Verification of SBL models by mobile SODAR measurements

2012 ◽  
Vol 50 (1/2/3/4) ◽  
pp. 250
Author(s):  
Paweł Netzel ◽  
Jacek �š ◽  
N.A. lopek ◽  
Anetta Drzeniecka Osiadacz
Keyword(s):  
Author(s):  
Bret W. Butler ◽  
Daniel M. Jimenez ◽  
Casey C. Teske

1999 ◽  
Vol 11 (1) ◽  
pp. 93-99 ◽  
Author(s):  
S. Argentini ◽  
G. Mastrantonio ◽  
A. Viola

Simultaneous acoustic Doppler sodar and tethersonde measurements were used to study some of the characteristics of the unstable boundary layer at Dumont d'Urville, Adélie Land, East Antarctica during the summer 1993–94. A description of the convective boundary layer and its behaviour in connection with the wind regime is given along with the frequency distribution of free convection episodes. The surface heat flux has been evaluated using the vertical velocity variance derived from sodar measurements. The turbulent exchange coefficients, estimated by coupling sodar and tethered balloon measurements, are in strong agreement with those present in literature for the Antarctic regions.


2007 ◽  
Vol 7 (3) ◽  
pp. 7535-7567
Author(s):  
J. Lauros ◽  
E. D. Nilsson ◽  
M. Dal Maso ◽  
M. Kulmala

Abstract. The connection between new particle formation and micro- and mesoscale meteorology was studied based on measurements at SMEAR II station in Southern Finland. We analyzed turbulent conditions described by sodar measurements and utilized these combined with surface layer measurements and a simple model to estimate the upper boundary layer conditions. Turbulence was significantly stronger on particle formation days and the organic vapor saturation ratio increase due to large eddies was stronger on event than nonevent days. We examined which variables could be the best indicators of new particle formation and concluded that the formation probability depended on the condensation sink and temporal temperature change at the top of the atmospheric boundary layer. Humidity and heat flux may also be good indicators for particle formation.


2007 ◽  
Vol 7 (18) ◽  
pp. 4781-4792 ◽  
Author(s):  
J. Lauros ◽  
E. D. Nilsson ◽  
M. Dal Maso ◽  
M. Kulmala

Abstract. The connection between new particle formation and micro- and mesoscale meteorology was studied based on measurements at SMEAR II station in Southern Finland. We analyzed turbulent conditions described by sodar measurements and utilized these combined with surface layer measurements and a simple model to estimate the upper boundary layer conditions. Turbulence was significantly stronger on particle formation days and the organic vapor saturation ratio increase due to large eddies was stronger on event than nonevent days. We examined which variables could be the best indicators of new particle formation and concluded that the formation probability depended on the condensation sink and temporal temperature change at the top of the atmospheric boundary layer. Humidity and heat flux may also be good indicators for particle formation.


2013 ◽  
Vol 2013 (0) ◽  
pp. _J056021-1-_J056021-5
Author(s):  
Yasunari KAMDA ◽  
Takao MAEDA ◽  
Junsuke MURATA ◽  
Nobuyuki HAYASAKI ◽  
Makoto IIDA ◽  
...  
Keyword(s):  

2011 ◽  
Vol 143 (1) ◽  
pp. 97-106 ◽  
Author(s):  
Paul Behrens ◽  
J. O’Sullivan ◽  
R. Archer ◽  
S. Bradley

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