Physics Department

Research Group
"Optical Remote Measurements - Analysis of Atmospheric Processes with Optical Methods"


PRD - PEARL RIVER DELTA EXPERIMENT

Introduction

As part of the 2004 intensive Pearl River Delta measurement campaign, Raman lidar and Sun photometer observations were performed in October-November 2004 to characterize the optical properties of anthropogenic haze in the southern coastal region of the Guangdong province close to the south coast of China. The field site was chosen at Xinken (22.6° N, 113.6° W) which is located at the Pearl River, about 80 km northwest of the center of Hong Kong, 60 km southwest of Guangzhou, and 50 km west of Shenzen. The Guangdong province is one of the fastest growing economical centers in China. 40-50 million people live in the Pearl River Delta (PRD) region (about 250 km x 250 km) at the south coast of China.


Raman lidar Polly in front of the aerosol container for in situ aerosol observations of IfT in Xinken, China (Thomas Tuch, 2004)



The chemical composition of the aerosol in that area (including Hong Kong) has recently been analyzed in detail. The haze mainly consists of particles from fossil fuel consumption and biomass burning. Minor contributions result from regional and long-range transport of dust (including road dust) and sea breeze effects (maritime particles). The climate-relevant optical properties of the haze, a mixture of young and well-aged particles, have not been quantified yet. More generally speaking, column and height-resolved observations of aerosol optical properties in the subtropical region of east Asia are very limited. Such observations are, however, urgently needed for a realistic estimation of the climatic impact of present and future states of aerosol pollution in eastern Asia.

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Measurements

For the first time, Raman lidar observations of aerosol optical properties were conducted in China. The portable Raman lidar Polly separately measures profiles of the volume extinction and backscatter coefficients of the particles, and thus the respective extinction-to-backscatter ratio at 532-nm wavelength during nighttime. At daytime, when Raman signals cannot be detected, the lidar delivers profiles of the particle backscatter coefficient only. The automatic Sun photometer, on the other hand, continuously records aerosol optical depths with high spectral resolution (about 10 aerosol channels) from 351–1063 nm during daytime. Optical depth uncertainties are of the order of 0.01–0.03.



Range-corrected signal at 532 nm,
at Xinken, China, on October 23, 2004;
the boundary-layer height derived with a wavelet-analysis technique is indicated
(Click on picture to enlarge!)

Discussion

Raman lidar and Sun photometer observations at Xinken, Pearl River Delta (22.6° N, 113.6° E), near the south coast of China in October 2004 revealed high values of aerosol optical depth of, on average, 0.91 at 532-nm wavelength. Column-averaged particle extinction coefficients of up to 800 Mm-1 were found in the haze layer that typically reached up to 1.5–3 km height. Lidar ratios (mainly 40–60 sr) and Angström exponents (around 1 for the 381–502-nm and 1.2 for the 502–1046-nm spectral range) indicate comparably large and considerably absorbing particles (effective radius of about 0.3 µm, single scattering albedo of 0.85–0.9) that mainly originate from industrial and biomass-burning emissions. The observed high aerosol optical depth in the Guangdong province, one of the fasted growing economic centers of China, is in agreement with the expected 1990–2005 pollution trend, derived from 1960– 1990 observations of aerosol optical depth.

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Last modification: 2005-12-21