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Sulfur cycle and sulfate radiative forcing simulated from a coupled global climate-chemistry model

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Table 1. Gaseous- and aqueous-phase reactions considered in the sulfur cycle.
Table 2. SO 2 global emission used in GCCM.
Table 4. Differences of global-mean radiative forcing (in W m −2 ) between simulations at the surface and top of atmosphere (TOA) under both clear-sky and all-sky conditions.
Table 5. Simulated shortwave radiative forcing and meteorological responses over the globe.
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