The distinct difference between the numerical results and the experimental one at higher altitudes is due to anomalous heating of the F layer ionosphere.
更高高度上模拟结果和实验结果的偏差是由于模拟过程中没有考虑F层异常吸收的作用。
The distinct difference between the numerical results and the experimental one at higher altitudes is due to anomalous heating of the F layer ionosphere.
更高高度上模拟结果和实验结果的偏差是由于模拟过程中没有考虑F层异常吸收的作用。
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