首页> 外文期刊>Journal of atmospheric and solar-terrestrial physics >Concerning the upper stratospheric gravity wave and mesospheric cloud relationship over Sondrestrom, Greenland
【24h】

Concerning the upper stratospheric gravity wave and mesospheric cloud relationship over Sondrestrom, Greenland

机译:关于格陵兰桑德斯特罗姆地区上层平流层重力波和中层云的关系

获取原文
获取原文并翻译 | 示例
           

摘要

Recent research has shown experimental evidence that upper stratospheric gravity waves observed over Sondrestrom, Greenland (67°N, 310°E) portray a relationship with overlaying mesospheric clouds. It is the purpose of this paper to update the data from these studies with additional observations and reinvestigate the recently proposed hypothesis that suggests an anti-correlation between upper stratospheric gravity wave activity and mesospheric cloud strength. Data collected with the molecular/aerosol lidar at the ARCtic LIdar TEchnology (ARCLITE) facility in Sondrestrom have provided a total of 37 mesospheric cloud and upper stratospheric gravity wave observations from 1995-2001 that lend additional support to this hypothesis. We find a -0.44 linear correlation between the upper stratospheric gravity wave activity and the observed mesospheric cloud brightness within the 95% confidence interval. Even after considering geophysical variability due to observational limits, the linear correlation between the two fields is still -0.35 and also within a 95% confidence interval. These results suggest that there is indeed a statistically significant negative correlation between the upper stratospheric gravity wave activity and the mesospheric clouds. We then present two case studies from July 2001 that indicate that the upper stratospheric gravity wave activity leads the corresponding onset of mesospheric cloud activity with a time lag of ~ 1-4 h. Five additional data sets from 2001, which are not included here, are consistent with these lag values. The results support recent arguments for upper stratospheric gravity wave activity being related to mesospheric cloud characteristics (1) through the associated vertical group velocity propagation, (2) through a phase delay of the gravity wave field, or (3) through a spurious relationship with other gravity waves generated from a related source spectrum. In an effort to show causality, a scenario is proposed that relates the two phenomena and explains the physical nature of the mesospheric cloud-stratospheric gravity wave relationship.
机译:最近的研究表明,实验证据表明,在格陵兰岛桑德斯特罗姆(67°N,310°E)上空观测到的高空平流层重力波与与覆盖的中层云有关。本文的目的是通过其他观察来更新这些研究的数据,并重新研究最近提出的假设,该假设表明平流层上方重力波活动与中层云强度之间存在反相关关系。在Sondrestrom的ARCtic LIdar技术(ARCLITE)设施使用分子/气溶胶激光雷达收集的数据提供了1995年至2001年的总共37个中层云和平流层上方重力波观测资料,为这一假设提供了进一步的支持。我们发现在95%置信区间内,平流层上层重力波活动与观测到的中层云亮度之间存在-0.44线性相关性。即使在考虑了由于观测极限引起的地球物理变化之后,两个场之间的线性相关性仍为-0.35,并且在95%的置信区间内。这些结果表明,高层平流层重力波活动与中层云之间确实存在统计学上显着的负相关。然后,我们从2001年7月开始进行两个案例研究,这些研究表明平流层上层重力波活动以〜1-4 h的时间滞后导致相应的中层云活动的开始。来自2001年的另外五个数据集(未在此处包括)与这些滞后值一致。结果支持最近的论证,即平流层上层重力波活动与中层云特征有关(1)通过相关的垂直群速度传播,(2)通过重力波场的相位延迟,或者(3)通过与从相关源光谱产生的其他重力波。为了显示因果关系,提出了一种将这两种现象联系起来并解释中层云与平流层重力波关系的物理性质的场景。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号