Rayleigh lidar system for middle atmosphere research in the arctic

被引:44
作者
Thayer, JP [1 ]
Nielsen, NB [1 ]
Warren, RE [1 ]
Heinselman, CJ [1 ]
Sohn, J [1 ]
机构
[1] DANISH METEOROL INST,KELLYVILLE RADAR,DK-3910 KANGERLUSSUAQ,GREENLAND,DENMARK
关键词
lidar; Rayleigh scatter; middle atmosphere; arctic; temperature; aerosols;
D O I
10.1117/1.601361
中图分类号
O43 [光学];
学科分类号
070207 ; 0803 ;
摘要
A Rayleigh/Mie lidar system deployed at the Sondrestrom Atmospheric Research Facility located on the west coast of Greenland near the town of Kangerlussuaq (67.0 deg N, 50.9 deg W) has been in operation since 1993 making unique observations of the arctic middle atmosphere. The vertically directed lidar samples the elastically back-scattered laser energy from molecules (Rayleigh) and aerosols (Mie) over the altitude range from 15 to 90 km at high spatial resolution. The limited amount of arctic observations of the middle atmosphere currently available emphasizes the importance and utility of a permanent Rayleigh lidar system in Greenland. The lidar system consists of a frequency-doubled, 17-W Nd:YAG laser at 532 nm, a 92 cm Newtonian telescope, and a two-channel photon counting receiver. The principal objective of the lidar project is to contribute to studies concerned with the climatology and phenomenology of the arctic middle atmosphere. To this end, we describe the lidar system in detail, evaluate system performance, describe data analysis, and discuss the system capabilities in determining the density, temperature, and the presence of aerosols in the arctic middle atmosphere. Particular emphasis is placed on the derivation of temperature from the lidar measurement and on the impact of signal-induced noise on this analysis. Also, we develop a statistical filter based on a Bayesian approach to optimally smooth the lidar profile in range. This filter preserves the short-term fluctuations in the low-altitude data consisting of relatively high SNR, whereas more smoothing is applied to the high-altitude data as the SNR decreases. (C) 1997 Society of Photo-Optical Instrumentation Engineers.
引用
收藏
页码:2045 / 2061
页数:17
相关论文
共 52 条
[11]   SEMIDIURNAL AND DIURNAL TIDAL EFFECTS IN THE MIDDLE ATMOSPHERE AS SEEN BY RAYLEIGH LIDAR [J].
GILLE, ST ;
HAUCHECORNE, A ;
CHANIN, ML .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1991, 96 (D4) :7579-7587
[12]   SIMULTANEOUS OBSERVATIONS OF NOCTILUCENT CLOUDS AND MESOPAUSE TEMPERATURES BY LIDAR [J].
HANSEN, G ;
VONZAHN, U .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1994, 99 (D9) :18989-18999
[13]   1ST DETECTION OF A NOCTILUCENT CLOUD BY LIDAR [J].
HANSEN, G ;
SERWAZI, M ;
VONZAHN, U .
GEOPHYSICAL RESEARCH LETTERS, 1989, 16 (12) :1445-1448
[14]   DENSITY AND TEMPERATURE PROFILES OBTAINED BY LIDAR BETWEEN 35-KM AND 70-KM [J].
HAUCHECORNE, A ;
CHANIN, ML .
GEOPHYSICAL RESEARCH LETTERS, 1980, 7 (08) :565-568
[15]   A 2-D DYNAMIC-MODEL OF MESOSPHERIC TEMPERATURE INVERSIONS IN WINTER [J].
HAUCHECORNE, A ;
MAILLARD, A .
GEOPHYSICAL RESEARCH LETTERS, 1990, 17 (12) :2197-2200
[16]   MESOSPHERIC TEMPERATURE INVERSION AND GRAVITY-WAVE BREAKING [J].
HAUCHECORNE, A ;
CHANIN, ML ;
WILSON, R .
GEOPHYSICAL RESEARCH LETTERS, 1987, 14 (09) :933-936
[17]   Multi-instrument zenith observations of noctilucent clouds over Greenland on July 30/31, 1995 [J].
Hecht, JH ;
Thayer, JP ;
Gutierrez, DJ ;
McKenzie, DL .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D2) :1959-1970
[18]  
KECKHUT P, 1993, J ATMOS OCEAN TECH, V10, P850, DOI 10.1175/1520-0426(1993)010<0850:ACROTD>2.0.CO
[19]  
2
[20]   A REVIEW OF LASER RADAR MEASUREMENTS OF ATMOSPHERIC PROPERTIES [J].
KENT, GS ;
WRIGHT, RWH .
JOURNAL OF ATMOSPHERIC AND TERRESTRIAL PHYSICS, 1970, 32 (05) :917-+