At Wakkanai, IRI-predicted foF2 agrees with observations, but the proposed BMUF correction for high solar activity is an in-sample fit with no out-of-sample validation.
Ionospheric data from the ionosonde stations such as Wakkanai station can be used to monitor this environment by observing Mid- latitude propagation conditions
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Using High Frequency Propagation to Calculate Basic Maximum Usable Frequency
At Wakkanai, IRI-predicted foF2 agrees with observations, but the proposed BMUF correction for high solar activity is an in-sample fit with no out-of-sample validation.