1979—2100年青藏高原夏季大气0 ℃层高度变化分析
张怡(
), 段克勤(), 石培宏
), 段克勤(), 石培宏
Analysis of the 0 ℃ level height variation over the Qinghai-Tibet Plateau in summer from 1979 to 2100
Yi ZHANG(), Keqin DUAN(), Peihong SHI
), Keqin DUAN(), Peihong SHI
图6. 青藏高原夏季地面温度气候倾向率空间分布（a）以及大气0 ℃层高度和地面温度年际变化曲线（b），红点表示通过了信度为0.01的显著性检验，黑点表示通过了信度为0.05的显著性检验
Fig.6. Spatial distribution of climate tendency rate of summer near-surface air temperature （a） and interannual variation curves of the 0 ℃ level height and near-surface air temperature （b） over the Qinghai-Tibet Plateau， the red dot indicates that it has passed the significance test with the reliability of 0.01， and the black dot indicates that it has passed the significance test with the reliability of 0.05
