File Download
There are no files associated with this item.
Links for fulltext
(May Require Subscription)
- Publisher Website: 10.1016/j.atmosenv.2010.01.012
- Scopus: eid_2-s2.0-77649342103
- WOS: WOS:000276736600010
- Find via
Supplementary
- Citations:
- Appears in Collections:
Article: Improved land cover and emission factors for modeling biogenic volatile organic compounds emissions from Hong Kong
Title | Improved land cover and emission factors for modeling biogenic volatile organic compounds emissions from Hong Kong | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|
Authors | |||||||||||
Keywords | Bvoc Emission Isoprene Monoterpene Other Vocs | ||||||||||
Issue Date | 2010 | ||||||||||
Publisher | Pergamon. The Journal's web site is located at http://www.elsevier.com/locate/atmosenv | ||||||||||
Citation | Atmospheric Environment, 2010, v. 44 n. 11, p. 1456-1468 How to Cite? | ||||||||||
Abstract | This paper describes a study of local biogenic volatile organic compounds (BVOC) emissions from the Hong Kong Special Administrative Region (HKSAR). An improved land cover and emission factor database was developed to estimate Hong Kong emissions using MEGAN, a BVOC emission model developed by Guenther et al. (2006). Field surveys of plant species composition and laboratory measurements of emission factors were combined with other data to improve existing land cover and emission factor data. The BVOC emissions from Hong Kong were calculated for 12 consecutive years from 1995 to 2006. For the year 2006, the total annual BVOC emissions were determined to be 12,400 metric tons or 9.82 × 109 g C (BVOC carbon). Isoprene emission accounts for 72%, monoterpene emissions account for 8%, and other VOCs emissions account for the remaining 20%. As expected, seasonal variation results in a higher emission in the summer and a lower emission in the winter, with emission predominantly in day time. A high emission of isoprene occurs for regions, such as Lowest Forest-NT North, dominated by broadleaf trees. The spatial variation of total BVOC is similar to the isoprene spatial variation due to its high contribution. The year to year variability in emissions due to weather was small over the twelve-year period (-1.4%, 2006 to 1995 trendline), but an increasing trend in the annual variation due to an increase in forest land cover can be observed (+7%, 2006 to 1995 trendline). The results of this study demonstrate the importance of accurate land cover inputs for biogenic emission models and indicate that land cover change should be considered for these models. © 2010 Elsevier Ltd. | ||||||||||
Persistent Identifier | http://hdl.handle.net/10722/157058 | ||||||||||
ISSN | 2023 Impact Factor: 4.2 2023 SCImago Journal Rankings: 1.169 | ||||||||||
ISI Accession Number ID |
Funding Information: The project is supported by the Hong Kong Research Grant Council (HKU 714606) and the EPD of the HKSAR Government. We would like to thank SDD, AFCD, and LCSD for providing various data for this project, Miss Jeanie Tsui for conducting the experiment and Dr. Paul Tam for conducting the field surveys. The National Center for Atmospheric Research is sponsored by the U.S. National Science Foundation. | ||||||||||
References |
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Leung, DYC | en_US |
dc.contributor.author | Wong, P | en_US |
dc.contributor.author | Cheung, BKH | en_US |
dc.contributor.author | Guenther, A | en_US |
dc.date.accessioned | 2012-08-08T08:45:09Z | - |
dc.date.available | 2012-08-08T08:45:09Z | - |
dc.date.issued | 2010 | en_US |
dc.identifier.citation | Atmospheric Environment, 2010, v. 44 n. 11, p. 1456-1468 | en_US |
dc.identifier.issn | 1352-2310 | en_US |
dc.identifier.uri | http://hdl.handle.net/10722/157058 | - |
dc.description.abstract | This paper describes a study of local biogenic volatile organic compounds (BVOC) emissions from the Hong Kong Special Administrative Region (HKSAR). An improved land cover and emission factor database was developed to estimate Hong Kong emissions using MEGAN, a BVOC emission model developed by Guenther et al. (2006). Field surveys of plant species composition and laboratory measurements of emission factors were combined with other data to improve existing land cover and emission factor data. The BVOC emissions from Hong Kong were calculated for 12 consecutive years from 1995 to 2006. For the year 2006, the total annual BVOC emissions were determined to be 12,400 metric tons or 9.82 × 109 g C (BVOC carbon). Isoprene emission accounts for 72%, monoterpene emissions account for 8%, and other VOCs emissions account for the remaining 20%. As expected, seasonal variation results in a higher emission in the summer and a lower emission in the winter, with emission predominantly in day time. A high emission of isoprene occurs for regions, such as Lowest Forest-NT North, dominated by broadleaf trees. The spatial variation of total BVOC is similar to the isoprene spatial variation due to its high contribution. The year to year variability in emissions due to weather was small over the twelve-year period (-1.4%, 2006 to 1995 trendline), but an increasing trend in the annual variation due to an increase in forest land cover can be observed (+7%, 2006 to 1995 trendline). The results of this study demonstrate the importance of accurate land cover inputs for biogenic emission models and indicate that land cover change should be considered for these models. © 2010 Elsevier Ltd. | en_US |
dc.language | eng | en_US |
dc.publisher | Pergamon. The Journal's web site is located at http://www.elsevier.com/locate/atmosenv | en_US |
dc.relation.ispartof | Atmospheric Environment | en_US |
dc.subject | Bvoc Emission | en_US |
dc.subject | Isoprene | en_US |
dc.subject | Monoterpene | en_US |
dc.subject | Other Vocs | en_US |
dc.title | Improved land cover and emission factors for modeling biogenic volatile organic compounds emissions from Hong Kong | en_US |
dc.type | Article | en_US |
dc.identifier.email | Leung, DYC:ycleung@hku.hk | en_US |
dc.identifier.authority | Leung, DYC=rp00149 | en_US |
dc.description.nature | link_to_subscribed_fulltext | en_US |
dc.identifier.doi | 10.1016/j.atmosenv.2010.01.012 | en_US |
dc.identifier.scopus | eid_2-s2.0-77649342103 | en_US |
dc.identifier.hkuros | 171122 | - |
dc.relation.references | http://www.scopus.com/mlt/select.url?eid=2-s2.0-77649342103&selection=ref&src=s&origin=recordpage | en_US |
dc.identifier.volume | 44 | en_US |
dc.identifier.issue | 11 | en_US |
dc.identifier.spage | 1456 | en_US |
dc.identifier.epage | 1468 | en_US |
dc.identifier.eissn | 1873-2844 | - |
dc.identifier.isi | WOS:000276736600010 | - |
dc.publisher.place | United Kingdom | en_US |
dc.identifier.scopusauthorid | Leung, DYC=7203002484 | en_US |
dc.identifier.scopusauthorid | Wong, P=35779341100 | en_US |
dc.identifier.scopusauthorid | Cheung, BKH=24450033800 | en_US |
dc.identifier.scopusauthorid | Guenther, A=7102062952 | en_US |
dc.identifier.citeulike | 6709531 | - |
dc.identifier.issnl | 1352-2310 | - |