Diurnal variation of the trade-wind boundary layer.

K. Brill, Bruce A Albrecht

Research output: Contribution to journalArticle

23 Citations (Scopus)

Abstract

Cloud fraction observations and trade-wind inversion base heights from both GATE and the undisturbed period of ATEX are examined for diurnal variation. The cloud fraction tends to be larger in the morning than in the afternoon. The inversion base height has a morning maximum and an afternoon minimum. -from Authors

Original languageEnglish (US)
Pages (from-to)601-613
Number of pages13
JournalMonthly Weather Review
Volume110
Issue number6
StatePublished - 1982
Externally publishedYes

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trade wind
diurnal variation
boundary layer
inversion

ASJC Scopus subject areas

  • Atmospheric Science

Cite this

Brill, K., & Albrecht, B. A. (1982). Diurnal variation of the trade-wind boundary layer. Monthly Weather Review, 110(6), 601-613.

Diurnal variation of the trade-wind boundary layer. / Brill, K.; Albrecht, Bruce A.

In: Monthly Weather Review, Vol. 110, No. 6, 1982, p. 601-613.

Research output: Contribution to journalArticle

Brill, K & Albrecht, BA 1982, 'Diurnal variation of the trade-wind boundary layer.', Monthly Weather Review, vol. 110, no. 6, pp. 601-613.
Brill, K. ; Albrecht, Bruce A. / Diurnal variation of the trade-wind boundary layer. In: Monthly Weather Review. 1982 ; Vol. 110, No. 6. pp. 601-613.
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