Change search
Refine search result
1617181920 361 - 380 of 389
CiteExportLink to result list
Permanent link
Cite
Citation style
  • apa
  • ieee
  • modern-language-association-8th-edition
  • vancouver
  • Other style
More styles
Language
  • de-DE
  • en-GB
  • en-US
  • fi-FI
  • nn-NO
  • nn-NB
  • sv-SE
  • Other locale
More languages
Output format
  • html
  • text
  • asciidoc
  • rtf
Rows per page
  • 5
  • 10
  • 20
  • 50
  • 100
  • 250
Sort
  • Standard (Relevance)
  • Author A-Ö
  • Author Ö-A
  • Title A-Ö
  • Title Ö-A
  • Publication type A-Ö
  • Publication type Ö-A
  • Issued (Oldest first)
  • Issued (Newest first)
  • Created (Oldest first)
  • Created (Newest first)
  • Last updated (Oldest first)
  • Last updated (Newest first)
  • Disputation date (earliest first)
  • Disputation date (latest first)
  • Standard (Relevance)
  • Author A-Ö
  • Author Ö-A
  • Title A-Ö
  • Title Ö-A
  • Publication type A-Ö
  • Publication type Ö-A
  • Issued (Oldest first)
  • Issued (Newest first)
  • Created (Oldest first)
  • Created (Newest first)
  • Last updated (Oldest first)
  • Last updated (Newest first)
  • Disputation date (earliest first)
  • Disputation date (latest first)
Select
The maximal number of hits you can export is 250. When you want to export more records please use the Create feeds function.
  • 361.
    Andersson, Lars
    et al.
    SMHI, Core Services.
    Rahm, Lars
    SMHI, Research Department, Oceanography.
    THERMALLY DRIVEN CIRCULATION WITHIN AN EXPERIMENTAL ENCLOSURE1990In: Estuarine, Coastal and Shelf Science, ISSN 0272-7714, E-ISSN 1096-0015, Vol. 30, no 2, p. 111-129Article in journal (Refereed)
  • 362. WULFF, F
    et al.
    STIGEBRANDT, A
    Rahm, Lars
    SMHI, Research Department, Oceanography.
    NUTRIENT DYNAMICS OF THE BALTIC SEA1990In: Ambio, ISSN 0044-7447, E-ISSN 1654-7209, Vol. 19, no 3, p. 126-133Article in journal (Refereed)
  • 363.
    Svensson, Urban
    et al.
    SMHI, Research Department, Oceanography.
    Omstedt, Anders
    SMHI, Research Department, Oceanography.
    A MATHEMATICAL-MODEL OF THE OCEAN BOUNDARY-LAYER UNDER DRIFTING MELTING ICE1990In: Journal of Physical Oceanography, ISSN 0022-3670, E-ISSN 1520-0485, Vol. 20, no 2, p. 161-171Article in journal (Refereed)
  • 364.
    Carlberg, Stig
    et al.
    SMHI, Core Services.
    Engström, Sven
    SMHI.
    Fonselius, Stig
    SMHI, Research Department, Oceanography.
    Palmén, Håkan
    SMHI.
    Thelén, Eva-Gun
    SMHI.
    Fyrberg, Lotta
    SMHI, Core Services.
    Zagradkin, Danuta
    SMHI.
    Juhlin, Bo
    SMHI, Core Services.
    Szaron, Jan
    SMHI.
    Program för miljökvalitetsövervakning – PMK: Utsjöprogram under 19881989Report (Other academic)
  • 365.
    Fransson, L.
    et al.
    SMHI.
    Håkansson, Bertil
    SMHI, Research Department, Oceanography.
    Omstedt, Anders
    SMHI, Research Department, Oceanography.
    Stehn, L.
    SMHI.
    Sea ice properties studied from the ice-breaker Tor during BEPERS-881989Report (Other academic)
  • 366.
    Häggkvist, Kenneth
    et al.
    SMHI, Professional Services.
    Svensson, Urban
    SMHI, Research Department, Oceanography.
    Taesler, Roger
    SMHI, Research Department.
