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DOI10.5194/acp-19-9927-2019
Investigation of Arctic middle-atmospheric dynamics using 3 years of H2O and O3 measurements from microwave radiometers at Ny-Ålesund
Schranz F.; Tschanz B.; Rüfenacht R.; Hocke K.; Palm M.; Kämpfer N.
发表日期2019
ISSN16807316
起始页码9927
结束页码9947
卷号19期号:15
英文摘要We used 3 years of water vapour and ozone measurements to study the dynamics in the Arctic middle atmosphere. We investigated the descent of water vapour within the polar vortex, major and minor sudden stratospheric warmings and periodicities at Ny-Ålesund. The measurements were performed with the two ground-based microwave radiometers MIAWARA-C and GROMOS-C, which have been co-located at the AWIPEV research base at Ny-Ålesund, Svalbard (79° N, 12° E), since September 2015. Both instruments belong to the Network for the Detection of Atmospheric Composition Change (NDACC). The almost continuous datasets of water vapour and ozone are characterized by a high time resolution of the order of hours. A thorough intercomparison of these datasets with models and measurements from satellite, ground-based and in situ instruments was performed. In the upper stratosphere and lower mesosphere the MIAWARA-C water vapour profiles agree within 5% with SD-WACCM simulations and ACEFTS measurements on average, whereas AuraMLS measurements show an average offset of 10 %-15% depending on altitude but constant in time. Stratospheric GROMOS-C ozone profiles are on average within 6% of the SD-WACCM model, the AuraMLS and ACE-FTS satellite instruments and the OZORAM ground-based microwave radiometer which is also located at Ny-Ålesund. During these first 3 years of the measurement campaign typical phenomena of the Arctic middle atmosphere took place, and we analysed their signatures in the water vapour and ozone measurements. Two major sudden stratospheric warmings (SSWs) took place in March 2016 and February 2018 and three minor warmings were observed in early 2017. Ozone-rich air was brought to the pole and during the major warmings ozone enhancements of up to 4 ppm were observed. The reversals of the zonal wind accompanying a major SSW were captured in the GROMOS-C wind profiles which are retrieved from the ozone spectra. After the SSW in February 2018 the polar vortex re-established and the water vapour descent rate in the mesosphere was 355 md-1. Inside of the polar vortex in autumn we found the descent rate of mesospheric water vapour from MIAWARA-C to be 435 md-1 on average. We find that the water vapour descent rate from SD-WACCM and the vertical velocity w̄∗ of the residual mean meridional circulation from SD-WACCM are substantially higher than the descent rates of MIAWARA-C. w̄∗ and the zonal mean water vapour descent rate from SD-WACCM agree within 10% after the SSW, whereas in autumn w̄∗ is up to 40 % higher. We further present an overview of the periodicities in the water vapour and ozone measurements and analysed seasonal and interannual differences. © Author(s) 2019.
语种英语
scopus关键词atmospheric chemistry; atmospheric dynamics; microwave radiometer; middle atmosphere; ozone; polar vortex; sudden stratospheric warming; water vapor; Arctic; Ny-Alesund; Spitsbergen; Svalbard; Svalbard and Jan Mayen
来源期刊Atmospheric Chemistry and Physics
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/144229
作者单位Institute of Applied Physics, University of Bern, Bern, Switzerland; Institute of Environmental Physics, University of Bremen, Bremen, Germany; Federal Office for Meteorology and Climate MeteoSwiss, Payerne, Switzerland
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Schranz F.,Tschanz B.,Rüfenacht R.,et al. Investigation of Arctic middle-atmospheric dynamics using 3 years of H2O and O3 measurements from microwave radiometers at Ny-Ålesund[J],2019,19(15).
APA Schranz F.,Tschanz B.,Rüfenacht R.,Hocke K.,Palm M.,&Kämpfer N..(2019).Investigation of Arctic middle-atmospheric dynamics using 3 years of H2O and O3 measurements from microwave radiometers at Ny-Ålesund.Atmospheric Chemistry and Physics,19(15).
MLA Schranz F.,et al."Investigation of Arctic middle-atmospheric dynamics using 3 years of H2O and O3 measurements from microwave radiometers at Ny-Ålesund".Atmospheric Chemistry and Physics 19.15(2019).
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