Climatological study of the ion temperature in the ionosphere as recorded by Millstone Hill incoherent scatter radar and comparison with the IRI model

Author(s):  
Alessio Pignalberi ◽  
Kateryna D. Aksonova ◽  
Shun-Rong Zhang ◽  
Vladimir Truhlik ◽  
Padma Gurram ◽  
...  
2017 ◽  
Vol 60 (2) ◽  
pp. 452-460 ◽  
Author(s):  
K.G. Ratovsky ◽  
A.V. Dmitriev ◽  
A.V. Suvorova ◽  
A.A. Shcherbakov ◽  
S.S. Alsatkin ◽  
...  

Author(s):  
Christiano Garnett Marques Brum ◽  
Fabiano da Silveira Rodrigues ◽  
Pedrina Terra dos Santos ◽  
Aleshka Carrion Matta ◽  
Nestor Aponte ◽  
...  

2004 ◽  
Vol 22 (3) ◽  
pp. 863-876 ◽  
Author(s):  
E. M. Griffin ◽  
A. Aruliah ◽  
I. C. F. Müller-Wodarg ◽  
A. Aylward

Abstract. The climatological behaviour of the thermospheric meridional wind above Kiruna, Sweden (67.4°N, 20.4°E) has been investigated for seasonal and solar cycle dependence using six different techniques, comprising both model and experimental sources. Model output from both the empirical Horizontal Wind Model (HWM) (Hedin et al., 1988) and the numerical Coupled Thermosphere and Ionosphere Model (CTIM) are compared to the measured behaviour at Kiruna, as a single site example. The empirical International Reference Ionosphere (IRI) model is used as input to an implementation of servo theory, to provide another climatology combining empirical input with a theoretical framework. The experimental techniques have been introduced in a companion paper in this issue and provide climatologies from direct measurements, using Fabry-Perot Interferometers (FPI), together with 2 separate techniques applied to the European Incoherent Scatter radar (EISCAT) database to derive neutral winds. One of these techniques uses the same implementation of servo theory as has been used with the IRI model. Detailed comparisons for each season and solar activity category allow for conclusions to be drawn as to the major influences on the climatological behaviour of the wind at this latitude. Comparison of the incoherent scatter radar (ISR) derived neutral winds with FPI, empirical model and numerical model winds is important to our understanding and judgement of the validity of the techniques used to derive thermospheric wind databases. The comparisons also test model performance and indicate possible reasons for differences found between the models. In turn, the conclusions point to possible improvements in their formulation. In particular it is found that the empirical models are over-reliant on mid-latitude data in their formulation, and fail to provide accurate estimates of the winds at high-latitudes. Key words. Meteorology and atmospheric dynamics (thermospheric dynamics), Ionosphere (ionosphere-atmosphere interactions, auroral ionosphere)


2004 ◽  
Vol 22 (10) ◽  
pp. 3523-3529 ◽  
Author(s):  
C. J. Davis ◽  
I. W. McCrea

Abstract. The variation of parameters in time series data from the EISCAT UHF incoherent scatter radar has been used to estimate the uncertainties in measurements of electron concentration, electron and ion temperature and line-of-sight ion velocity. Good agreement was found with the results of previous analyses that estimated uncertainties in velocity and electron temperature from similar data using a complementary method. By contrast, uncertainties in ion temperature and electron concentration estimated from the same time series data were found to differ from the expected theoretical values by factors of 1.8 and 2.7, respectively. It was found that the relative sizes of these uncertainties more closely matched those predicted by a previous Monte Carlo simulation than values predicted by currently accepted theoretical formulae. Although the specific measured and theoretical uncertainties reported here relate to a very simple kind of ISR experiment, the method itself is general and can be applied to data from any incoherent scatter radar.


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