Cover Journal of the Atmospheric Sciences
Journal of the Atmospheric Sciences

 

Volume 51 (1994): Issue 20 (Oct 1994)

Print ISSN:
0022-4928
Online ISSN:
1520-0469
Cover Journal of the Atmospheric Sciences
EDITORIAL
EDITORIAL
ARTICLES
Dynamical Evolution of the Northern Stratosphere in Early Winter 1991/92, as Observed by the Improved Stratospheric and Mesospheric Sounder
Evolution of the Stratosphere during Northern Winter 1991/92 as Diagnosed from U.K. Meteorological Office Analyses
Measurements of N2O by the UARS Improved Stratospheric and Mesospheric Sounder during the Early Northern Winter 1991/92
Simulation of Stratospheric N2O in the NCAR CCM2: Comparison with CLAES Data and Global Budget Analyses
Global Ozone Observations from the UARS MLS: An Overview of Zonal-Mean Results
Large-Scale Variations in Ozone from the First Two Years of UARS MLS Data
Observations of Lower-Stratospheric CIONO2, HNO3, and Aerosol by the UARS CLAES Experiment between January 1992 and April 1993
Summer Polar Chemistry Observations in the Stratosphere Made by HALOE
Three-Dimensional Evolution of Water Vapor Distributions in the Northern Hemisphere Stratosphere as Observed by the MLS
Spring Dehydration in the Antarctic Stratospheric Vortex Observed by HALOE
Synoptic Interpretation of Measurements from HALOE
Mixing Processes within the Polar Night Jet
On the Motion of Air through the Stratospheric Polar Vortex
High-Resolution Stratospheric Tracer Fields Estimated from Satellite Observations Using Lagrangian Trajectory Calculations
Isentropic Mass Exchange between the Tropics and Extratropics in the Stratosphere
Properties of Northern Hemisphere Polar Stratospheric Clouds and Volcanic Aerosol in 1991/92 from UARS/ISAMS Satellite Measurements
Spectral Signatures of Polar Stratospheric Clouds and Sulfate Aerosol
The Tropical Semiannual Oscillations in Temperature and Ozone as Observed by the MLS
Equatorial Kelvin Waves: A UARS MLS View
Observations of the Diurnal Tide from Space
An Estimate of the Momentum Deposition in the Lower Thermosphere by the Observed Diurnal Tide
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