WIND PROFILES IN THE STABLE BOUNDARY-LAYER, AND THE EFFECT OF LOW RELIEF

被引:0
作者
GRANT, ALM
机构
关键词
D O I
10.1256/smsqj.51502
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Wind profiles through the stable boundary layer are presented. The data were collected at a site located in a shallow river valley and show evidence of upstream effects near the edge of the valley. The wind-speed profiles are consistent with a non-dimensional shear phi(m) = 1 + 3z/L for z/L < 0.5. Changes in wind speed and direction are found to occur over a greater depth than the depth of the turbulent nocturnal boundary layer estimated from various diagnostic formulae.
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页码:27 / 46
页数:20
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共 47 条
  • [1] ARYA SPS, 1975, Q J ROY METEOR SOC, V101, P147
  • [2] ARYA SPS, 1981, J APPL METEOROL, V20, P1192, DOI 10.1175/1520-0450(1981)020<1192:PTHOTS>2.0.CO
  • [3] 2
  • [4] BELJAARS ACM, 1985, KNMI852 SCI REP
  • [5] BOUWMAN P, 1990, KNMI TR13 TECHN RAP
  • [6] BROST RA, 1978, J ATMOS SCI, V35, P1427, DOI 10.1175/1520-0469(1978)035<1427:AMSOTS>2.0.CO
  • [7] 2
  • [8] Carson D. J., 1978, Boundary-Layer Meteorology, V14, P67, DOI 10.1007/BF00123990
  • [9] CAUGHEY SJ, 1979, J ATMOS SCI, V36, P1041
  • [10] Chintawongvanich P., 1989, J ATMOS OCEAN TECH, V6, P785, DOI [10.1175/1520-0426(1989)006&LT