Determination of mixing layer heights from ceilometer data

被引:33
作者
Schäfer, K
Emeis, S
Rauch, A
Münkel, C
Vogt, S
机构
[1] Forschungszentrum Karlsruhe, Inst Meteorol & Klimaforsch, IMK, IFU, D-82467 Garmisch Partenkirchen, Germany
[2] Forschungszentrum Karlsruhe GmbH, Inst Meteorol & Klimaforsch, IMK, ASF, D-76021 Karlsruhe, Germany
来源
REMOTE SENSING OF CLOUDS AND THE ATMOSPHERE IX | 2004年 / 5571卷
关键词
non-intrusive measurement techniques; ceilometer; LIDAR; SODAR; mixing layer height;
D O I
10.1117/12.565592
中图分类号
TP7 [遥感技术];
学科分类号
081102 ; 0816 ; 081602 ; 083002 ; 1404 ;
摘要
The Vaisala ceilometer LD40 is an eye-safe commercial lidar. It is designed originally to detect cloud base heights and vertical visibility for aviation safety purposes. The instrument was operated continuously at different measurement campaigns to detect mixing layer height from aerosol backscatter profiles. First results with the CT25K ceilometer were presented last year in the paper SPIE 5235-64 from the environmental measuring campaign in the frame of the BMBF-funded project VALIUM in Hanover, Germany, investigating the air pollution in a street canyon and the surrounding with various sensors. A software for routine retrieval of mixing layer height (MLH) from ceilometer data was developed. A comparison with mixing layer height retrievals from a SODAR and a wind-temperature-radar (WTR) operated in the urban region of Munich will be shown. The three instruments give information that partly agree and partly complement each other. The ceilometer gives information on the aerosol content of the air and the WTR provides a direct measurement of the vertical temperature distribution in the boundary layer. The WTR and the ceilometer add information on the moisture structure of the boundary layer that is not detected by the SODAR which gives information on the thermal structure. On the other hand this comparison validates known techniques by which the MLH is derived from SODAR data. In the absence of low clouds and precipitation ceilometers can estimate the mixing-layer-height fairly well. The potential of the ceilometer, being the smallest instrument among the used ones as LIDAR, SODAR and WTR, will be discussed to be used in future MLH studies.
引用
收藏
页码:248 / 259
页数:12
相关论文
共 13 条
[1]   Frequency distributions of the mixing height over an urban area from SODAR data [J].
Emeis, S ;
Türk, M .
METEOROLOGISCHE ZEITSCHRIFT, 2004, 13 (05) :361-367
[2]   Vertical wind profiles over an urban area [J].
Emeis, S .
METEOROLOGISCHE ZEITSCHRIFT, 2004, 13 (05) :353-359
[3]   Atmospheric boundary-layer structure from simultaneous SODAR, RASS, and ceilometer measurements [J].
Emeis, S ;
Münkel, C ;
Vogt, S ;
Müller, WJ ;
Schäfer, K .
ATMOSPHERIC ENVIRONMENT, 2004, 38 (02) :273-286
[4]   Comparison of lidar methods to determine the Aerosol Mixed Layer top [J].
Martucci, G ;
Srivastava, MK ;
Mitev, V ;
Matthey, R ;
Frioud, M ;
Richner, H .
REMOTE SENSING OF CLOUDS AND THE ATMOSPHERE VIII, 2004, 5235 :447-456
[5]   Aerosol concentration measurements with a lidar ceilometer:: results of a one year measuring campaign [J].
Münkel, C ;
Emeis, S ;
Müller, WJ ;
Schäfer, K .
REMOTE SENSING OF CLOUDS AND THE ATMOSPHERE VIII, 2004, 5235 :486-496
[6]   Observation of aerosol in the mixing layer by a ground-based lidar ceilometer [J].
Münkel, C ;
Emeis, S ;
Müller, WJ ;
Schäfer, K .
REMOTE SENSING OF CLOUDS AND THE ATMOSPHERE VII, 2003, 4882 :344-352
[7]  
RASANEN J, 2000, P 3 S URB ENV AUG 15, P34
[8]   Satellite-derived determination of PM10 concentration and of the associated risk on public health [J].
Sarigiannis, D ;
Sifakis, NI ;
Soulakellis, N ;
Tombrou, M ;
Schäfer, K .
REMOTE SENSING OF CLOUDS AND THE ATMOSPHERE VIII, 2004, 5235 :408-416
[9]   Multidisciplinary data and model fusion:: a key to integrated air quality assessment [J].
Sarigiannis, D ;
Soulakellis, N ;
Sifakis, NI ;
Tombrou, M ;
Schäfer, K .
REMOTE SENSING OF CLOUDS AND THE ATMOSPHERE VII, 2003, 4882 :520-531
[10]  
SCHAFER K, 2002, INT J WATER AIR SOIL, V2, P91