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Table 3 RMS deviation of TECiri from TECgps, in TECU, at the main phase of the ionospheric storms at solar maximum (2000) and solar minimum (2006). Results of IRI-Plas model for two options: (1) ionosonde-derived inputof foF2 and hmF2 combined with input of TECgps, (2) input of foF2 and hmF2 from ionosonde alone. Instantaneous results (i) and monthly median results (m) are shown. Data are missing for two stations for 2000.

From: Inter-hemispheric imaging of the ionosphere with the upgraded IRI-Plas model during the space weather storms

Station

2000

2006

RMS(1)i

RMS(2)i

RMS(1)m

RMS(2)m

RMS(1)i

RMS(2)i

RMS(1)m

RMS(2)m

Magadan

0.68

2.54

0.34

1.32

0.13

1.16

0.10

0.76

Wakkanai

1.26

2.57

0.50

1.96

0.19

1.12

0.18

1.36

Kokubunji

0.80

2.38

0.22

1.10

0.24

1.43

0.17

1.41

Yamagawa

—

—

—

—

0.70

2.60

0.29

2.07

Okinawa

1.92

5.31

0.37

1.83

0.25

2.40

0.18

1.48

Kwajalein

—

—

—

—

0.75

3.86

0.53

2.74

Darwin

1.51

3.87

1.42

2.44

0.42

3.75

0.13

0.97

Hobart

0.48

1.56

0.17

0.79

0.36

0.97

0.03

0.28