Differences between ICM and UNNOFIT inversions of THEMIS/MTR data for an ICM with an average model atmosphere.
|Vect. mag. field (G)||ϵ(G)||σ(G)|
|0 < B < 500||–32||42|
|500 < B < 1000||–28||101|
|1000 < B < 1500||–17||189|
|1500 < B < 2000||–2||190|
|2000 < B < 2500||–77||175|
Notes. Same caption as in Table 3.
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