Details

Autor(en) / Beteiligte

• Stickler, A
• Fischer, H
• Bozem, H
• Gurk, C
• Schiller, C
• Martinez-Harder, M
• Kubistin, D
• Harder, H
• Williams, J
• Eerdekens, G
• Yassaa, N
• Ganzeveld, L
• Sander, R
• Lelieveld, J

Titel

Chemistry, transport and dry deposition of trace gases in the boundary layer over the tropical Atlantic Ocean and the Guyanas during the GABRIEL field campaign

Ist Teil von

• Atmospheric chemistry and physics discussions, 2007-04, Vol.7 (2), p.4781-4855

Ort / Verlag

European Geosciences Union

Erscheinungsjahr

2007

Quelle

EZB Electronic Journals Library

Beschreibungen/Notizen

• We present a comparison of different Lagrangian and steady state box model runs with measurement data obtained during the GABRIEL campaign over the tropical Atlantic Ocean and the rainforest in the Guyanas, October 2005. Lagrangian modelling of boundary layer (BL) CO constrained by measurements of reactive trace gases and radiation is used to derive a horizontal gradient (≈ 5.6 pmol/mol km super(− 1)) of this compound from the ocean to the rainforest (east to west). This is significantly smaller than that derived from the measurements (16-48 pmol/mol km super(− 1)), indicating that photochemical production from organic precursors alone cannot explain the observed strong gradient. It appears that HCHO is overestimated by the Lagrangian and QUOTATION_MARKsteady stateQUOTATION_MARK models, which include dry deposition but not exchange with the free troposphere (FT). The relatively short lifetime of HCHO (50-100 min) implies substantial BL-FT exchange. The mixing-in of FT air affected by African and South American biomass burning at an estimated rate of 0.12 h super(− 1) increases the CO and lowers the HCHO mixing ratios, leading to a better agreement with measurements. A 24 h mean deposition velocity of 1.35 cm/s for H sub(2)O sub(2) over the ocean as well as over the rainforest is deduced assuming BL-FT exchange adequate to the results for CO. The measured increase of the organic peroxides from the ocean to the rainforest (≈ 0.66 nmol/mol d super(− 1)) is significantly overestimated by the Lagrangian model, even when using high values for the deposition velocity and the entrainment rate. Our results point at either heterogeneous loss of organic peroxides and/or their radical precursors or a missing reaction path of peroxy radicals not forming peroxides in isoprene chemistry. We calculate a mean integrated daytime net ozone production (NOP) in the BL of (0.2 plus or minus 5.9) nmol/mol (ocean) and (2.4 plus or minus 2.1) nmol/mol (rainforest). The NOP strongly correlates with NO and shows a positive tendency in the boundary layer over the rainforest.