    NUMERICAL SIMULATIONS OF PRESSURE FIELDS AROUND BUILDINGS1989In: Building and Environment, ISSN 0360-1323, E-ISSN 1873-684X, Vol. 24, no 1, p. 65-72Article in journal (Refereed)
  • 367.
    Rahm, Lars
    et al.
    SMHI, Research Department, Oceanography.
    Svensson, Urban
    SMHI, Research Department, Oceanography.
    Dispersion in a stratified benthic boundary layer1989In: Tellus. Series A, Dynamic meteorology and oceanography, ISSN 0280-6495, E-ISSN 1600-0870, Vol. 41A, no 2Article in journal (Refereed)
    Abstract [en]

    A dispersion model for the stratified benthic boundary layer is formulated. It is based on "small-scale" vertical dispersion and a "large-scale" horizontal flow field. A modified Langevin equation governs the stochastic vertical migration of an ensemble of marked fluid elements. These elements are spread out by the horizontal flow, determined by a one-dimensional model, which includes a two-equation (k - epsilon) turbulence scheme. The later yields statistical information necessary for the stochastic process. Statistical properties of the dispersion process are then calculated from the evolution of the ensemble of elements. A rather idealized case with a linearly stratified fluid subject to a suddenly imposed barotropic pressure gradient is considered. A quasi-geostrophic interior flow is formed with a benthic boundary layer at the bottom. Marked fluid elements are released at the bottom and then followed for several pendulum days. It is found that the dispersion process is well characterized by K = Cu(*)l/(where u(*) and l are the friction velocity at the bottom and the layer thickness, respectively), and where C approximate to 15. A similar relation but based on external parameters only, becomes: K = C-b vertical bar partial derivative P/partial derivative y vertical bar(2)/rho(2) f(5/2) N-1/2, where C-b approximate to 0.11 in the range N/f = 28- 88

  • 368.
    Rahm, Lars
    et al.
    SMHI, Research Department, Oceanography.
    Svensson, Urban
    SMHI, Research Department, Oceanography.
    ON THE MASS-TRANSFER PROPERTIES OF THE BENTHIC BOUNDARY-LAYER WITH AN APPLICATION TO OXYGEN FLUXES1989In: NETHERLANDS JOURNAL OF SEA RESEARCH, ISSN 0077-7579, Vol. 24, no 1, p. 27-35Article in journal (Refereed)
  • 369.
    Svensson, Urban
    et al.
    SMHI, Research Department, Oceanography.
    Sahlberg, Jörgen
    SMHI, Professional Services.
    FORMULAS FOR PRESSURE-GRADIENTS IN ONE-DIMENSIONAL LAKE MODELS1989In: JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, Vol. 94, no C4, p. 4939-4946Article in journal (Refereed)
  • 370.
    Håkansson, Bertil
    SMHI, Research Department, Oceanography.
    Ice reconnaissance and forecasts in Storfjorden, Svalbard1988Report (Other academic)
  • 371.
    Carlberg, Stig
    et al.
    SMHI, Core Services.
    Engström, Sven
    SMHI.
    Fonselius, Stig
    SMHI, Research Department, Oceanography.
    Palmén, Håkan
    SMHI.
    Thelén, Eva-Gun
    SMHI.
    Fyrberg, Lotta
    SMHI, Core Services.
    Zagradkin, Danuta
    SMHI.
    Program för miljökvalitetsövervakning – PMK: Utsjöprogram under 19871988Report (Other academic)
  • 372.
    Svensson, Urban
    et al.
    SMHI, Research Department, Oceanography.
    Rahm, Lars
    SMHI, Research Department, Oceanography.
    MODELING THE NEAR-BOTTOM REGION OF THE BENTHIC BOUNDARY-LAYER1988In: JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, Vol. 93, no C6, p. 6909-6915Article in journal (Refereed)
  • 373. WULFF, F
    et al.
    Rahm, Lars
    SMHI, Research Department, Oceanography.
    LONG-TERM, SEASONAL AND SPATIAL VARIATIONS OF NITROGEN, PHOSPHORUS AND SILICATE IN THE BALTIC - AN OVERVIEW1988In: Marine Environmental Research, ISSN 0141-1136, E-ISSN 1879-0291, Vol. 26, no 1, p. 19-37Article in journal (Refereed)
  • 374.
