LOGIN TO YOUR ACCOUNT

Username
Password
Remember Me
Or use your Academic/Social account:

CREATE AN ACCOUNT

Or use your Academic/Social account:

Congratulations!

You have just completed your registration at OpenAire.

Before you can login to the site, you will need to activate your account. An e-mail will be sent to you with the proper instructions.

Important!

Please note that this site is currently undergoing Beta testing.
Any new content you create is not guaranteed to be present to the final version of the site upon release.

Thank you for your patience,
OpenAire Dev Team.

Close This Message

CREATE AN ACCOUNT

Name:
Username:
Password:
Verify Password:
E-mail:
Verify E-mail:
*All Fields Are Required.
Please Verify You Are Human:
fbtwitterlinkedinvimeoflicker grey 14rssslideshare1
RYDBERG, LARS (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
Rotating deep-water channel flow is considered. The concept of critical flow is redefined for “wide” channels (with depth variations across the channel) where strong variations of the interface height occur along the flow. Numerical solutions are obtained for the flow structure across the channel, and a criterion for the interior interface height upstream the channel as a function of prescribed flow is presented. The solutions are compared to hydrographic observations from the Bornholm Strait (within the Baltic) and the Faroe Bank Channel with encouraging results. The present theory allows for frictional effects within the channel, and the results differ qualitatively from earlier contributions to this subject.DOI: 10.1111/j.2153-3490.1980.tb01724.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • Anati, D., Ass&, D. and Thompson, R. 1977. Laboratory models of sea straits. J. Fluid Me&. 81, 34 1-35 1.
    • Crease, 3. 1965. The flow of Norwegian Sea Water through the Faroe Bank Channel. Deep-sea Res. 12, 143-1 50.
    • Gill, A. E. 1977. The hydraulics of rotating-channel flow. J. Fluid Mech. 80,64 1-670.
    • Lundberg, R. 1977. On the mechanics of the deep water flow in the Bornholm Channel. Rep. No. 20, Oceanografiska Inst., Goteborgs Universitet, Gothenburg.
    • Lundberg, P. and Rydberg, L. 1979. Observations of the deep-water flow in the Bornholm Basin. (To appear as a report of Dept. of Oceanography, University of Gothenburg.)
    • Rydberg, L. 1978. Deep-water flow and oxygen consumption within the Baltic. Rep. No. 27, Oceanografiska Inst., Goteborgs Universitet, Gothenburg.
    • Sambuco, E. and Whitehead, J. A. 1976. Hydraulic control by a wide weir in a rotating fluid. J. Fluid Mech. 73,521-529.
    • Smith, P. C. 1975. A streamtube model for bottom boundary currents in the ocean. Deep-sea Res. 22, 85 3-8 73.
    • Tait, J. B., ed. 1976. The Iceland-Faroe Ridge International (ICES) “Overtlow” Expedition, May-June 1960. Cons. Int. Explor. Mer. Rapp. Proc. Verb. Reun., 157.
    • Taylor, G., Turner, J. and Morton, B. R. 1956. Turbulent gravitational convection from maintained and instantaneous sources. Proc. Roy. SOCA. 36, 1-23.
    • Walin, G. and Petrcn, 0. 1976. Some observations of the deep-flow in the Bornholm Strait during the period June 1973-December 1974. Tellus 28,7687.
    • Walin, G. 1977. A theoretical framework for the description of estuaries. Tellus 29, 128-136.
    • Whitehead, J. A., Leetma, A. and Knox, R. A. 1974. Rotating hydraulics of strait and sill flows. Geophysical FI. Dyn. 6, 101-125.
  • No related research data.
  • No similar publications.

Share - Bookmark

Cite this article

Collected from