Parallel Comparison of Major Sudden Stratospheric Warming Events in CESM1-WACCM and CESM2-WACCM

التفاصيل البيبلوغرافية
العنوان: Parallel Comparison of Major Sudden Stratospheric Warming Events in CESM1-WACCM and CESM2-WACCM
المؤلفون: Can Cao, Jian Rao, Si-Ming Liu, Mu-Han Ma, Yao-bin Wang, Yuan-Hao Chen, Si-Yu Li
المصدر: Atmosphere
Volume 10
Issue 11
Atmosphere, Vol 10, Iss 11, p 679 (2019)
بيانات النشر: Multidisciplinary Digital Publishing Institute, 2019.
سنة النشر: 2019
مصطلحات موضوعية: Atmospheric Science, Geopotential height, CESM1-WACCM, vortex split, lcsh:QC851-999, Environmental Science (miscellaneous), Sudden stratospheric warming, Vortex, Troposphere, Atmosphere, CESM2-WACCM, Polar vortex, Climatology, Polar, lcsh:Meteorology. Climatology, Climate model, vortex displacement, Geology
الوصف: After the recent release of the historical runs by community Earth system model version 2&ndash
the whole atmosphere community climate model (CESM2-WACCM), the major sudden stratospheric warming (SSW) events in this model and in its previous version (CESM1-WACCM) are compared based on a modern reanalysis (JRA55). Using the World Meteorological Organization (WMO) definition of SSWs and a threshold-based classification method that can describe the polar vortex morphology, SSWs in models and the reanalysis are further classified into two types, vortex displacement SSWs and vortex split SSWs. The general statistical characteristics of the two types of SSW events in the two model versions are evaluated. Both CESM1-WACCM and CESM2-WACCM models are shown to reproduce the SSW frequency successfully, although the circulations differences between vortex displacement SSWs and vortex split SSWs in CESM2-WACCM are smaller than in CESM1-WACCM. Composite polar temperature, geopotential height, wind, and eddy heat flux anomalies in both the two models and the reanalysis show similar evolutions. In addition, positive Pacific&ndash
North America and negative Western Pacific patterns in the troposphere preceding vortex displacement and split SSWs are observed in both observations and the models. The strong negative North Atlantic oscillation-like pattern, especially after vortex split SSW onset, is also identified in models. The near-surface cold Eurasia&ndash
warm North America pattern before both types of SSW onset, the warm Eurasia&ndash
cold North America pattern after displacement SSW onset, and the cold Eurasia&ndash
cold North America pattern after split SSW onset are consistently identified in JRA55, CESM1-WACCM, and CESM2-WACCM, although the temperature anomalies after the split SSW onset in CESM2-WACCM are somewhat underestimated.
وصف الملف: application/pdf
اللغة: English
تدمد: 2073-4433
DOI: 10.3390/atmos10110679
URL الوصول: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4f19c8199e889efc0c585b0c910849b5
حقوق: OPEN
رقم الأكسشن: edsair.doi.dedup.....4f19c8199e889efc0c585b0c910849b5
قاعدة البيانات: OpenAIRE
الوصف
تدمد:20734433
DOI:10.3390/atmos10110679