FLOW OVER AN ISOLATED HILL OF MODERATE SLOPE

被引：180

作者：

MASON, PJ

SYKES, RI

机构：

[1] Meteorological Office, Bracknell, Berkshire

来源：

QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY | 1979年 / 105卷 / 444期

关键词：

D O I：

10.1002/qj.49710544405

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

A two‐dimensional theory of Jackson and Hunt for turbulent flow over a shallow ridge is extended to three‐dimensional topography. The results are compared both with theoretical results for a ridge and with surface wind observations from a nearly circular isolated hill. Agreement between theory and observations is encouraging. Copyright © 1979 Royal Meteorological Society

引用

页码：383 / 395

页数：13

共 11 条

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[7] 2
[8] MASON PJ, 1979, Q J ROY METEOR SOC, V105, P129, DOI 10.1002/qj.49710544309
[9] STRATIFICATION EFFECTS IN BOUNDARY-LAYER FLOW OVER HILLS
SYKES, RI
[J]. PROCEEDINGS OF THE ROYAL SOCIETY OF LONDON SERIES A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1978, 361 (1705): : 225 - 243
[10] TAYLOR P A, 1977, Boundary-Layer Meteorology, V12, P37, DOI 10.1007/BF00116397

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