Precipitation Composition and Its Variability in the Southern Indian Ocean' Amsterdam Island, 1980-1987

• Published in: Journal of Geophysical Research
• Main Authors: Moody, J., Pszenny, A., Gaudry, A., Keene, W., Galloway, J., Polian, G.
• Other Authors: NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML), National Oceanic and Atmospheric Administration (NOAA), Centre des Faibles Radioactivités, Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 1991
• Subjects: [SDU.OCEAN]Sciences of the Universe [physics]/Ocean; Atmosphere; [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces; environment; Indian; Amsterdam Island
• Online Access: https://hal.science/hal-03583323; https://hal.science/hal-03583323/document; https://hal.science/hal-03583323/file/Journal%20of%20Geophysical%20Research%20Atmospheres%20-%2020%20November%201991%20-%20Moody%20-%20Precipitation%20composition%20and%20its%20variability%20in.pdf; https://doi.org/10.1029/91JD01921

International audience Event precipitation samples have been collected on Amsterdam Island (3f 47' S, 77 • 31' E) from May 1980 through January 1987 and analyzed for SOn-, NO•-, CF, Na + , Mg ++ , I•, Ca ++ , I-1', HCOOt, and CH• COO t. The objective of this paper is to assess the processes which influence variability in the chemical composition of precipitation at this remote marine site. Back trajectories and gas phase 222 Rn measurements were used to identify source regions and their relative contributions to precipitation composition. The technique of cluster analysis was applied to trajectory data as a method for determining to what degree different atmospheric flow patterns influence variability in the obse•d composition. The dominant source regions for chemical deposition were found to be Madagascar and/or S.E. Africa and the ocean region north and east of Amsterdam Island. A strong seasonal signal in the precipitation composition is illustrated. Processes which influence variability in the chemical composition include the following: seasonality in the source strength of biogenic precursors for non-sea-salt (mss) SOn-, NI• + and carboxylic acids; seasonality in biomass-burning conlinental sources for the concentration of NO a-and a portion of riss CF; and variations in source region driven by daily changes in meteorology, as well as seasonal and annual differences in transport and removal patterns. In addition, interannual differences in riss SOn-concentration appear to be related to fluctuations in large-scale circulation patterns as defined by the Southern Oscillation.