvis Island have not yet adapted to the pace of anthropogenic climate change.
    Description: This research was supported by US National Science Foundation Awards OCE-1220529, ANT-1246387, OCE-1737311, CE-1601365, OCE-1805618, OCE-1537338, OCE-2016133, and from the Woods Hole Oceanographic Institution through the Ocean Life Institute, the Ocean Ventures Fund, the Grassle Fellowship Fund, and the MIT-WHOI Academic Programs Office. Additional funding was provided by the Taiwan MOST Grant 104-2628-M-001-007-MY3, the Robertson Foundation, the Leverhulme Trust in UK, the Atlantic Donor Advised Fund, The Prince Albert 2 of Monaco Foundation, the Akiko Shiraki Dynner Fund, the New England Aquarium, the Martin Family Society Fellowship for Sustainability, the Gates Millenium Scholarship, the Arthur Vining Davis Foundation, the NOAA Coral Reef Conservation Program, and from the Woods Hole Oceanographic Institution through Investment in Science Fund, the Early Career Award, and the Access to the Sea Award.
    Keywords: Coral reef ; Climate ; Proxy
    Repository Name: Woods Hole Open Access Server
    Type: Thesis
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  • 15
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    Massachusetts Institute of Technology and Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution September, 1970
    Description: A series of laboratory experiments were conducted in a glass wave tank to investigate the propagation of internal gravity waves up a sloping bottom in a fluid with constant Brunt-Vaisala frequency. Measurements of the wave motion in the fluid interior were primarily taken with electrical conductivity probes; measurements in the boundary layer were made with dye streaks and neutrally buoyant particles. The results indicate that, outside of the breaking zone, the amplitude and horizontal wave number of the high-frequency waves increase lineariy with decreasing depth; this is shown to agree with existing linear, inviscid solutions. A zone of breaking or runup is induced by these high-frequency waves well upslope. Shadowgraph observations show that, if the wave characteristics are coincident, or nearly so, with the bottom slope, the upslope propagation of the low-frequency waves causes a line of regularly spaced vortices to form along the slope. Subsequent mixing in the vortex cells creates thin horizontal laminae that are more homogeneous than the adjacent layers. These laminae slowly penetrate the fluid interior, creating a step-like vertical density structure. Available linear theoretical solutions for the velocity in the viscous boundary layer, determined to be valid for certain experimental conditions, are used to develop a criterion for incipient motion of bottom sediment induced by shoaling internal waves. The maximum sediment sizes that can be placed into motion, according to this criterion, are larger than certain mean sediment sizes on the continental margin off New England. This suggests that internal waves might induce initial sediment movement. Speculation about the geological effects of breaking and vortex instabilities is also given. These processes, not definitely measured in the field as yet, might also be conducive to sediment movement.
    Description: This work was supported by the Office of Naval Research.
    Keywords: Sediment transport ; Waves
    Repository Name: Woods Hole Open Access Server
    Type: Thesis
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