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In this article, we present detailed seasonal, monthly and daily statistics of temperature difference in the surface layer at Muztagh-ata site based on the temperature measurements at two heights of 2 m and 6 m. We find that the temperature inversion occurs frequently at our site during nighttime especially in cold season. Strong Temperature inversion always represents stable atmospheric turbulence, which is crucial for optical observatory. By analyzing the behavior of temperature inversion and its correlation with wind and cloud amount, one conclusion can be made that radiation inversion is main reason for the existence of temperature inversion in the surface-layer at Muztagh-ata site.

Site-testing at Muztagh-ata site III: temperature inversion in surface-layer atmosphere