THE FORMATION OF AREALLY-AVERAGED ROUGHNESS LENGTHS

[1] ON THE EFFECTIVE ROUGHNESS LENGTH FOR USE IN NUMERICAL 3-DIMENSIONAL MODELS [J]. BOUNDARY-LAYER METEOROLOGY, 1986, 35 (03) : 231 - 245

[2] ARYA SPS, 1975, Q J ROY METEOR SOC, V101, P147

[3] A MIXED SPECTRAL FINITE-DIFFERENCE MODEL FOR NEUTRALLY STRATIFIED BOUNDARY-LAYER FLOW OVER ROUGHNESS CHANGES AND TOPOGRAPHY [J]. BOUNDARY-LAYER METEOROLOGY, 1987, 38 (03) : 273 - 303

[4] BUSINGER JA, 1971, J ATMOS SCI, V28, P181, DOI 10.1175/1520-0469(1971)028<0181:FPRITA>2.0.CO

[5] 2

[6] Fiedler F., 1972, Q J ROY METEOR SOC, V98, P213, DOI DOI 10.1002/QJ.49709841519

[7] TURBULENT WIND FLOW OVER A LOW HILL [J]. QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1975, 101 (430) : 929 - 955

[8] JENSEN NO, 1978, Q J ROY METEOR SOC, V104, P351, DOI 10.1002/qj.49710444009

[9] JENSEN NO, 1984, WMO WCP86 REP

[10] Launder B.E., 1972, MATH MODELS TURBULEN

[1] ON THE EFFECTIVE ROUGHNESS LENGTH FOR USE IN NUMERICAL 3-DIMENSIONAL MODELS [J]. BOUNDARY-LAYER METEOROLOGY, 1986, 35 (03) : 231 - 245

[2] ARYA SPS, 1975, Q J ROY METEOR SOC, V101, P147

[3] A MIXED SPECTRAL FINITE-DIFFERENCE MODEL FOR NEUTRALLY STRATIFIED BOUNDARY-LAYER FLOW OVER ROUGHNESS CHANGES AND TOPOGRAPHY [J]. BOUNDARY-LAYER METEOROLOGY, 1987, 38 (03) : 273 - 303

[4] BUSINGER JA, 1971, J ATMOS SCI, V28, P181, DOI 10.1175/1520-0469(1971)028<0181:FPRITA>2.0.CO

[5] 2

[6] Fiedler F., 1972, Q J ROY METEOR SOC, V98, P213, DOI DOI 10.1002/QJ.49709841519

[7] TURBULENT WIND FLOW OVER A LOW HILL [J]. QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1975, 101 (430) : 929 - 955

[8] JENSEN NO, 1978, Q J ROY METEOR SOC, V104, P351, DOI 10.1002/qj.49710444009

[9] JENSEN NO, 1984, WMO WCP86 REP

[10] Launder B.E., 1972, MATH MODELS TURBULEN