    Carlberg, Stig
    et al.
    SMHI, Core Services.
    Engström, Sven
    SMHI.
    Fonselius, Stig
    SMHI, Research Department, Oceanography.
    Palmén, Håkan
    SMHI.
    Thelén, Eva-Gun
    SMHI.
    Fyrberg, Lotta
    SMHI, Core Services.
    Program för miljökvalitetsövervakning – PMK: Utsjöprogram under 19861987Report (Other academic)
  • 375.
    Funquist, Lennart
    SMHI, Research Department, Oceanography.
    Numerisk beräkning av vågor i kraftverksdammar1987Report (Other academic)
    Abstract [sv]

    Kraftiga vågrörelser uppstår i kraftverksmagasin,  när avtappningen hastigt stryps. Detta kan vara fallet vid störningar i kraftverksdriften eller eldistributionsnätet.Om vattennivån i magasinet ligger nära dämningsgränsen, kan vågorna orsaka störningar i ytregleringsautomatiken och katastrofskyddet, samtidigt som dämningsgränsen kan överskridas. Liknande problem kan uppstå i korttidsreglerade magasin.Amplituder på upp till o.60 m har registrerats just vid utloppet (Stugun), medan längre uppströms endast registreras vågor med en amplitud mindre än 0.15 m. Initialt bildas vågor av flera frekvenser, och de högfrekventa och med högst  amplitud dämpas mycket kraftigt och försvinner efter 100 - 200 m. Vattenståndshöjningen, som orsakas av det plötsliga stoppet, är emellertid synlig i hela magasinet som en solitär våg med en amplitud av upp till 0.20 m. Dessutom uppstår egensvängningar i delbassänger nära utloppet med en amlitud på 0.05 - 0.15 m, vilket kan vara nog för att i vissa fall överskrida dämningsgränsen.Avsikten med den här redovisade studien är att utröna huruvida uppmätta vågor går att reproducera i en numerisk modell, och vidare om modellen kan tillämpas på godtyckligt magasin för studier av effekten av dessa vågor.

  • 376.
    Lundqvist, Jan-Eric
    et al.
    SMHI.
    Omstedt, Anders
    SMHI, Research Department, Oceanography.
    Isförhållandena i Sveriges södra och västra farvatten1987Report (Other academic)
  • 377.
    Fonselius, Stig
    SMHI, Research Department, Oceanography.
    Kattegatt - havet i väster1987Report (Other academic)
  • 378.
    Rahm, Lars
    SMHI, Research Department, Oceanography.
    OXYGEN-CONSUMPTION IN THE BALTIC PROPER1987In: Limnology and Oceanography, ISSN 0024-3590, E-ISSN 1939-5590, Vol. 32, no 4, p. 973-978Article in journal (Refereed)
  • 379.
    Funquist, Lennart
    et al.
    SMHI, Research Department, Oceanography.
    Gidhagen, Lars
    SMHI, Research Department, Air quality.
    Svensson, Urban
    SMHI, Research Department, Oceanography.
    THE MATHEMATICAL-MODELING OF BAROCLINIC WAVES AND FRONTS IN THE OCEAN1987In: Applied Mathematical Modelling, ISSN 0307-904X, E-ISSN 1872-8480, Vol. 11, no 1, p. 11-18Article in journal (Refereed)
  • 380.
    Omstedt, Anders
    SMHI, Research Department, Oceanography.
    FORECASTING WATERCOOLING IN THE KATTEGAT, THE ORESUND, THE BELT SEA AND THE ARKONA BASIN1987In: Nordic Hydrology, ISSN 0029-1277, E-ISSN 1996-9694, Vol. 18, no 4-5, p. 247-258Article in journal (Refereed)
1617181920 361 - 380 of 389
CiteExportLink to result list
Permanent link
Cite
Citation style
  • apa
  • ieee
  • modern-language-association-8th-edition
  • vancouver
  • Other style
More styles
Language
  • de-DE
  • en-GB
  • en-US
  • fi-FI
  • nn-NO
  • nn-NB
  • sv-SE
  • Other locale
More languages
Output format
  • html
  • text
  • asciidoc
  • rtf
v. 2.35.9
|