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Showing 1 to 20 of 3911 for “"Bottom"”.

  1. Ocean bottom seismic scattering

    Seismic studies of the oceanic crust, both experimental and theoretical, often assume a flat seafloor and laterally homogeneous crust. This is done regardless of the appearance in seismic data of obvious effects due to scattering from lateral heterogeneities both on and in the seafloor. Detailed …

    woods-hole Repository record for Ocean bottom seismic scattering (opens in a new tab)

  2. Ocean bottom seismic scattering

    Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, and Woods Hole Oceanographic Institution, 1990.

    mit Repository record for Ocean bottom seismic scattering (opens in a new tab)

  3. Baroclinic vortices over a sloping bottom

    Nonlinear quasigeostrophic flows in two layers over a topographic slope are considered. The evolution depends on the size of two parameters which indicate the degree of nonlinearity at depth. The first measures the importance of relative vorticity advection and the second of stretching vorticity. …

    woods-hole Repository record for Baroclinic vortices over a sloping bottom (opens in a new tab)

  4. Appreciating Beauty in the Bottom 80

    … were not in the top 20% of their classes, "The Bottom 80," and examined them in the context of education objectives and future prospects. Interviewees were a representative sample of eleven parents, three educators, and two experts. Information from additional experts was obtained as part of a …

    penn Repository record for Appreciating Beauty in the Bottom 80 (opens in a new tab)

  5. Bottom-up Methodologies in Emerging Models

    … hierarchical models, toward a de-centralized, bottom-up style demonstrated in recent movements. This paper examines the shift of doctrine and praxis within the American evangelical church and a simultaneous development of new methodologies in social justice organizations in these response …

    denver Repository record for Bottom-up Methodologies in Emerging Models (opens in a new tab)

  6. Free surface flow over bottom topography

    This thesis explores flow in a channel over a bottom topography. In particular, the problem of finding the shape of the unknown free-surface if the bottom topography is prescribed forms the main problem of this thesis. In chapter 2 the forced Korteweg De- Vries equation is derived from first …

    adelaide Repository record for Free surface flow over bottom topography (opens in a new tab)

  7. Long waves over an uneven bottom.

    Massachusetts Institute of Technology. Dept. of Civil Engineering. Thesis. 1970. Sc.D.

    mit Repository record for Long waves over an uneven bottom. (opens in a new tab)

  8. Bottom-Up Standardization For Data Preparation

    … simple and as standard as possible. We propose a bottom-up script standardization framework that takes a user’s data preparation script and transforms it into a simpler, more standardized, more boring version of itself. Our framework takes the user’s input script not as an unchangeable definition …

    mit Repository record for Bottom-Up Standardization For Data Preparation (opens in a new tab)

  9. Wave-current interaction over uneven bottom

    Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Civil Engineering, 1983.

    mit Repository record for Wave-current interaction over uneven bottom (opens in a new tab)

  10. Baroclinic vortices over a sloping bottom

    Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1996.

    mit Repository record for Baroclinic vortices over a sloping bottom (opens in a new tab)

  11. An on-the-bottom sea gravimeter.

    Massachusetts Institute of Technology. Dept. of Geology and Geophysics. Thesis. 1966. Ph.D.

    mit Repository record for An on-the-bottom sea gravimeter. (opens in a new tab)

  12. Modelling bottom stress in depth-averaged flows

    … relationship between depth-averaged velocity and bottom stress for wind-driven flow in unstratified coastal waters is examined here. The adequacy of traditional linear and quadratic drag laws is addressed by comparison with a 2 1/2-D model. A 2 1/2-D model is one in which a simplified 1-D …

    woods-hole Repository record for Modelling bottom stress in depth-averaged flows (opens in a new tab)

  13. Rewetting Temperature During Top and Bottom Reflood

    Made available in DSpace on 2017-07-06T18:56:22Z (GMT). No. of bitstreams: 2 Siegel_Alan_D_MS.pdf: 51485799 bytes, checksum: f0352a352d8b1c48211ca671f4c53089 (MD5) license.txt: 4813 bytes, checksum: 715c4321821a960fa1a1e91d2ac7ebce (MD5) Previous issue date: 1979

    uiuc Repository record for Rewetting Temperature During Top and Bottom Reflood (opens in a new tab)

  14. Petrography of Northeastern Lake Michigan Bottom Sediments

    Made available in DSpace on 2014-12-04T19:13:56Z (GMT). No. of bitstreams: 1 6003964.pdf: 3342567 bytes, checksum: 814354eb2109410074d58455730b699c (MD5) Previous issue date: 1960

    uiuc Repository record for Petrography of Northeastern Lake Michigan Bottom Sediments (opens in a new tab)

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