Last edited by Mazukinos
Monday, April 13, 2020 | History

2 edition of Atmospheric flow over two-dimensional bluff surface obstructions found in the catalog.

Atmospheric flow over two-dimensional bluff surface obstructions

Juergen Bitte

Atmospheric flow over two-dimensional bluff surface obstructions

  • 174 Want to read
  • 0 Currently reading

Published by National Aeronautics and Space Administration, for sale by the National Technical Information Service in Washington, Springfield, Va .
Written in English

    Subjects:
  • Atmospheric turbulence.

  • Edition Notes

    StatementJuergen Bitte and Walter Frost ; prepared by the University of Tennessee Space Institute.
    SeriesNASA contractor report ; NASA CR-2750, NASA contractor report -- NASA CR-2750.
    ContributionsFrost, Walter, 1935-, United States. National Aeronautics and Space Administration., University of Tennessee (System). Space Institute.
    The Physical Object
    Paginationxviii, 207 p. :
    Number of Pages207
    ID Numbers
    Open LibraryOL15222075M

    Morphometric and geotechnical basin characteristics are examined to assess their influence on the frequency and magnitude of debris flows. Frequency is assessed primarily from the dendrochronologic record. Magnitude is determined from a combination of field surveys of deposits and empirical methods, and calculations of probable magnitudes reconstructed from Cited by:


Share this book
You might also like
Selection and acquisition of data base management systems

Selection and acquisition of data base management systems

Two Years in Revolutionary China, 1925-1927 (Harvard East Asian Monographs)

Two Years in Revolutionary China, 1925-1927 (Harvard East Asian Monographs)

Textbook of Gastroenterology, 4/E and Atlas of Gastroenterology, 3/E , Two-Volume Textbook Plus Atlas

Textbook of Gastroenterology, 4/E and Atlas of Gastroenterology, 3/E , Two-Volume Textbook Plus Atlas

Identity, the Sri Lanka architect

Identity, the Sri Lanka architect

Condensation products of some a-diketones

Condensation products of some a-diketones

LogoVisual thinking

LogoVisual thinking

Write away

Write away

How to manage a successful business in China

How to manage a successful business in China

handlist of the Byzantine lead seals and tokens (and of Western and Islamic seals) in the Barber Institute of Fine Arts, University of Birmingham

handlist of the Byzantine lead seals and tokens (and of Western and Islamic seals) in the Barber Institute of Fine Arts, University of Birmingham

Older people and their homes

Older people and their homes

All Ireland

All Ireland

Sampled-data control systems [by] John R. Ragazzini [and] Gene F. Franklin.

Sampled-data control systems [by] John R. Ragazzini [and] Gene F. Franklin.

Brief from the Department of the Solicitor General presented to the Commission of Enquiry into the Non-Medical Use of Drugs.

Brief from the Department of the Solicitor General presented to the Commission of Enquiry into the Non-Medical Use of Drugs.

Eur opean Parliament

Eur opean Parliament

Water, no longer taken for granted

Water, no longer taken for granted

Wives, mistresses, and matriarchs

Wives, mistresses, and matriarchs

OVERHEADS

OVERHEADS

Atmospheric flow over two-dimensional bluff surface obstructions by Juergen Bitte Download PDF EPUB FB2

Atmospheric flow over two-dimensional bluff surface obstructions. Washington: National Aeronautics and Space Administration, (OCoLC) Material Type: Government publication, National government publication: Document Type: Book: All Authors / Contributors: Juergen Bitte; Walter Frost; University of Tennessee (Knoxville campus.

REFERENCES (1) J. Bitte and W. Frost, "Atmospheric Flow over Two-Dimensional Bluff Surface Obstructions," NASA Contract Report, NASA CR, October U.K.

Kaul and W. Frost, "Turbulent Atmospheric Flow over a Backward-Facing Step," NASA Contract Report, NASA CR, October 19 Author: C.F.

Shieh, W. Frost. Atmospheric flow over two-dimensional bluff surface obstructions / (Washington: National Aeronautics and Space Administration, ), by Juergen Bitte, Walter Frost, George C. Marshall Space Flight Center, and University of Tennessee (Knoxville campus).

Space Institute (page images at HathiTrust). George C. Marshall Space Flight Center. Books from the extended shelves: Atmospheric flow over two-dimensional bluff surface obstructions / (Washington: George C. Marshall Space Flight Center: Atmospheric turbulence simulation techniques with application to flight analysis /.

The effects of the distorted flow- in the wake behind two-dimensional bluff surface obstacles, in a turbulent boundary layer, upon emissions of various freight and downwind locations is evaluated.

A source elevated to only times the obstacle height is found to be greatly influenced unless it is placed farther than 10 obstacle heights downwind. The effects of the distorted flow, in the wake behind two-dimensional bluff surface obstacles in a turbulent boundary layer, upon emissions of various height and downwind locations is evaluated.

