TTL cooling and drying during the January 2013 stratospheric sudden warming

• Published in: Quarterly journal of the Royal Meteorological Society Vol. 141; no. 693; pp. 3030 - 3039
• Main Authors: Evan, Stephanie, Rosenlof, K. H., Thornberry, Troy, Rollins, Andrew, Khaykin, Sergey
• Format: Journal Article
• Language: English
• Published: Chichester, UK John Wiley & Sons, Ltd 01.10.2015; Wiley Subscription Services, Inc; Wiley
• Subjects: Atmospheric and Oceanic Physics; Climatology; Convective activity; Cooling; Cyclones; Dehydration; Deployment; Drying; Earth Sciences; Environmental Sciences; Global Changes; In situ measurement; Lower stratosphere; Physics; Polar temperatures; Quasi-biennial oscillation; Satellite data; Satellites; Sciences of the Universe; Stratosphere; Stratospheric warming; sudden stratospheric warming; Temperature; Tropical climate; Tropical tropopause; Tropopause; Troposphere; TTL; Upper troposphere; Water temperature; Water vapor; Water vapour; sudden stratospheric warming; TTL; water vapour
• ISSN: 0035-9009; 1477-870X
• DOI: 10.1002/qj.2587

Extremely low water vapour concentrations (as low as 1.5 ppmv) in the tropical tropopause layer (TTL) were observed by in situ measurements during the Airborne Tropical TRopopause Experiment (ATTREX) winter 2013 deployment in February 2013. The January 2013 tropical (15°N–15°S) mean value of Microwave Limb Sounder (MLS) water vapour satellite data at 82 hPa (2.3 ppmv) was one of the lowest during the instrument record (2004–2013). The relationship between a cooling of the tropical tropopause, a sudden stratospheric warming (SSW) event and convective activity in the western Pacific is investigated using satellite data and reanalysis meteorological products to elucidate the likely origin of those extremely low water vapour concentrations. A major midwinter SSW developed on 6 January 2013. Stratospheric polar temperatures increased by ∼30 K in a matter of days and temperatures in the tropical upper troposphere and lower stratosphere (UTLS) dropped at the same time. As a result of the easterly shear phase of the Quasi‐Biennial Oscillation and the SSW, the tropical tropopause in January 2013 was anomalously cold (zonal mean of 187 K) and elevated (85 hPa). The tropical cold point tropopause (CPT) temperature and water vapour concentration at 82 hPa decreased by about 2 K and 1.5 ppmv respectively within the first 15 days of January; the water vapour change was likely a result of dehydration associated with the rapid cooling of the tropical CPT during that period.