A global model of meteoric sodium

被引:91
作者
Marsh, Daniel R. [1 ]
Janches, Diego [2 ]
Feng, Wuhu [3 ]
Plane, John M. C. [3 ]
机构
[1] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
[2] NASA, Space Weather Lab, GSFC, Greenbelt, MD USA
[3] Univ Leeds, Sch Chem, Leeds LS2 9JT, W Yorkshire, England
基金
英国自然环境研究理事会; 美国国家科学基金会;
关键词
MESOSPHERIC NA LAYER; LARGE-APERTURE RADARS; INPUT FUNCTION; UPPER-ATMOSPHERE; HIGH-POWER; 40-DEGREES-N; CLIMATOLOGY; TEMPERATURE; CHEMISTRY; DYNAMICS;
D O I
10.1002/jgrd.50870
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A global model of sodium in the mesosphere and lower thermosphere has been developed within the framework of the National Center for Atmospheric Research's Whole Atmosphere Community Climate Model (WACCM). The standard fully interactive WACCM chemistry module has been augmented with a chemistry scheme that includes nine neutral and ionized sodium species. Meteoric ablation provides the source of sodium in the model and is represented as a combination of a meteoroid input function (MIF) and a parameterized ablation model. The MIF provides the seasonally and latitudinally varying meteoric flux which is modeled taking into consideration the astronomical origins of sporadic meteors and considers variations in particle entry angle, velocity, mass, and the differential ablation of the chemical constituents. WACCM simulations show large variations in the sodium constituents over time scales from days to months. Seasonality of sodium constituents is strongly affected by variations in the MIF and transport via the mean meridional wind. In particular, the summer to winter hemisphere flow leads to the highest sodium species concentrations and loss rates occurring over the winter pole. In the Northern Hemisphere, this winter maximum can be dramatically affected by stratospheric sudden warmings. Simulations of the January 2009 major warming event show that it caused a short-term decrease in the sodium column over the polar cap that was followed by a factor of 3 increase in the following weeks. Overall, the modeled distribution of atomic sodium in WACCM agrees well with both ground-based and satellite observations. Given the strong sensitivity of the sodium layer to dynamical motions, reproducing its variability provides a stringent test of global models and should help to constrain key atmospheric variables in this poorly sampled region of the atmosphere. Key Points The first global model of mesospheric sodium has been developed Model includes new description of the meteoroid input function Meridional winds and stratospheric sudden warnings affect the sodium column ©2013. American Geophysical Union. All Rights Reserved.
引用
收藏
页码:11442 / 11452
页数:11
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