A source elevated to only times the obstacle height is found to be greatly influenced unless it is placed farther than 10 obstacle heights downwind. Meroney, R.N., FLUID DYNAMICS OF FLOW OVER HILLS AND MOUNTAINS: Insights Obtained Through Physical Modeling, Chapter 7 of AMS Monograph on Current Directions in Atmospheric Processes Over Complex Terrain, AMS Monograph Vol Num Junepp.

The impact of atmospheric boundary layer (ABL) interactions with large-scale stably stratified flow over an isolated, two-dimensional hill is investigated using turbulence-resolving large-eddy. an analytical solution is presented for the flow of an adiabatic turbulent boundary layer on a uniformly rough surface over a two-dimensional hump Author: Neil Jerram.

Engineering Turbulence Modelling and Experiments 6 found to exist in the mixing layer at Mc = and their formation mechanism shows good agreement with the model of flow around a bluff body.

The effect of compressibility on the large-scale structures is stronger than that on the small-scale ones. SIO appears over the suction side of a. On a two-dimensional mode-matching technique for sound generation and transmission in axial-flow outlet guide vanes Journal of Sound and Vibration, Vol.

Causal mechanism behind the stall delay by airfoil’s pitching-up motionCited by: c. 1 inch is equal to 5, inches on the Earth's surface d. 1 nautical mile on the chart is equal to 5, inches on the Earth's surface When the index and horizon mirrors of a properly adjusted sextant are at an angle of 45° to each other, the arc reads __________.

The fluid is moving faster over the upper surface, particularly near the leading edge, than over the lower surface so the pressure on the upper surface is lower than the pressure on the lower surface.

The difference in pressure between the upper and lower surfaces results in lift. End new section; Michael Belisle9 February (UTC). Unfortunately, this book can't be printed from the OpenBook.

If you need to print pages from this book, we recommend downloading it as a PDF. Visit to get more information about this book, to buy it in print, or to download it as a free PDF.

The average localized mist density, based on a combined total flow averaged over the entire compartment floor area, ranged from Lpm/m2 ( gpm/W) which corresponds to a volumetric density of Lpm/m3 ( gpm/ft2).

Convection in Porous Media Number Flow at Low Rayleigh Number Flow at Intermediate Rayleigh Number Vertical Cylinder Cone General Two-Dimensional or Axisymmetric Surface Horizontal Line Heat Source Flow at High Rayleigh Number Darcy Model Forchheimer Model Flow at Low Rayleigh Number Point Heat.

Search the history of over billion web pages on the Internet. search Search the Wayback Machine. Featured texts All Books All Texts latest This Just In Smithsonian Libraries FEDLINK (US) Genealogy Lincoln Collection Full text of "Principles Of Heat Transfer Fourth Edition".

Search the history of over billion web pages on the Internet. search Search the Wayback Machine. Featured texts All Books All Texts latest This Just In Smithsonian Libraries FEDLINK (US) Genealogy Lincoln Collection.

National Emergency Library. Top Full text of "Fluid. Transport Phenomena in Porous Media II covers a wide range of the engineering and technological applications, including both stable and unstable flows, heat and mass transfer, porosity, and ort Phenomena in Porous Media II is the second volume in a series emphasising the fundamentals and applications of research in porous media.

Lamb presented the first analysis of this phenomenon for the case of a two‐dimensional, circular, stationary cylinder beneath the free surface of a steady, uniform, potential flow. He arrived at an expression for the wave drag force per unit length of cylinder that was rewritten by Alonso [] to yield the following expression for the wave Cited by: 1.

Two-Dimensional Water-Surface Computer Models 2. One-Dimensional Unsteady Flow Models 3. Starting Water-Surface Elevations 4. Modeling Techniques for Streams with Supercritical Flow Regimes. Split-Flow Analyses CHAPTER 6. APPROXIMATE FLOODPLAIN BOUNDARY DELINEATIONS AND SIMPLIFIED METHODS.

CHAPTER 7. Prepare for or supplement your studies for your USCG license exam here. Click here to create an account and enter SeaSources new online study. And, no nourishing, connecting flow to make it a viable river and waterway will be required again until NEXT April, at the earliest.

It just sits—baking, starved of water. During this spring’s migration season just over 7% of theshad that passed. Flow of a real fluid-effect of viscosity on fluid flow-laminarand turbulent flow-boundary layer thickness-displacement, momentumand energy thickness-flow through pipes-laminar and turbulent flow inpipes-critical Reynolds number-Darcy-Weisback equation-hydraulicradius-Moody;s chart-pipes in series and parallel-siphon losses inpipes-power.

L45 Ideal Flow over a circular cylinder, D Alembert s Paradox, Magnus effect, Kutta Jonk owski s Theorem, Starting Vortex, Kutta condition, Real flow over smooth and rough cylinder. Vortex Filament, Biot and Savart Law, Bound Vortex and trailing Vortex, Horse Sh oe Vortex, Lifting Line Theory and its limitations.

