skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Mean winds and momemtum fluxes over Jicamarca, Peru, during June and August 1987

Journal Article · · Journal of the Atmospheric Sciences; (United States)
;  [1];  [2];  [3]; ;  [4]
  1. Univ. of Wisconsin, Madison (United States)
  2. Univ. of Colorado, Boulder (United States)
  3. Saint Louis Univ., MO (United States)
  4. Univ. of Illinois, Champaign (United States)

Data from the mesophere-stratosphere-troposphere (MST) radar at Jicamarca, Peru, together with other available data, are used to diagnose the mean structure of winds and gravity-wave momentum fluxes from the surface to 90 km during two ten-day campaigns in June and August of 1987. In the stratosphere a layer of maximum eastward flow associated with the quasi-biennial oscillation (QBO) was seen to strengthen and descend rapidly from June to August, overlying persitent westward flow. A layer of enhanced signal return, suggestive of a turbulent layer, was observed just above the descending QBO eastward maximum. Notable zonal asymmetries were present during this transition and the local meridional circulation departed form zonal-mean QBO theory. A substantial northeastward momentum flux was found below 25 km, which may be related to topographic gravity waves excited by southeastward flow across the Andes. In the lower mesosphere a relatively weak second mesopause semiannual oxcillation is confirmed. Gravity-wave zonal and meridional momentum fluxes usually opposed the flow, yielding body forces of [approximately]10-100 ms[sup [minus]1] day [sup [minus]1]. In both the lower stratosphere and mesosphere, body forces were comparable in magnitude to inferred Coriolis torques. 52 refs., 9 figs.

OSTI ID:
6721223
Journal Information:
Journal of the Atmospheric Sciences; (United States), Vol. 49:24; ISSN 0022-4928
Country of Publication:
United States
Language:
English