1999
DOI: 10.1016/s1352-2310(98)00422-1
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Climate-relevant aerosol parameters of South-East-Asian forest fire haze

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Cited by 43 publications
(10 citation statements)
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“…8). This result is similar to the airborne observations of VON HOYNINGEN-HUENE et al (1999) which show the upper level of haze is between 2000 m to 2500 m and of BRAAK (1929) who observed that the haze is most dense between 1000 and 2000 m. This also confirms the observation that the boundary layer and the trade wind inversion within these levels largely influence the haze transport in the tropics. The trade wind inversion serves as a lid or capping for the haze (HEIL et al, 1998;BRAAK, 1929).…”
Section: Discussion On Haze Transportsupporting
confidence: 91%
See 1 more Smart Citation
“…8). This result is similar to the airborne observations of VON HOYNINGEN-HUENE et al (1999) which show the upper level of haze is between 2000 m to 2500 m and of BRAAK (1929) who observed that the haze is most dense between 1000 and 2000 m. This also confirms the observation that the boundary layer and the trade wind inversion within these levels largely influence the haze transport in the tropics. The trade wind inversion serves as a lid or capping for the haze (HEIL et al, 1998;BRAAK, 1929).…”
Section: Discussion On Haze Transportsupporting
confidence: 91%
“…Although secondary aerosols play a critical role in the study of long-range transport of the haze, as indicated by their presence in observations in Kuala Lumpur in 1997(vON HOYNINGEN-HUENE et al, 1999, chemical transformations of particulate matter and other products of biomass burning are not included in the model. The simulations focus only on the transport of primary total particulate matter with no associated aqueous and gas phase chemistry involved.…”
Section: Removal Processesmentioning
confidence: 99%
“…There are very few absorption retrievals for Songkhla. In comparison, broadband retrievals made by Hoyningen-Huene et al (1999) observing aged smoke being transported out of the IC. With particle size and ω o slightly higher than Chiang Mai in the source region, aerosol optical properties are consistent with known evolution .…”
Section: Aeronet Sites At Chiang Mai and Silpakorn Universities Inmentioning
confidence: 99%
“…Figure 1 shows the distribution of the real parts of biomass burning (Westphal et al 1991;Yamasoe et al 1998;von Hoyningen-Huene et al 1999;Guyon et al 2003;Procopio et al 2003;Colarco 2004;Schkolnik et al 2007;Hungershoefer et al 2008;Levin et al 2010), and organic (Schnaiter et al 2003;Pettersson et al 2004;Lack et al 2006;Abo Riziq et al 2007;Barkey et al 2007;Yu et al 2008;LangYona et al 2009;Wex et al 2009;Lang-Yona et al 2010b;Nakayama et al 2010b;Trainic et al 2011;Flores et al 2012;Trainic et al 2012) and inorganic (Abo Riziq et al 2007;LangYona et al 2009;Trainic et al 2011) aerosols found in the literature. In this study, we exclude soot particles due to their complex aggregated structure.…”
Section: Approachmentioning
confidence: 99%