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
Starr, Victor P. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:

Classified by OpenAIRE into

arxiv: Physics::Atmospheric and Oceanic Physics, Physics::Fluid Dynamics
The effect of gradients in the cross-current eddy motions on the geostrophic balance is illustrated by means of an integrated model. It is suggested that gradients of the Reynolds stress associated with such eddy motions in the atmosphere and in the oceans may lead to sensible average geostrophic departures which appear as a normal inertial effect in eddying currents.DOI: 10.1111/j.2153-3490.1950.tb00334.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • GOLDSTEINS,., 1938 : Modern developments in j?uid dynamics, Vol. I . Oxford University Press, 330 pp.
    • LOEWE,F., and U. RADOK,1950: A meridional aerological cross section in the Southwest Pacific. J . Meteor., 7, 58-65.
    • NEAMTASN.,M., 1946: The motion of harmonic waves in the atmosphere. /. Meteor., 3. 53-56.
  • No related research data.
  • No similar publications.

Share - Bookmark

Cite this article

Collected from