Comparison of GPS-TEC measurements with IRI-2007 and IRI-2012 modeled TEC at an equatorial latitude station, Bangkok, Thailand

被引:16
|
作者
Arunpold, Sanit [1 ]
Tripathi, Nitin K. [1 ]
Chowdhary, V. Rajesh [1 ]
Raju, Durairaju Kumaran [2 ]
机构
[1] Asian Inst Technol, Sch Engn & Technol, RS&GIS Field Study, Klong Laung 12120, Pathumthani, Thailand
[2] Natl Univ Singapore, Trop Marine Sci Inst, Singapore 119227, Singapore
关键词
GPS-TEC; IRI-2007; IRI-2012; GPS SCINDA; TOTAL ELECTRON-CONTENT; PREDICTIONS; NETWORK; VARIABILITY; IONOSPHERE; SATELLITE; REGION;
D O I
10.1016/j.jastp.2014.06.001
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
This paper presents the first vertical total electron content (VTEC) data derived from a dual-frequency GPS receiver installed at the Asian Institute of Technology in Bangkok, as part of project SCINDA (Scintillation Network and Decision Aid) with a magnetic dip latitude of 14 degrees N, The diurnal, monthly, and seasonal variation in TEC, measured between August 2010 and July 2012, was compared with values derived from two International Reference Ionosphere (IRI) models: the IRI-2007 and the recently released IRI-2012. The highest diurnal TEC always occurred between 08:00 and 12:00 Universal Time (UT). The diurnal pattern of GPS-TEC reached its maximum values during equinoctial months (March, April, September, and October) and minimum values during solstice months (June, July, December, and January), which can be attributed to the solar extreme ultra-violet ionization coupled with the upward vertical E x B drift. The modeled TEC was underestimated in 2010 and 2011 and overestimated in 2012, especially with the IRI-2007 model. The measured values were better correlated with the IRI-2012 model, especially in 2012. However, neither of the IRI models responded to geomagnetic activity, despite the selection of the "storm" option, generally showing a smooth curve and underestimating TEC during a storm. To verify this phenomenon, the impacts of geomagnetic storms were considered. (C) 2014 Elsevier Ltd. All rights reserved.
引用
收藏
页码:88 / 94
页数:7
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