Atmospheric Chemistry: Report of the Dahlem Workshop on by E. D. Goldberg (auth.), E. D. Goldberg (eds.)

By E. D. Goldberg (auth.), E. D. Goldberg (eds.)

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Additional info for Atmospheric Chemistry: Report of the Dahlem Workshop on Atmospheric Chemistry, Berlin 1982, May 2 – 7

Sample text

One such modification is the enrichment of N0 3 - and SO~- often observed in salt particles, sometimes in conjunction with a CI- deficiency. Enrichment is usually given the symbol E, and can be defined as E X Y( ) - (X/Y) air (X/Y) seawater (4) Y is a species characteristic of seawater that passes across the air-sea interface without enrichment. E > 1 implies en- richment of X in the atmosphere relative to seawater, while E = 1 implies no enrichment and a seawater source for X. P. Ayers Island (44 0 S) (3).

Stockholm) 22: 89-134. 1872. Air and Rain. London: Longmans, Aquatic Chemistry. 1976. Nitrogen, SCOPE Report 7. Atmospheric Chemistry, ed. D. Goldberg, pp. 41-56. Berl in, Heidelberg, New York: Springer-Verlag. Dahlem Konferenzen 1982. The Chemical Composition of Precipitation: A Southern Hemisphere Perspective G. Ayers Division of Cloud Physics, CSIRO Sydney, Australia Abstract. Measurements made in the Australian region form the basis for a discussion on the chemical composition of preclpltation.

3%, see Eq. 2. CNitrate loadings for southern maritime atmosphere taken from GAMETAG results (14). dObserved long-term mean gas concentration at Cape Grim (2). 49 The Chemical Composition of Precipitation be said to be of the same order as the nitrate levels in Table 1. This is similar for the sulfate levels; in fact, the total sulfate enrichment that would be deduced from the predictions is the same as that found by Andreae in aerosol samples at Cape Grim. On the other hand, the predicted ammonia concentration seems too high in comparison with those of Table 1.

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