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Structure and dynamics of the Saharan atmospheric boundary layer during the West African Monsoon onset: Observations and analyses from research flights of 14 and 17 July 2006

Messager, Ch. und Parker, D. und Reitebuch, O. und Agusti-Panareda, A. und Taylor, Ch. und Cuesta, J. (2010) Structure and dynamics of the Saharan atmospheric boundary layer during the West African Monsoon onset: Observations and analyses from research flights of 14 and 17 July 2006. Quarterly Journal of the Royal Meteorological Society, Seiten 107-124. DOI: 10.1002/qj.469.

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Offizielle URL: http://www3.interscience.wiley.com/cgi-bin/fulltext/122528229/PDFSTART

Kurzfassung

This paper presents the results of co-ordinated research flights over the Saharan heat-low, conducted during July 2006 as part of the African Monsoon Multidisciplinary Analysis (AMMA) Special Observing Periods. The flights consisted of a morning transect on 14 July 2006 with the Falcon F20 aircraft of the Deutsches Zentrum für Luft- und Raumfahrt (DLR), using the Doppler lidar WIND to observe the tropospheric winds, followed by an afternoon flight on 17 July with the BAe146 aircraft of the Facility for Airborne Atmospheric Measurements (FAAM) releasing a curtain of 16 dropsondes. Measurements from radiosondes at the Algerian stations of Tamanrasset and In Salah, as well as the CALIPSO spaceborne lidar, are analysed also. It is shown that the daytime Saharan atmospheric boundary layer exhibits a remarkable split structure, with a well-mixed convective layer lying beneath a residual layer whose dynamics appear to be more nearly laminar. Observations from Saharan radiosonde stations confirm that the Saharan residual boundary layer is, on some days, a persistent rather than a transient feature, and that on occasion the residual layer can last right through the day. The broad features of the Saharan heat-low thermodynamics and winds are successfully captured by the ECMWF operational analyses and the discrepancies are quantified here. The lidar winds of 14 July confirm that the analysis represents the main airflows accurately, apart from the zone to the southeast of a mid-level trough, for which the southerly component of winds was underestimated by some 8 m s-1. On 17 July, the strengths of both the southwesterly monsoon and the northeasterly Harmattan winds were slightly underestimated also. The region of maximum boundary-layer temperature over the desert was around 1 degree too far north, and too broad in the analysis, while the equivalent potential temperature in the Saharan convective boundary layer was around 2 K lower than observed. The near-saturated layer observed at the top of the Saharan atmospheric boundary layer was underestimated also in the analysis, in horizontal extent and altitude. The intertropical front of 17 July was coincident with strong surface contrasts in vegetation and fluxes. On each study day the intertropical front in the analyses was around 1 degree further north than observed.

Dokumentart:Zeitschriftenbeitrag
Zusätzliche Informationen:Published Online: 3 Aug 2009
Titel:Structure and dynamics of the Saharan atmospheric boundary layer during the West African Monsoon onset: Observations and analyses from research flights of 14 and 17 July 2006
Autoren:
AutorenInstitution oder E-Mail-Adresse der Autoren
Messager, Ch.CNRS, Plouzané, F
Parker, D.Univ. Leeds, Leeds, UK
Reitebuch, O.DLR
Agusti-Panareda, A.ECMWF, Reading, UK
Taylor, Ch.Center Ecology Hydrology, Wallingford, UK
Cuesta, J.IPSL, Palaiseau, F
Datum:2010
Erschienen in:Quarterly Journal of the Royal Meteorological Society
Referierte Publikation:Ja
In Open Access:Nein
In SCOPUS:Ja
In ISI Web of Science:Ja
DOI :10.1002/qj.469
Seitenbereich:Seiten 107-124
Status:veröffentlicht
Stichwörter:Convective and residual layers, Saharan heat-low dynamics, SHL radiosoundings and lidar profiles
HGF - Forschungsbereich:Verkehr und Weltraum (alt)
HGF - Programm:Weltraum (alt)
HGF - Programmthema:W EO - Erdbeobachtung
DLR - Schwerpunkt:Weltraum
DLR - Forschungsgebiet:W EO - Erdbeobachtung
DLR - Teilgebiet (Projekt, Vorhaben):W - Projekt ADM II (alt)
Standort: Oberpfaffenhofen
Institute & Einrichtungen:Institut für Physik der Atmosphäre > Lidar
Hinterlegt von: Oliver Reitebuch
Hinterlegt am:02 Dez 2009 18:36
Letzte Änderung:12 Dez 2013 20:46

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