scholarly journals Odin/SMR limb observations of stratospheric trace gases: Level 2 processing of ClO, N2O, HNO3, and O3

2005 ◽  
Vol 110 (D14) ◽  
pp. n/a-n/a ◽  
Author(s):  
J. Urban ◽  
N. Lautié ◽  
E. Le Flochmoën ◽  
C. Jiménez ◽  
P. Eriksson ◽  
...  
Keyword(s):  
Trace Gases ◽  
Level 2 ◽  
Stratospheric Trace Gases

Development of a new methodology for the retrieval of in-situ stratospheric trace gases concentration from airborne limb-absorption measurements

2002 ◽  
Author(s):  
Andrea Petritoli ◽  
Giorgio Giovanelli ◽  
Fabrizio Ravegnani ◽  
Daniele Bortoli ◽  
Ivan K. Kostadinov ◽  
...  
Keyword(s):  
Trace Gases ◽  
Stratospheric Trace Gases ◽  
Absorption Measurements

A cryogenically operated laser diode spectrometer for airborne measurement of stratospheric trace gases

2008 ◽  
Vol 90 (3-4) ◽  
pp. 581-592 ◽  
Author(s):  
S. Viciani ◽  
F. D’Amato ◽  
P. Mazzinghi ◽  
F. Castagnoli ◽  
G. Toci ◽  
...  
Keyword(s):  
Laser Diode ◽  
Trace Gases ◽  
Airborne Measurement ◽  
Stratospheric Trace Gases

Revisiting the factors that drive interannual variability in stratospheric entry water vapour

2020 ◽  
Author(s):  
Shlomi Ziskin Ziv ◽  
Chaim I. Garfinkel
Keyword(s):  
Water Vapor ◽  
Interannual Variability ◽  
Large Scale ◽  
Trace Gases ◽  
Transport Processes ◽  
Tropospheric Temperature ◽  
Stratospheric Water Vapor ◽  
Cold Point ◽  
Stratospheric Trace Gases

<p>Understanding the sinks, sources and transport processes of stratospheric trace gases can improve our prediction of mid to long term climate change. In this study we consider the processes that lead to variability in stratospheric water vapor. We perform a Multiple Linear Regression(MLR) on the SWOOSH combined anomaly filled water vapor product with ENSO, QBO, BDC, mid-tropospheric temperature, and CH4 as predictors, in an attempt to find the factors that most succinctly explain observed water vapor variability. We also consider the fraction of entry water vapor variability that can be accounted for by variations of the cold point temperature as an upper bound on how much water vapor variability is predictable from large scale processes. Several periods in which the MLR fails to account for interannual variability are treated as case studies in order to better understand variability in entry water not governed by these large scale processes.</p>

Interannual variability of stratospheric trace gases: The role of extratropical wave driving

2004 ◽  
Vol 130 (602) ◽  
pp. 2459-2474 ◽  
Author(s):  
J. Ma ◽  
D.W. Waugh ◽  
A.R. Douglass ◽  
S.R. Kawa ◽  
P.A. Newman ◽  
...  
Keyword(s):  
Interannual Variability ◽  
Trace Gases ◽  
Stratospheric Trace Gases
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