On seasonality of stratomesospheric CO above midlatitudes: new insight from solar FTIR spectrometry at Zugspitze and Garmisch

  • A significant seasonality in stratomesospheric CO (24–100 km) above mid-latitudes is derived from FTIR via a new regularization scheme. Half hourly means from the Zugspitze (47.42°N, 10.98°E, 2964 m a.s.l.) and nearby Garmisch (745 m a.s.l.) measurements show excellent agreement (R = 0.94, slope 0.91, standard deviation 12%). Mean seasonality of the Zugspitze series (1999–2008) shows a November–April enhancement (February maximum 3.63 × 1016 cm−2) and a summer background (1.64 × 1016 cm−2) which agrees with the WACCM model. Measured monthly means reveal a year-to-year variability of up to 32% (1-sigma) in winter not reproduced by WACCM (R = −0.13). Frequency distributions of daily means are right skewed in winter due to enhancements by vortex air transport (1–3 days duration) which typically reflect CO levels of the vortex border and may even reach vortex-center levels (≈300% of the multi-annual monthly median).

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Metadaten
Author:Tobias Borsdorff, Ralf SussmannORCiDGND
Frontdoor URLhttps://opus.bibliothek.uni-augsburg.de/opus4/120740
ISSN:0094-8276OPAC
ISSN:1944-8007OPAC
Parent Title (English):Geophysical Research Letters: Atmospheric Science
Publisher:Wiley
Place of publication:Hoboken, NJ
Type:Article
Language:English
Year of first Publication:2009
Release Date:2025/03/31
Volume:36
Issue:21
First Page:L21804
DOI:https://doi.org/10.1029/2009gl040056
Institutes:Fakultät für Angewandte Informatik
Fakultät für Angewandte Informatik / Institut für Geographie
Fakultät für Angewandte Informatik / Institut für Geographie / Lehrstuhl für Physische Geographie mit Schwerpunkt Klimaforschung
Dewey Decimal Classification:5 Naturwissenschaften und Mathematik / 55 Geowissenschaften, Geologie / 550 Geowissenschaften