DOI: 10.1002/jgrd.50761
论文题名: A modeling assessment of the origin of Beryllium-7 and Ozone in the Canadian Rocky Mountains
作者: D'Amours R. ; Mintz R. ; Mooney C. ; Wiens B.J.
刊名: Journal of Geophysical Research Atmospheres
ISSN: 21698996
出版年: 2013
卷: 118, 期: 17 起始页码: 10125
结束页码: 10138
语种: 英语
英文关键词: 7Be transport
; dispersion modeling
; inverse Lagrangian modeling
; stratospheric exchanges
Scopus关键词: Beryllium
; Boundary layers
; Dispersions
; Inverse problems
; Lagrange multipliers
; Troposphere
; 7Be transport
; Boundary layer air
; Dispersion modeling
; Inverse modeling
; Lagrangian dispersion model
; Lagrangian models
; Surface observation
; Upper troposphere
; Ozone
; air mass
; assessment method
; atmospheric modeling
; atmospheric pollution
; atmospheric transport
; beryllium isotope
; boundary layer
; concentration (composition)
; data set
; dispersion
; numerical model
; observational method
; ozone
; relative humidity
; stratosphere
; troposphere
; Pacific Ocean
; Rocky Mountains
英文摘要: This paper seeks to investigate the extent to which stratosphere-to- troposphere transport (STT) impacts the Canadian Rocky Mountain foothills. Beryllium-7 (7Be) was monitored weekly at Harlech, Alberta, from July 2003 to June 2004, and daily during the spring of 2004. These data, together with hourly ozone (O3 ) and relative humidity (RH) measurements, are presented and analyzed, with a focus on the spring of 2004. A Lagrangian dispersion model was used to help determine the origin of air parcels arriving at Harlech in order to assess if these periods were related to well-defined stratospheric intrusions. The modeling results show that events consisting of above average surface observations of 7Be and O3 , and below average surface observations of RH, are the result of the arrival of air originating from the middle and upper troposphere. During the spring of 2004, no direct STTs were observed; all identified events were determined to be indirect STTs or middle to upper troposphere transport that occurred several days prior to being detected at Harlech. The most significant event occurred between 2 and 11 April, which had the longest period of elevated 7Be and O 3 observations and the lowest RH measured during the spring of 2004, and where the modeling showed a strong stratospheric input. This input can be connected with two well-defined stratospheric intrusions occurring over the northern Pacific Ocean, more than 5 days before the associated surface observations. Furthermore, the modeling shows that periods of below average 7Be and O3 occurred when the station was mainly influenced by air masses circulating in the boundary layer. Key Points 14-day inverse modeling for daily 7Be and O3 in Alberta, March-June 2004Only indirect stratospheric intrusions can be associated to high concentrationsLow concentrations are associated mainly to boundary layer air masses ©2013. American Geophysical Union. All Rights Reserved. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/63364
Appears in Collections: 影响、适应和脆弱性 气候减缓与适应
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作者单位: Department of Earth Sciences, University of Alberta, Edmonton, AB, Canada; Canadian Meteorological Centre, Edmonton, QC, Canada; Meteorological Service of Canada, Environment Canada, Edmonton, AB, Canada
Recommended Citation:
D'Amours R.,Mintz R.,Mooney C.,et al. A modeling assessment of the origin of Beryllium-7 and Ozone in the Canadian Rocky Mountains[J]. Journal of Geophysical Research Atmospheres,2013-01-01,118(17)