@Article{OozeerCCZSCMC:2016:NuStTr,
author = "Oozeer, M. Y. and Chan, A. and Chel-Gee Ooi, M. and Zarzur, Alonso
Mauricio and Salinas, S. V. and Chew, B. -N. and Morris, K. I. and
Choong, W. -K",
affiliation = "{University of Nottingham Malaysia Campus} and {University of
Nottingham Malaysia Campus} and {University of Nottingham Malaysia
Campus} and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{National University of Singapore} and {National University of
Singapore} and {University of Nottingham Malaysia Campus} and
{University of Nottingham Malaysia Campus}",
title = "Numerical study of the transport and convective mechanisms of
biomass burning haze in South-Southeast Asia",
journal = "Aerosol and Air Quality Research",
year = "2016",
volume = "16",
number = "11",
pages = "2950--2963",
month = "Nov.",
keywords = "Biomass burning, Deep convection, Southeast Asia, Vertical
transport mechanism, WRF-Chem.",
abstract = "This study aims to identify the vertical transport mechanisms that
uplifted the forest fire emissions from Sumatra to the upper
troposphere during the June 2013 haze crisis. WRF-Chem is used to
simulate the formation and transport of biomass-burning haze
during the study period of 18th to 26th June 2013. The
South-Southeast Asian synoptic weather patterns and their effects
on the transport of biomass-burning emissions from Sumatra to
Peninsular Malaysia were studied computationally to explain the
phenomenon. Results show that PM10 emissions were lifted to 200
hPa height (approximately 12 km) over the Strait of Malacca on
24th June. The two identified vertical transport mechanisms
confirmed a previously conjectured convergence over the Strait of
Malacca and orographic lifting over Peninsular Malaysia. These
mechanisms were able to uplift the biomass-burning emissions to
the upper troposphere and this could have significant long-range
transport and global climatic effects.",
issn = "1680-8584",
language = "en",
urlaccessdate = "17 maio 2024"
}