Climate Change Data Portal
DOI | 10.1029/2020JD032495 |
The Role of Vertically and Obliquely Propagating Gravity Waves in Influencing the Polar Summer Mesosphere | |
Thurairajah B.; Cullens C.Y.; Siskind D.E.; Hervig M.E.; Bailey S.M. | |
发表日期 | 2020 |
ISSN | 2169897X |
卷号 | 125期号:9 |
英文摘要 | Using an 8-year (2007–2014) data set from two different limb-viewing instruments, we evaluate the relative roles of vertically versus obliquely propagating gravity waves (GWs) as sources of GWs in the polar summer mesosphere. Obliquely propagating waves are of interest because they are presumed to be generated by the summer monsoons. In the high-latitude upper mesosphere, the correlation coefficient between the time series of ice water content (IWC) and GW amplitude is 0.48, indicating that the observed GWs enhance polar mesospheric clouds (PMCs). For vertically propagating waves, the correlation coefficient between IWC and stratospheric/lower mesospheric (20–70 km) GW amplitude at the same high latitudes becomes more negative with increasing altitude. This change in correlation from negative in the lower mesosphere to positive at PMC altitudes suggests the presence of another source of GWs. The positive correlation coefficient between the time series of IWC and GW amplitude from 0–50°N, 20–90 km shows a slanted structure suggesting oblique propagation. This slanted structure is more robust in some seasons compared to others, and this interannual variability may be due to the latitudinal gradient of the mesospheric easterly jet where steeper gradients allow for low-latitude tropospheric GWs to be refracted to the high-latitude mesosphere more efficiently. Gravity-Wave Regional or Global Ray Tracer (GROGRAT) ray tracing simulations show that more GWs propagate obliquely compared to vertically propagating waves that reach PMC altitudes. For obliquely propagating waves, GROGRAT simulations indicate that nonorographic tropospheric GWs with faster phase speed (>20 m/s) and longer horizontal wavelength (>400 km) have a higher probability of reaching the polar summer mesosphere. ©2020. American Geophysical Union. All Rights Reserved. |
英文关键词 | gravity waves; oblique propagation; polar mesospheric clouds |
语种 | 英语 |
来源期刊 | Journal of Geophysical Research: Atmospheres
![]() |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/186027 |
作者单位 | Center for Space Science and Engineering Research, Bradley Department of Electrical and Computer Engineering, Virginia Tech, Blacksburg, VA, United States; Space Science Laboratory, University of California, Berkeley, CA, United States; Space Science Division, Naval Research Laboratory, Washington, DC, United States; GATS, Inc., Driggs, ID, United States |
推荐引用方式 GB/T 7714 | Thurairajah B.,Cullens C.Y.,Siskind D.E.,et al. The Role of Vertically and Obliquely Propagating Gravity Waves in Influencing the Polar Summer Mesosphere[J],2020,125(9). |
APA | Thurairajah B.,Cullens C.Y.,Siskind D.E.,Hervig M.E.,&Bailey S.M..(2020).The Role of Vertically and Obliquely Propagating Gravity Waves in Influencing the Polar Summer Mesosphere.Journal of Geophysical Research: Atmospheres,125(9). |
MLA | Thurairajah B.,et al."The Role of Vertically and Obliquely Propagating Gravity Waves in Influencing the Polar Summer Mesosphere".Journal of Geophysical Research: Atmospheres 125.9(2020). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。