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
Jess, Edward O. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
500-mb prognoses computed with a barotropic model from progressively lessening amounts of data, showed increasing statistical differences. These differences also grew with the passage of time. With increasing paucity of data, the smaller meteorological features disappeared, while larger features were smoothed and suffered a change in speed of motion. Random errors, which simulated a natural error source, were added to the data. This appeared to intensify and decelerate the features on the prognostic charts.DOI: 10.1111/j.2153-3490.1960.tb01280.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • BERGGRENR.,, 1957: O n the Accuracy of 500 mb Analysis with Reference to Numerical Forecasting. Tellus, 9, pp. 323-340.
    • BERGTHOBSSOP.N,,et. als., 1955: Routine Forecasting with the Barotropic Model, Tellus, 7, pp. 272-274.
    • BERGTHORSSPO.,ND, ijos, B., 1955: Numerical Weather Map Analyses, Tellus, 7. pp. 329-340.
    • BEST,W . H., 1956: Differencesin Numerical Prognoses Resulting from Differences in Analyses, Tellus, 8, PP. 351-356.
    • BOLIN,B., 1955: Numerical Forecasting with the Barotropic Model, Tellus, 7, pp. 27-49.
    • CONRADV, ., and POLLAKL,. W., 1950: Methods in Climatology, Cambridge; Harvard University Press, 459.
    • Doos, B. R., 1956: Automation of 500 mb Forecasts Through Successive Numerical Map Analyses, Tellus, 8, pp. 76-81.
    • ELLSAESSEHR. ,W., 1956: Errors in Upper Level Wind Forecasts, AWS Technical Report, No. IOS-140/1, Washington, U.S.A.F., p. 17.
    • FJ0RTOFT, R., 1953: O n the Changes in the Spectral Distribution of Kinetic Energy for Two-Dimensional, Non-Divergent Flow, Tellus, 5, pp. 225-230.
    • PETTEASESN.,, 1957: A Note on Verification of Prognostic Charts, Tellus, 9, pp. 313-31s.
    • PHILLIPSN,. A., 1958: An Example of Non-Linear Computational Instability. To be published in Rossby Memorial Volume.
    • THOMPSONP., D., 1957: Uncertainty of Initial State as a Factor in the Predictability of Large Scale Atmospheric Flow Patterns, Tellus, 9 , pp. 275-295.
  • No related research data.
  • No similar publications.

Share - Bookmark

Cite this article

Collected from