One year ozonesonde measurements at Kerguelen Island (49.2°S, 70.1°E)

Influence of stratosphere-to-troposphere exchange and long-range transport of biomass burning plumes

Jean Luc Baray, Valentin Duflot, Franoise Posny, Jean Pierre Cammas, Anne Mee Thompson, Franck Gabarrot, Jean Louis Bonne, Guang Zeng

Research output: Contribution to journalArticle

5 Citations (Scopus)

Abstract

We analyze a 1 year campaign of 17 ozonesondes launched in 2008-2009 at Kerguelen Island (49.2°S, 70.1°E), the first such soundings performed at this location. Tropospheric ozone presents a large variability in austral summer (December to February) and austral winter (June to September). The baseline tropospheric ozone is higher in winter (between 30 and 50 ppbv) than in summer (between 20 and 40 ppbv). We compare these observations to a data set obtained during the same period at Lauder (45.0°S, 169.7°E), which presents a marked seasonal pattern. The analysis of trajectory runs and reanalysis output help identify two significant contributors to the tropospheric ozone level at Kerguelen: the stratosphere-to-troposphere air mass transport and the long-range transport of biomass burning plumes. The stratosphere-to- troposphere transport is exemplified by a case study of a dry and enriched ozone layer over Kerguelen (70 ppbv at an altitude of 6 km on 28 February 2009). Using Lagrangian model simulations, we show that wintertime enhancement of the tropospheric ozone baseline can be partially attributed to the long-range transport of ozone precursors from biomass burning plumes originating in southern America and Africa. However, owing to limited data and to the many factors that can cause this wintertime baseline ozone enhancement, further investigations are needed to fully explain it. Additional measurements are also needed to establish an ozone climatology, to further characterize the ozone annual cycle and wintertime enhancement, and to better compare Kerguelen with other midlatitude sites.

Original languageEnglish (US)
Article numberD06305
JournalJournal of Geophysical Research Atmospheres
Volume117
Issue number6
DOIs
StatePublished - Jan 1 2012

Fingerprint

ozonesondes
ozonesonde
biomass burning
Upper atmosphere
Troposphere
Ozone
long range transport
stratosphere
troposphere
ozone
plumes
Ion exchange
Biomass
plume
biomass
winter
summer
mass transport
annual cycle
air mass

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Oceanography
  • Forestry
  • Aquatic Science
  • Ecology
  • Condensed Matter Physics
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Physical and Theoretical Chemistry
  • Polymers and Plastics
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Materials Chemistry
  • Palaeontology

Cite this

Baray, Jean Luc ; Duflot, Valentin ; Posny, Franoise ; Cammas, Jean Pierre ; Thompson, Anne Mee ; Gabarrot, Franck ; Bonne, Jean Louis ; Zeng, Guang. / One year ozonesonde measurements at Kerguelen Island (49.2°S, 70.1°E) : Influence of stratosphere-to-troposphere exchange and long-range transport of biomass burning plumes. In: Journal of Geophysical Research Atmospheres. 2012 ; Vol. 117, No. 6.
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abstract = "We analyze a 1 year campaign of 17 ozonesondes launched in 2008-2009 at Kerguelen Island (49.2°S, 70.1°E), the first such soundings performed at this location. Tropospheric ozone presents a large variability in austral summer (December to February) and austral winter (June to September). The baseline tropospheric ozone is higher in winter (between 30 and 50 ppbv) than in summer (between 20 and 40 ppbv). We compare these observations to a data set obtained during the same period at Lauder (45.0°S, 169.7°E), which presents a marked seasonal pattern. The analysis of trajectory runs and reanalysis output help identify two significant contributors to the tropospheric ozone level at Kerguelen: the stratosphere-to-troposphere air mass transport and the long-range transport of biomass burning plumes. The stratosphere-to- troposphere transport is exemplified by a case study of a dry and enriched ozone layer over Kerguelen (70 ppbv at an altitude of 6 km on 28 February 2009). Using Lagrangian model simulations, we show that wintertime enhancement of the tropospheric ozone baseline can be partially attributed to the long-range transport of ozone precursors from biomass burning plumes originating in southern America and Africa. However, owing to limited data and to the many factors that can cause this wintertime baseline ozone enhancement, further investigations are needed to fully explain it. Additional measurements are also needed to establish an ozone climatology, to further characterize the ozone annual cycle and wintertime enhancement, and to better compare Kerguelen with other midlatitude sites.",
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One year ozonesonde measurements at Kerguelen Island (49.2°S, 70.1°E) : Influence of stratosphere-to-troposphere exchange and long-range transport of biomass burning plumes. / Baray, Jean Luc; Duflot, Valentin; Posny, Franoise; Cammas, Jean Pierre; Thompson, Anne Mee; Gabarrot, Franck; Bonne, Jean Louis; Zeng, Guang.