SIAM Journal on Scientific ComputingAA Abstract | PDF ( KB) () Numerical simulation of the motion of an ice keel in a stratified by: mph) wind speeds for over 5 minutes without growth me dia scour (or module displacement if air flow was prevented from reaching the underside of the tested specimen).

Also, the researchers showed that in the extreme case where no vegetation coverage or moisture was provided, growth media scour could occur at wind speeds as low as 13 m/s (30 mph).

For example, FE-SEM analysis of surface samples removed from Abbey’s The Spirit of Light ( x cm) revealed that the efflorescence appears as plate-like structures ( microns wide and less than 1 micron thick) on the surface of the painting, and EDS showed that the efflorescence is composed primarily of carbon and zinc.

The two-dimensional, laterally averaged model CE-QUAL-W2 was used to simulate water velocity, ice cover, water temperature, specific conductance, dissolved and suspended solids, dissolved oxygen, total nitrogen, ammonia, nitrate, total phosphorus, orthophosphate, dissolved and particulate organic matter, and three algal groups.

Tuttle SG, Chaudhuri S, Kostka S, Kopp-Vaughan KM, Jensen TR, Cetegen BM, Renfro MW () Time-resolved blowoff transition measurements for two-dimensional bluff body-stabilized flames in vitiated flow. Combust Flame – CrossRef Google ScholarAuthor: Medhat A. Nemitallah, Mohamed A. Habib, Hassan M.

Badr. Texas Tech University. Wind Science and Engineering Research Center Texas Tech Wind Science and Engineering Research Center Records, and undated The Texas Tech Wind Science and Engineering Research Center Records contain reports, research data, books, and printed material related to that organization's activities in the documentation, research.

Peter Hernon. The New Madrid Seismic Zone is miles, stretching across five states. In and enormous earthquakes erupted along this zone, affecting 24 states, creating lakes in Tennessee and causing the Mississippi River to run backward.

In Peter Hernon’s the New Madrid awakens, threatening the country with systematic collapse in a chillingly plausible case. (abbrev. AO)- The Arctic Oscillation is a pattern in which atmospheric pressure at polar and middle latitudes fluctuates between negative and positive phases.

The negative phase brings higher-than-normal pressure over the polar region and lower-than-normal pressure at about 45 degrees north latitude. Download this file. lines ( with data), MB. Binder, BJ, Blyth, Mark and Balasuriya, S () Steady free-surface flow over spatially periodic topography.

Journal of Fluid Mechanics, ISSN Binder, Benjamin J., Blyth, M. G and McCue, Scott W. () Free-surface flow past arbitrary topography and an inverse approach for wave-free solutions.

Measurement and Instrumentation Principles 65 Determination of the frequency at which instruments should be calibrated is dependent upon several factors that require specialist knowledge. If an instrument is required to measure some quantity and an inaccuracy of š2% is acceptable, then a certain amount of performance degradation can be allowed.

A model for predicting the sediment transport capacity of turbulent interrill flow on rough surfaces is developed from flume experiments with flow depths ranging from to mm, flow velocities from to m s super(-1), Reynolds numbers from toFroude numbers from tobed slopes from degree to 10 degree, sediment diameters.

The returns from drift bottles launched in the Gulf of Maine area since have been analyzed to determine the annual cycle of surface drift. The source of surface flow into the Bay of Fundy expands from a minimum during January in the offing of the eastern side of the bay to a maximum in May which includes most of Georges Bank.

Search the history of over billion web pages on the Internet. search Search the Wayback Machine. Featured texts All Books All Texts latest This Just In Smithsonian Libraries FEDLINK (US) Genealogy Lincoln Collection.

National Emergency Full text of "Aeronautical dictionary". In the first book of the series, which dealt with classic science fiction (s.f.) novellas of the s, I said that the s was the decade in which science fiction found its the end of that decade, the voice began to resemble, more and more, that of John Wood Campbell, Jr., and in the s, J.W.C.

dominated the field to the point where to many he seemed all of science. The 1 4th Multidisciplinary Conference on Sinkholes and the Engineering & Environmental Impacts of Karst Page 19 AM John D.

Barry and Jeffrey A. Green, Minnesota Dept. of Natural Resources; Julia R Steenberg, Minnesota Geological Survey Conduit Flow in the Cambrian Lone Rock Formation, Southeast Minnesota, U.S.A.

AM Kimm Crawford.Biblioteca en línea. Materiales de aprendizaje gratuitos. Ninguna Categoria; Subido por delvis Heat Exchanger Design Handbook, 2nd Ed (1).Department of Mathematical Sciences SCEN University of Arkansas Fayetteville, AR P F E-mail: [email protected]