Search Results
Airborne Wind Lidar Measurements of Vertical and Horizontal Winds for the Investigation of Orographically Induced Gravity Waves.1002/2015JD023197 Browning , K. , and R. Wexler , 1968 : The determination of kinematic properties of a wind field using Doppler radar . J. Appl. Meteor. , 7 , 105 – 113 , doi: 10.1175/1520-0450(1968)007<0105:TDOKPO>2.0.CO;2 . 10.1175/1520-0450(1968)007<0105:TDOKPO>2.0.CO;2 Chen , C.-C. , G. J. Hakim , and D. R. Durran , 2007 : Transient mountain waves and their interaction with large scales . J. Atmos. Sci. , 64 , 2378 – 2400 , doi: 10.1175/JAS3972.1 . 10.1175/JAS3972.1 Chouza , F
.1002/2015JD023197 Browning , K. , and R. Wexler , 1968 : The determination of kinematic properties of a wind field using Doppler radar . J. Appl. Meteor. , 7 , 105 – 113 , doi: 10.1175/1520-0450(1968)007<0105:TDOKPO>2.0.CO;2 . 10.1175/1520-0450(1968)007<0105:TDOKPO>2.0.CO;2 Chen , C.-C. , G. J. Hakim , and D. R. Durran , 2007 : Transient mountain waves and their interaction with large scales . J. Atmos. Sci. , 64 , 2378 – 2400 , doi: 10.1175/JAS3972.1 . 10.1175/JAS3972.1 Chouza , F
kinematic displacement In (12) , we use the perturbation vertical velocity w ′( x ) and total along-track wind speed U ( x ) ( Smith et al. 2008 ). The mean vertical velocity has been subtracted from each leg according to . The integral begins at the upwind end of the cross-mountain leg. The d ( x ) patterns for RF12 and RF16 are shown in Fig. 9 for all cross-mountain legs. These traces show the smooth upwind region, the waves over the mountain crest, and the short periodic waves downwind. The
kinematic displacement In (12) , we use the perturbation vertical velocity w ′( x ) and total along-track wind speed U ( x ) ( Smith et al. 2008 ). The mean vertical velocity has been subtracted from each leg according to . The integral begins at the upwind end of the cross-mountain leg. The d ( x ) patterns for RF12 and RF16 are shown in Fig. 9 for all cross-mountain legs. These traces show the smooth upwind region, the waves over the mountain crest, and the short periodic waves downwind. The