In: Journal of Geophysical Research Atmospheres, Vol. 117, No. 6, D06305, 01.01.2012.

Research output: Contribution to journalArticle

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T1 - One year ozonesonde measurements at Kerguelen Island (49.2°S, 70.1°E)

T2 - Influence of stratosphere-to-troposphere exchange and long-range transport of biomass burning plumes

AU - Baray, Jean Luc

AU - Duflot, Valentin

AU - Posny, Franoise

AU - Cammas, Jean Pierre

AU - Thompson, Anne Mee

AU - Gabarrot, Franck

AU - Bonne, Jean Louis

AU - Zeng, Guang

PY - 2012/1/1

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N2 - We analyze a 1 year campaign of 17 ozonesondes launched in 2008-2009 at Kerguelen Island (49.2°S, 70.1°E), the first such soundings performed at this location. Tropospheric ozone presents a large variability in austral summer (December to February) and austral winter (June to September). The baseline tropospheric ozone is higher in winter (between 30 and 50 ppbv) than in summer (between 20 and 40 ppbv). We compare these observations to a data set obtained during the same period at Lauder (45.0°S, 169.7°E), which presents a marked seasonal pattern. The analysis of trajectory runs and reanalysis output help identify two significant contributors to the tropospheric ozone level at Kerguelen: the stratosphere-to-troposphere air mass transport and the long-range transport of biomass burning plumes. The stratosphere-to- troposphere transport is exemplified by a case study of a dry and enriched ozone layer over Kerguelen (70 ppbv at an altitude of 6 km on 28 February 2009). Using Lagrangian model simulations, we show that wintertime enhancement of the tropospheric ozone baseline can be partially attributed to the long-range transport of ozone precursors from biomass burning plumes originating in southern America and Africa. However, owing to limited data and to the many factors that can cause this wintertime baseline ozone enhancement, further investigations are needed to fully explain it. Additional measurements are also needed to establish an ozone climatology, to further characterize the ozone annual cycle and wintertime enhancement, and to better compare Kerguelen with other midlatitude sites.

AB - We analyze a 1 year campaign of 17 ozonesondes launched in 2008-2009 at Kerguelen Island (49.2°S, 70.1°E), the first such soundings performed at this location. Tropospheric ozone presents a large variability in austral summer (December to February) and austral winter (June to September). The baseline tropospheric ozone is higher in winter (between 30 and 50 ppbv) than in summer (between 20 and 40 ppbv). We compare these observations to a data set obtained during the same period at Lauder (45.0°S, 169.7°E), which presents a marked seasonal pattern. The analysis of trajectory runs and reanalysis output help identify two significant contributors to the tropospheric ozone level at Kerguelen: the stratosphere-to-troposphere air mass transport and the long-range transport of biomass burning plumes. The stratosphere-to- troposphere transport is exemplified by a case study of a dry and enriched ozone layer over Kerguelen (70 ppbv at an altitude of 6 km on 28 February 2009). Using Lagrangian model simulations, we show that wintertime enhancement of the tropospheric ozone baseline can be partially attributed to the long-range transport of ozone precursors from biomass burning plumes originating in southern America and Africa. However, owing to limited data and to the many factors that can cause this wintertime baseline ozone enhancement, further investigations are needed to fully explain it. Additional measurements are also needed to establish an ozone climatology, to further characterize the ozone annual cycle and wintertime enhancement, and to better compare Kerguelen with other midlatitude sites.

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