Vertical short-scale structures in the upper tropospheric and lower stratospheric temperature and ozone at la Reunion Island (20.8 degrees S, 55.3 degrees E)
F. Chane-ming et al., Vertical short-scale structures in the upper tropospheric and lower stratospheric temperature and ozone at la Reunion Island (20.8 degrees S, 55.3 degrees E), J GEO RES-A, 105(D22), 2000, pp. 26857-26870
The distribution and the nature of vertical short-scale structures observed
in ozone and temperature are investigated in the upper troposphere and the
lower stratosphere at La Reunion Island located in the vicinity of the sou
thern subtropical barrier by using wavelet-based methods. A climatology of
dominant wavelike patterns with short vertical wavelengths reveals the pres
ence of localized structures on both the ozone and the temperature perturba
tions, extracted from ozonesonde and temperature data, up to the middle str
atosphere. Some case studies are presented to identify the nature of short-
scale structures with 1- to 5-km vertical wavelengths in the troposphere an
d the stratosphere. A climatology of short-scale structures induced by grav
ity waves and the horizontal advection shows that short-scale structures ar
e mainly detected in the middle and upper troposphere and in the lower stra
tosphere. The weak value of the coefficient R(z) that links the ozone and t
emperature perturbations induced by gravity waves is a major limit to detec
ting such short-scale structures above 21-km altitude. Some structures with
vertical wavelengths ranging from 1 to 5 km are attributed to gravity wave
s produced by convection in summer and the subtropical jet in winter, or qu
asi-horizontal large-scale motions from both sides of the subtropical barri
er.