A Raman lidar to measure water vapor in the atmospheric boundary layer

被引:41
作者
Froidevaux, Martin [1 ]
Higgins, Chad W. [2 ]
Simeonov, Valentin [1 ]
Ristori, Pablo [3 ]
Pardyjak, Eric [4 ]
Serikov, Ilya [5 ]
Calhoun, Ronald [6 ]
van den Bergh, Hubert [1 ]
Parlange, Marc B. [1 ]
机构
[1] Ecole Polytech Fed Lausanne, Sch Architecture Civil & Environm Engn, CH-1015 Lausanne, Switzerland
[2] Oregon State Univ, Dept Biol & Ecol Engn, Corvallis, OR 97331 USA
[3] CEILAP CITEFA CONICET, Zufriategui, Argentina
[4] Univ Utah, Dept Mech Engn, Salt Lake City, UT 84112 USA
[5] Max Planck Inst Meteorol, D-20146 Hamburg, Germany
[6] Arizona State Univ, Tempe, AZ USA
关键词
Atmospheric boundary layer; Raman lidar; Water vapor; LARGE-EDDY SIMULATION; TURBULENT-FLOW; WIND-TUNNEL; COHERENT STRUCTURES; WAVING WHEAT; AIR-FLOW; SCALE; EVAPORATION; MODEL; PROFILES;
D O I
10.1016/j.advwatres.2012.04.008
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
A new multi-telescope scanning Raman lidar designed to measure the water vapor mixing ratio in the atmospheric boundary layer for a complete diurnal cycle with high resolution spatial (1.25 m) and temporal (1 s) resolutions is presented. The high resolution allows detailed measurements of the lower atmosphere and offers new opportunities for evaporation and boundary layer research, atmospheric profiling and visualization. This lidar utilizes a multi-telescope design that provides for an operational range with a nearly constant signal-to-noise ratio, which allows for statistical investigations of atmospheric turbulence. This new generation ground-based water vapor Raman lidar is described, and first observations from the Turbulent Atmospheric Boundary Layer Experiment (TABLE) are presented. Direct comparison with in-situ point measurements obtained during the field campaign demonstrate the ability of the lidar to reliably measure the water vapor mixing ratio. Horizontal measurements taken with time are used to determine the geometric characteristics of coherent structures. Vertical scans are used to visualize nocturnal jet features, layered structures within a stably stratified atmosphere and the internal boundary layer structure over a lake. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:345 / 356
页数:12
相关论文
共 80 条
[1]   Vortex organization in the outer region of the turbulent boundary layer [J].
Adrian, RJ ;
Meinhart, CD ;
Tomkins, CD .
JOURNAL OF FLUID MECHANICS, 2000, 422 :1-54
[2]   Natural integration of scalar fluxes from complex terrain [J].
Albertson, JD ;
Parlange, MB .
ADVANCES IN WATER RESOURCES, 1999, 23 (03) :239-252
[3]   Large-eddy simulation over heterogeneous terrain with remotely sensed land surface conditions [J].
Albertson, JD ;
Kustas, WP ;
Scanlon, TM .
WATER RESOURCES RESEARCH, 2001, 37 (07) :1939-1953
[4]   Entrainment results from the Flatland boundary layer experiments [J].
Angevine, WM ;
Grimsdell, AW ;
McKeen, SA ;
Warnock, JM .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1998, 103 (D12) :13689-13701
[5]  
[Anonymous], 2002, The Essential Physics of Medical Imaging
[6]   Field study of the dynamics and modelling of subgrid-scale turbulence in a stable atmospheric surface layer over a glacier [J].
Bou-Zeid, Elie ;
Higgins, Chad ;
Huwald, Hendrik ;
Meneveau, Charles ;
Parlange, Marc B. .
JOURNAL OF FLUID MECHANICS, 2010, 665 :480-515
[7]   A WIND-TUNNEL STUDY OF AIR-FLOW IN WAVING WHEAT - SINGLE-POINT VELOCITY STATISTICS [J].
BRUNET, Y ;
FINNIGAN, JJ ;
RAUPACH, MR .
BOUNDARY-LAYER METEOROLOGY, 1994, 70 (1-2) :95-132
[8]  
Brutsaert W., 2013, Evaporation into the Atmosphere: Theory, History and Applications
[9]  
Cohn SA, 1998, B AM METEOROL SOC, V79, P1329, DOI 10.1175/1520-0477(1998)079<1329:TLIFTL>2.0.CO
[10]  
2