Haze is a phenomenon which occurs when there is a great amount of tiny particulates suspended in the atmosphere. During the period of March 2014, a long period of haze event occurred in Penang, Malaysia. The haze condition was measured and monitored using a ground-based Lidar system. By using the measurements obtained, we evaluated the performance of the ECMWF MACC-II model. Lidar measurements showed that there was a thick aerosol layer confined in the planetary boundary layer (PBL) with extinction coefficients exceeding values of 0.3 km-1. The model however has underestimated the atmospheric conditions in Penang. Backward trajectories analysis was performed to identify aerosols sources and transport. It is speculated that the aerosols came from the North-East direction which was influenced by the North-East monsoon wind and some originated from the central eastern coast of Sumatra along the Straits of Malacca. ? 2015 AIP Publishing LLC.

Lidar measurements during a haze episode in Penang, Malaysia and validation of the ECMWF MACC-II model

Lolli S;
2015

Abstract

Haze is a phenomenon which occurs when there is a great amount of tiny particulates suspended in the atmosphere. During the period of March 2014, a long period of haze event occurred in Penang, Malaysia. The haze condition was measured and monitored using a ground-based Lidar system. By using the measurements obtained, we evaluated the performance of the ECMWF MACC-II model. Lidar measurements showed that there was a thick aerosol layer confined in the planetary boundary layer (PBL) with extinction coefficients exceeding values of 0.3 km-1. The model however has underestimated the atmospheric conditions in Penang. Backward trajectories analysis was performed to identify aerosols sources and transport. It is speculated that the aerosols came from the North-East direction which was influenced by the North-East monsoon wind and some originated from the central eastern coast of Sumatra along the Straits of Malacca. ? 2015 AIP Publishing LLC.
2015
lidar
aerosol
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/349330
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