DOI: 10.1002/jgrd.50211
论文题名: Meteorology and dust in the central Sahara: Observations from Fennec supersite-1 during the June 2011 Intensive Observation Period
作者: Marsham J.H. ; Hobby M. ; Allen C.J.T. ; Banks J.R. ; Bart M. ; Brooks B.J. ; Cavazos-Guerra C. ; Engelstaedter S. ; Gascoyne M. ; Lima A.R. ; Martins J.V. ; McQuaid J.B. ; O'Leary A. ; Ouchene B. ; Ouladichir A. ; Parker D.J. ; Saci A. ; Salah-Ferroudj M. ; Todd M.C. ; Washington R.
刊名: Journal of Geophysical Research Atmospheres
ISSN: 21698996
出版年: 2013
卷: 118, 期: 10 起始页码: 4069
结束页码: 4089
语种: 英语
英文关键词: dust
; haboob
; low-level jet
; monsoon
; Saharan heat low
; Saharan upper boundary-layer jet
Scopus关键词: Atmospheric thermodynamics
; Boundary layers
; Meteorology
; Moisture
; Wind
; haboob
; Heat low
; In-situ observations
; Intensive observation periods
; Low level jet
; monsoon
; Nocturnal low-level jets
; Short-wave radiation
; Dust
; atmospheric convection
; boundary layer
; diurnal activity
; dust
; energy balance
; heat budget
; in situ measurement
; jet
; meteorology
; monsoon
; parameterization
; remote sensing
; wind velocity
; Adrar [Algeria]
; Algeria
; Bordj Badji Mokhtar
; Sahara
; Vulpes zerda
英文摘要: We describe observations from the Fennec supersite at Bordj Badji Mokhtar (BBM) made during the June 2011 Fennec Intensive Observation Period. These are the first detailed in situ observations of meteorology and dust from the central Sahara, close to the center of the Saharan heat low and the summertime dust maximum. Historically, a shortage of such Saharan observations has created problems for evaluating processes, models, and remote sensing. There was a monsoon influence at BBM before 8 June and after 12 June, with dry Harmattan winds in between. A split boundary layer, generated by ventilation from the Atlantic, persisted during the drier phase. Extensive cold pools (haboobs) and microburst-type events were regularly observed. Moisture reached BBM at night from the monsoon and the embedded haboobs. As well as the regularly occurring nocturnal low-level jet (LLJ), a Saharan upper boundary layer (650 hPa) jet was observed, where winds feel drag from dry convection in the afternoon. This jet is linked to the diurnal cycles of moisture and cloud. Most dust was observed in the cloudier monsoon-affected periods, and covarying dust and cloud amounts explain most of the variations in shortwave radiation that control the surface sensible flux. Dustiness is related to a standard parameterization of uplift using 10 m winds ("uplift potential"), and this is used to estimate uplift. Around 50% of uplift is nocturnal. Around 30% is from the LLJ, and 50% is from haboobs, which are mainly nocturnal. This demonstrates, for the first time from observations, the key role of haboobs, which are problematic for models. Key PointsFirst detailed observations from the central Sahara (upper BL jet observed)Most dust in moist air. Together, dust & cloud control surface energy balance~50% of dust uplift is nocturnal. ~30% from the LLJ and ~50% from haboobs ©2013. American Geophysical Union. All Rights Reserved. 资助项目: NE/G017166/1
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/63743
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: National Centre for Atmospheric Science, University of Leeds, Leeds, United Kingdom; School of Earth and Environment, University of Leeds, Leeds, United Kingdom; University of Oxford, Oxford, United Kingdom; Imperial College, London, United Kingdom; University of Sussex, East Sussex, United Kingdom; University of Maryland, Baltimore County (UMBC), Baltimore MD, United States; Office National de Météorologie, Algiers, Algeria; Aeroqual Limited, Auckland, New Zealand
Recommended Citation:
Marsham J.H.,Hobby M.,Allen C.J.T.,et al. Meteorology and dust in the central Sahara: Observations from Fennec supersite-1 during the June 2011 Intensive Observation Period[J]. Journal of Geophysical Research Atmospheres,2013-01-01,118(10)