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solar cycle effects on gnss-derived ionospheric total electron content ...

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where it is evident that the 2nd and the 4th terms are functi<strong>on</strong>s of the maximum electr<strong>on</strong> density andfrequency, whereas the 3rd and 5th are a functi<strong>on</strong> of the maximum electr<strong>on</strong> density, the Earth `smagnetic field strength and the frequency. However, Komjathy (1997) showed that the c<strong>on</strong>tributi<strong>on</strong>of the 3rd, 4th and 5th terms to the error budget of the determinati<strong>on</strong> of the refractive index are 3, 5,and 6 orders of magnitude less than the sec<strong>on</strong>d term when assuming Θ = 0, and the typical values12 -3for F2 layer maximum electr<strong>on</strong> density ( N = 10 m ) and typical value for the Earth’s magnetic−5 -2field strength ( B 0= 5.0× 10 Wb.m ) respectively.When both collisi<strong>on</strong>s and the magnetic field are negligible, <strong>on</strong>ly the 1st and 2nd terms in equati<strong>on</strong>(2.7) are c<strong>on</strong>sidered. However, to enable calculating the phase refractive index of the i<strong>on</strong>osphere,appropriate for the carrier phase observati<strong>on</strong>s, we obtain:2.6.2 Group refractive indexAccording to Langley (1996), the group refractive index is defined as:nϕ40.3⋅N≅ 1 − .(2.8)2fdn= + . (2.9)ngn f dfBy invoking the value of phase refractive index n= n ϕin equati<strong>on</strong> (2.8),dn dn g d ⎛ 40.3⋅N ⎞= = ⎜1 − ,2 ⎟df df df ⎝ f ⎠d ⎛ 1 ⎞40.3 N , df ⎝ f ⎠= − ⋅ ⎜ 2 ⎟and therefore the equati<strong>on</strong> (2.9) takes the form:⎛ 1 ⎞2( 40.3 ) ,⎝ f ⎠= − ⋅ N ⎜ 3 ⎟(2.10)33

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