通过具体的数值计算结果和理论分析，研究了水云的异常吸收现象。
A detailed theoretical analysis of the numerical results is presented, which explains the phenomenon of cloud absorption anomaly.
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.
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