Aerosol lidar ratio characteristics measured by a multi-wavelength Raman lidar system at Anmyeon Island, Korea

Abstract Tropospheric aerosols were investigated with a multi-wavelength Raman lidar system during two measurement periods: March 15th–April 16th, 2004 and May 23rd–June 9th, 2005 at the Korea Global Atmospheric Watch Observatory (KGAWO, 36.32°N, 126.19°E), Anmyeon Island, Korea. The extinction coefficient, backscattering coefficient and lidar ratio ( S a ) were measured at 355 and 532 nm with the Raman method. Wavelength-dependent lidar ratio data can be used to determine aerosol type. Average values of S a were 46.8 ± 6.5 and 71.1 ± 8.2 sr at 355 nm and 49.0 ± 12.2 and 78.6 ± 9.6 sr at 532 nm during the two observation periods in 2004 and 2005, respectively. HYSPLIT backward trajectory analysis showed different pathways of air mass between the two observation periods. Air mass had moved to the measurement site from the Chinese continent by a northwesterly wind in 2004, whereas it moved rather slowly in an easterly direction over the Korean Peninsula in 2005. Raman lidar results obtained in this study can provide useful information on aerosol climatology and aerosol transport characteristics in Northeast Asia.

[1]  P. Bhartia,et al.  Derivation of aerosol properties from satellite measurements of backscattered ultraviolet radiation , 1998 .

[2]  J. Klett Stable analytical inversion solution for processing lidar returns. , 1981, Applied optics.

[3]  R. Stull An Introduction to Boundary Layer Meteorology , 1988 .

[4]  A. Ansmann,et al.  Closure study on optical and microphysical properties of a mixed urban and Arctic haze air mass observed with Raman lidar and Sun photometer , 2004 .

[5]  D. Tratt,et al.  Airborne lidar observations of tropospheric aerosols during the Global Backscatter Experiment (GLOBE) Pacific circumnavigation missions of 1989 and 1990 , 1997 .

[6]  Zhaoyan Liu,et al.  Extinction-to-backscatter ratio of Asian dust observed with high-spectral-resolution lidar and Raman lidar. , 2002, Applied optics.

[7]  A. Stohl,et al.  Raman lidar observations of aged Siberian and Canadian forest fire smoke in the free troposphere over Germany in 2003 : Microphysical particle characterization , 2005 .

[8]  Yasunobu Iwasaka,et al.  LIDAR Measurements of the Vertical Aerosol Profile and Optical Depth during the ACE-Asia 2001 IOP, at Gosan, Jeju Island, Korea , 2004, Environmental monitoring and assessment.

[9]  U. Wandinger,et al.  Inversion with regularization for the retrieval of tropospheric aerosol parameters from multiwavelength lidar sounding. , 2002, Applied optics.

[10]  A. Ansmann,et al.  Microphysical particle parameters from extinction and backscatter lidar data by inversion with regularization: theory. , 1999, Applied optics.

[11]  J. Rosen,et al.  Balloon‐borne measurements of the aerosol extinction‐to‐backscatter ratio , 1997 .

[12]  P. R. Bevington,et al.  Data Reduction and Error Analysis for the Physical Sciences , 1969 .

[13]  L. Brasseur,et al.  Raman lidar measurements of the aerosol extinction‐to‐backscatter ratio over the Southern Great Plains , 2001 .

[14]  Albert Ansmann,et al.  Saharan dust over a central European EARLINET‐AERONET site: Combined observations with Raman lidar and Sun photometer , 2003 .

[15]  J. Ackermann The Extinction-to-Backscatter Ratio of Tropospheric Aerosol: A Numerical Study , 1998 .

[16]  S. H. Melfi,et al.  Raman lidar system for the measurement of water vapor and aerosols in the Earth's atmosphere. , 1992, Applied optics.

[17]  V. Ramaswamy,et al.  Global sensitivity studies of the direct radiative forcing due to anthropogenic sulfate and black carbon aerosols , 1998 .

[18]  Albert Ansmann,et al.  High aerosol load over the Pearl River Delta, China, observed with Raman lidar and Sun photometer , 2005 .

[19]  F. G. Fernald Analysis of atmospheric lidar observations: some comments. , 1984, Applied optics.

[20]  Kenneth Sassen,et al.  Depolarization of Laser Light Backscattered by Artificial Clouds , 1974 .

[21]  A. John Mallinckrodt,et al.  Data Reduction and Error Analysis for the Physical Sciences , 1993 .

[22]  Lidar observations of the Planetary Boundary Layer above the city of Thessaloniki, Greece , 1998 .

[23]  Tomohiro Nagai,et al.  Ice clouds and Asian dust studied with lidar measurements of particle extinction-to-backscatter ratio, particle depolarization, and water-vapor mixing ratio over Tsukuba. , 2003, Applied optics.

[24]  Albert Ansmann,et al.  One‐year observations of particle lidar ratio over the tropical Indian Ocean with Raman lidar , 2001 .

[25]  M. Wendisch,et al.  Optical and microphysical characterization of biomass‐ burning and industrial‐pollution aerosols from‐ multiwavelength lidar and aircraft measurements , 2002 .

[26]  Tatsuro Tsukamoto,et al.  Characterization of Asian dust and Siberian smoke with multi‐wavelength Raman lidar over Tokyo, Japan in spring 2003 , 2004 .

[27]  David M. Winker Global Observations of Aerosols and Clouds from Combined Lidar and Passive Instruments to Improve Radiation Budget and Climate Studies , 1999 .

[28]  A. Ansmann,et al.  Measurement of atmospheric aerosol extinction profiles with a Raman lidar. , 1990, Optics letters.

[29]  Albert Ansmann,et al.  Vertical profiling of optical and physical particle properties over the tropical Indian Ocean with six‐wavelength lidar: 2. Case studies , 2001 .

[30]  A. Ansmann,et al.  Experimental determination of the lidar overlap profile with Raman lidar. , 2002, Applied optics.

[31]  W. Eichinger,et al.  Structure of the atmosphere in an urban planetary boundary layer from lidar and radiosonde observations , 1994 .

[32]  A. Ansmann,et al.  Independent measurement of extinction and backscatter profiles in cirrus clouds by using a combined Raman elastic-backscatter lidar. , 1992, Applied optics.

[33]  Y. J. Kim,et al.  Chemical Composition of Post-Harvest Biomass Burning Aerosols in Gwangju, Korea , 2004, Journal of the Air & Waste Management Association.

[34]  Albert Ansmann,et al.  Unexpectedly high aerosol load in the free troposphere over central Europe in spring/summer 2003 , 2003 .

[35]  Takashi Shibata,et al.  Case study of Raman lidar measurements of Asian dust events in 2000 and 2001 at Nagoya and Tsukuba, Japan , 2002 .