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DOI10.5194/acp-19-955-2019
Comparison of Antarctic polar stratospheric cloud observations by ground-based and space-borne lidar and relevance for chemistry-climate models
Snels M.; Scoccione A.; Di Liberto L.; Colao F.; Pitts M.; Poole L.; Deshler T.; Cairo F.; Cagnazzo C.; Fierli F.
发表日期2019
ISSN16807316
起始页码955
结束页码972
卷号19期号:2
英文摘要A comparison of polar stratospheric cloud (PSC) occurrence from 2006 to 2010 is presented, as observed from the ground-based lidar station at McMurdo (Antarctica) and by the satellite-borne CALIOP lidar (Cloud-Aerosol Lidar with Orthogonal Polarization) measuring over McMurdo. McMurdo (Antarctica) is one of the primary lidar stations for aerosol measurements of the NDACC (Network for Detection of Atmospheric Climate Change). The ground-based observations have been classified with an algorithm derived from the recent v2 detection and classification scheme, used to classify PSCs observed by CALIOP. A statistical approach has been used to compare groundbased and satellite-based observations, since point-to-point comparison is often troublesome due to the intrinsic differences in the observation geometries and the imperfect overlap of the observed areas. A comparison of space-borne lidar observations and a selection of simulations obtained from chemistry-climate models (CCMs) has been made by using a series of quantitative diagnostics based on the statistical occurrence of different PSC types. The distribution of PSCs over Antarctica, calculated by several CCMVal-2 and CCMI chemistry-climate models has been compared with the PSC coverage observed by the satellite-borne CALIOP lidar. The use of several diagnostic tools, including the temperature dependence of the PSC occurrences, evidences the merits and flaws of the different models. The diagnostic methods have been defined to overcome (at least partially) the possible differences due to the resolution of the models and to identify differences due to microphysics (e.g., the dependence of PSC occurrence on T -TNAT). A significant temperature bias of most models has been observed, as well as a limited ability to reproduce the longitudinal variations in PSC occurrences observed by CALIOP. In particular, a strong temperature bias has been observed in CCMVal-2 models with a strong impact on PSC formation. The WACCM-CCMI (Whole Atmosphere Community Climate Model - Chemistry-Climate Model Initiative) model compares rather well with the CALIOP observations, although a temperature bias is still present. © Author(s) 2019.
语种英语
scopus关键词aerosol; algorithm; CALIOP; climate modeling; comparative study; lidar; satellite data; stratosphere; Antarctica; East Antarctica; McMurdo Station
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/144696
作者单位Istituto di Scienze dell'Atmosfera e Del Clima, Via Fosso del Cavaliere 100, Rome, 00133, Italy; ENEA, Via Enrico Fermi 45, Frascati, 00044, Italy; NASA Langley Research Center, Hampton, VA 23681, United States; Science Systems and Applications Inc., Hampton, VA 23666, United States; Dept. of Atmospheric Science, University of Wyoming, Laramie, WY 82071, United States
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GB/T 7714
Snels M.,Scoccione A.,Di Liberto L.,et al. Comparison of Antarctic polar stratospheric cloud observations by ground-based and space-borne lidar and relevance for chemistry-climate models[J],2019,19(2).
APA Snels M..,Scoccione A..,Di Liberto L..,Colao F..,Pitts M..,...&Fierli F..(2019).Comparison of Antarctic polar stratospheric cloud observations by ground-based and space-borne lidar and relevance for chemistry-climate models.Atmospheric Chemistry and Physics,19(2).
MLA Snels M.,et al."Comparison of Antarctic polar stratospheric cloud observations by ground-based and space-borne lidar and relevance for chemistry-climate models".Atmospheric Chemistry and Physics 19.2(2019).
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