Please use this identifier to cite or link to this item: https://ptsldigital.ukm.my/jspui/handle/123456789/778117
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dc.contributor.authorI.E. Galbally-
dc.contributor.authorC.R. Roy-
dc.contributor.editorMohammad Ilyas-
dc.date.accessioned2025-02-27T06:17:32Z-
dc.date.available2025-02-27T06:17:32Z-
dc.identifier.isbn9838610623en_US
dc.identifier.urihttps://ptsldigital.ukm.my/jspui/handle/123456789/778117-
dc.description.abstractThe sources of ozone in the troposphere are stratospheric/tropospheric exchange and in situ photochemical production; the sinks include destruction at the earth's surface and in situ photochemical destruction. The distribution of ozone in the tropical troposphere reflects the rapidity of photochemical processes in the tropics. In this review of current knowledge of ozone in the tropical troposphere, a discussion on the atmospheric cycles of ozone over the remote tropical oceans, over the continents in unperturbed conditions, over the continents biomass burning and in tropical urban areas is presented. The areas of lowest tropospheric ozone content occur over the tropical oceans while the most enriched regions occur over the continents following biomass burning.en_US
dc.language.isoenen_US
dc.publisherUniversity of Science Malaysia; United Nations Environment Programmeen_US
dc.subjectTropospheric ozoneen_US
dc.subjectOzone layeren_US
dc.subjectAtmospheric chemistryen_US
dc.subjectOzone pollutionen_US
dc.titleOzone in the tropical troposphere : a reviewen_US
dc.typeSeminar Papersen_US
dc.format.pages139-158en_US
dc.identifier.callnoGBQC879.7.I57 1990e semkaten_US
dc.contributor.conferencenameInternational Conference on Tropical Ozone and Atmospheric Change-
dc.contributor.conferencenameOzone Depletion : Implications for the Tropics-
dc.coverage.conferencelocationPulau Pinang-
dc.date.conferencedate1990-02-20-
Appears in Collections:Seminar Papers/ Proceedings / Kertas Kerja Seminar/ Prosiding

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