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
Warner, J. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
Measurements have been made of liquid water content throughout many cumuliform clouds. The amount of water present at any level was always less than the adiabatic value, and the ratio of these two quantities decreased with height above cloud base. This ratio was found to be independent of the horizontal extent of the cloud except in the case of very small clouds. The transition between clear air and dense cloud was frequently abrupt.DOI: 10.1111/j.2153-3490.1955.tb01183.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • HOUGHTONH,. C. and H. E. CRAMER1,951: A theory of en rainment in convective currents. J. Met., 8, pp. 95-102.
    • MALKUSJ,. S., 1949: Effects of wind shear on some aspects of convection. Trnns. Amer. Geophy. Union, 3 0 , pp. 19-25.
    • MALKU SJ., S., 1952 a: Recent advances in the study of convective clouds and their interaction with the environment. Tellus, 4, pp. 71-87.
    • MALKUSJ,. S., 1952 b: The slopes of cumulus clouds in relation to external wind shear. Quart. J. R. Met. SOC.,78, pp. 530-542.
    • MALKUSJ,. S., 1954: Some results of a trade-cumulus cloud investigation. J. Met., 11, pp. 220-237.
    • MALKUSJ,. S. and SCORERR, . S., 1954: Marine meteorology-Erosion of cumulus towers. Woods Hole Oceanographic Inst., Ref. No. 54-55. Unpublished manuscript.
    • SCORERR, . S. and LUDLAMF,. H., 1933: Bubble theory of penetrative convection. Qtiarf.J. R. Mef. Soc., 79, pp. 94-103.
    • STOMMELH,., 1947: Entrainment of air into a cumulus cloud. Pt. I..J. Met., 4, pp. 91-94.
    • STOMMELH,., 1951 : Entrainment of air into a cumulus cloud. Pt. 11. J. Met., 8, pp. 127-129.
    • WARNERJ., and NEWNHAMT,. D., 1952: A new method of measurement of cloud-water content. Qunrt. J. R. Met. Soc., 78, pp. 46-52.
    • WARNEJR.,and BOWENE,. G., 1953: A new method of studying the fine structure of air movements in the free atmosphere. Tellus, 5 , pp. 36-41.
    • WEICKMANHN. , K. and AUFM KAMPE,H. J., 1953: Physical properties of cumulus clouds. J. Met., 10. pp. 204-211.
    • ZNTSEV,V. A,, 1950: Water content and distribution of drop in cumulus clouds. Glau. geofiz. Observ., Trudy, 19, pp. 122-132.
  • No related research data.
  • No similar publications.

Share - Bookmark

Cite this article

Collected from