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
BRATSETH, ARNE M. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
An iterative method is suggested, by which the gravity modes of a primitive shallow water equation model are damped very efficiently while the meteorological modes are preserved fairly well. The model equations are integrated in a forward/backward cycle. It is shown that information about the normal modes of the model can be used to increase the damping rate even if these modes are not known explicitly. The meteorological modes can be conserved by keeping the relevant terms constant during each iteration cycle. Experiments with a simple one-dimensional model show that this model reaches a balanced state after a couple of iterations.DOI: 10.1111/j.2153-3490.1982.tb01824.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • Kurihara, Y. and Tripoli, G. J. 1976. An iterative time Symposium on Num. Wea. Pred., vol. VI, pp. 11-20. integration scheme designed to preserve a low- Tokyo, Japan, 1968. frequency wave. Mon.Weu.Rev. 104,761-764. Okland, H.1972. On the balance, initialization and data
    • Machenhauer, B. 1977. On the dynamics of gravity assimilation in primitive equation prediction models. J . oscillations in a shallow water model, with appli- Atmos. Sci.29,64 1-648. cations to normal mode initialization. Contrib. A fmos. Temperton, C. and Williamson, D. L. 1979. Normal Phys. 50,253-271. mode initialization for a multi-level gridpoint model.
    • Nitta, T. 1969. Initialization and analysis for the ECMWF Technical Report No. I1,91 pp. primitive equation model. Proc. of the WMOIIUGG
  • No related research data.
  • No similar publications.

Share - Bookmark

Cite this article

Collected from