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Temperature deviations in the midlatitude mesosphere during STRATOSPHERIC WARMINGS AS MEASURED WITH RAYLEIGH-SCATTER LIDAR

机译:利用瑞利散射延雷达测量的平流层升温期间中间态圈温度偏差

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While mesospheric temperature anomalies associated with Sudden Stratospheric Warmings (SSWs) have been observed extensively in the polar regions, observations of these anomalies at midlatitudes are sparse. The original Rayleigh-scatter lidar that operated at the Atmospheric Lidar Observatory (ALO; 41.7°N, 111.8°W) in the Center for Atmospheric and Space Sciences (CASS) on the campus of Utah State University (USU) collected an extensive set of temperature data for 11 years in the 45-90 km altitude range. This work focuses on the extensive Rayleigh lidar observations made during six major SSW events that occurred between 1993 and 2004, providing a climatological study of the midlatitude mesospheric temperatures during these SSW events. An overall disturbance pattern was observed in the mesospheric temperatures during these SSWs. It included coolings in the upper mesosphere, comparable to those seen in the polar regions during SSW events, and warmings in the lower mesosphere.
机译:虽然已经在极地区域广泛观察到与突然平流层升温(SSW)相关联的伴随着突然平流层升温(SSW)的异常,但在中间瘤的这些异常的观察是稀疏的。在犹他州大学校园(USU)的大气和空间科学中心(ALO; 41.7°N,111.8°W)的原始瑞利散散雷达(ALO; 41.7°N,111.8°W)收集了一套广泛的温度数据在45-90公里的高度范围内11年。这项工作侧重于1993年至2004年期间发生的六个主要SSW事件中的广泛瑞利激光雷达观测,在这些SSW事件中提供了对中美态化器温度的气候研究。在这些SSW中的MeSospheric温度下观察到整体扰动模式。它包括上部介质层中的冷却,与SSW事件中的极地区域中看到的那些相当,以及较低介质层的暖温。

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