Open AccessInertia gravity wave generation by the tropospheric midlatitude jet as given by the Fronts and Atlantic Storm‐Track Experiment radio soundings
Author(s) -
Plougonven R.,
Teitelbaum H.,
Zeitlin V.
Publication year - 2003
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2003jd003535
Subject(s) - gravity wave , geology , jet stream , jet (fluid) , geophysics , stratosphere , gravitational wave , middle latitudes , storm track , troposphere , radio wave , orography , depth sounding , geopotential height , atmospheric sciences , storm , physics , meteorology , mechanics , astronomy , precipitation , oceanography , quantum mechanics
Generation of inertia gravity waves by the midlatitude tropospheric jet is studied on the basis of the data obtained from the radio soundings over the North Atlantic during the Fronts and Atlantic Storm‐Track Experiment campaign. A sample of 224 radio soundings is used to analyze the wave activity as a function of the distance to the jet. It is shown that radio soundings displaying the most intense gravity wave activity, both in the stratosphere and in the troposphere, are the ones closest to the jet axis. Thus the jet region is the dominant source of gravity waves in this region far from orography. Further examination allows for identification of two specific regions of the flow that are associated with intense gravity wave activity: the vicinity of the maximum of the jet velocity and the regions of strong curvature of the jet. The detailed case studies we provide suggest that geostrophic adjustment is the dynamical mechanism responsible for the generation of large‐amplitude inertia gravity waves in the regions of the strong curvature of the wind. The generation of waves in the vicinity of the regions where the wind veers, in the deep troughs of the geopotential, appears to be systematic.