Diurnal variations during the Australian Monsoon Experiment (AMEX) Phase II

24Citations
Citations of this article
12Readers
Mendeley users who have this article in their library.
Get full text

Abstract

The tropical cloudiness, as inferred from satellite and radar data, averaged over the entire period of AMEX Phase II, was at a maximum during the morning over the ocean and during the late afternoon over the Arnhem Land region of northern Australia. The diurnal variation in high cloud, as measured by satellite was 3:2 over the ocean and 4:1 over Arnhem Land. Radar data indicated a 10:1 variation in convection over Armhem Land, a 2:1 variation over the neighboring ocean and a 3:2 variation in the stratiform echoes over both Arnhem Land and the neighboring ocean. -from Authors

Cite

CITATION STYLE

APA

Keenan, T. D., McBride, J., Holland, G., Davidson, N., & Gunn, B. (1989). Diurnal variations during the Australian Monsoon Experiment (AMEX) Phase II. Monthly Weather Review, 117(11), 2535–2552. https://doi.org/10.1175/1520-0493(1989)117<2535:dvdtam>2.0.co;2

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free