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
Gryning, Sven-Erik; Mahrt, L.; Larsen, Søren (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
Observations of slope flows in a coastal valley are analyzed. The diurnal variation of upslope and downslope flows depends on season in a systematic way which appears to be related to the high latitude of the observational site and the presence of a nearby layer of marine air. Summer nocturnal flow over the sloping valley floor was studied during a special observing campaign. A downslope gravity flow interacts with even colder surface air at the valley floor. The latter originates as cold marine air or previous drainage of cold air. Regular oscillations, which appear to be trapped, terrain-related, internal gravity waves, exert a major influence on the downslope flow and its interaction with pre-existing cold air at the floor of the valley.DOI: 10.1111/j.1600-0870.1985.tb00281.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • Banta, R. 1984. Daytime boundary-layer evolution over mountainous terrain (I). Observations of the dry circulations. Mon. Wea. Rev. 112. 34C356.
    • DHI, 1979. Hydrografiske unders0gelser Narssaq 1979. (Hydrographical investigations Narssaq 1979). In Danish. Dansk Hydraulisk Institut. Hersholm. Denmark. Work carried out for The Greenland Technical Organization, Copenhagen, Denmark.
    • Geiger, R. 1975. The climate near the ground. Harvard University Press, 6 11 pp.
    • Gryning, S. E. 1981. Elecated source SF,-tracer dispersion experiments in the Copenhagen area. RiseR-446. Rise National Laboratory, DK-4000 Roskilde, Denmark, 187 pp.
    • Gryning, S. E. and Thomson. D. W. 1979. A tall-tower instrument system for mean and fluctuating velocity. fluctuating temperature and sensible heat flux measurements. J . Appl. Meteorol. 18, 1674-1 678.
    • Gryning, S. E. and Lyck, E. 1983.A tracer inrestigation of the atmospheric dispersion in the Dyrnces calley, Greenland. Rise-R-48I . Rise National Laboratory. DK-4000 Roskilde. Denmark, 67 pp.
    • Haltiner. G. J . 197 I . Numerical weather prediction. New York, J. Wiley and Sons Inc. 3 1 7 pp.
    • Heywood, G. S. P. 1933. Katabatic winds in a valley. Q . J . R . Meteoroi. Soc. 59.4 7-5 8.
    • Kristensen, L. 1983.Meteorological measurements at the KcaneJeld in the period September 1979-March 1983. Work carried out for the Uranium Project. Rise National Laboratory. DK-4000 Roskilde. Denmark.
    • Perkin. R. G. and Lewis. E. L. 1978. Mixing in an arctic fjord. J . Phjls. Oceanogr. 8.873-880.
    • Schnelle. F. 1963. Frostschutz in Pflanzenbau, vol. 1. Bayer Landwirtschafts Verlag. Miinchen. 488 pp.
    • Stigebrandt, A. 1976. Vertical diffusion driven by internal waves in a sill fjord. J . Phys. Oceanogr. 6 , 486-495.
    • Turner, J. L. 1981. Small-scale mixing processes. In: Eaolution of physical oceanographj1 (eds. B. A. Warren and C. Wunsck). The MIT Press. 236-262.
  • No related research data.
  • No similar publications.

Share - Bookmark

Cite this article

Collected from