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Sensitivity of sulfate direct climate forcing to the hysteresis of particle phase transitions Jun Wang, Andrew Hoffman, Scot Martin, Daniel Jacob Present.

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Presentation on theme: "Sensitivity of sulfate direct climate forcing to the hysteresis of particle phase transitions Jun Wang, Andrew Hoffman, Scot Martin, Daniel Jacob Present."— Presentation transcript:

1 Sensitivity of sulfate direct climate forcing to the hysteresis of particle phase transitions Jun Wang, Andrew Hoffman, Scot Martin, Daniel Jacob Present at 3rd GEOS–Chem Users' Meeting, April. 11, 2007

2 Introduction of sulfate phase & composition Solids: AS (NH 4 ) 2 SO 4 LET (NH 4 ) 3 H(SO 4 ) 2 AHS (NH 4 ) HSO 4 Aqueous: SO4aq SO 4 2-, H +, NH 4 +, H 2 O Extent of neutralization X= [NH 4 ]/2[SO 4 ] X = 1 X = 0.75 X = 0.5 0  X  1 Phase transition deliquesce Crystallization

3 To predict the phase transition requires: (a) Current phase (RH back-trajectory) which curve ? (b) RH in next time step which direction? (c) CRH(X) & DRH(X) Phase changes? The hysteresis of sulfate phase transition aqueous solids Aerosol phase transition Aerosol direct forcing on climate? Crystalline relative humidityDeliquesce relative humidity

4 CRH DRH Treatment of hysteresis effect in previous studies All previous forcing estimates diagnose the sulfate phase based on local RH only. A full consideration of the hysteresis loop has not been made in the past estimate of sulfate climate forcing. Chung et al., 2003  F: 18%, Haywood et al., 1997 24%, Martin et al., 2004 Limiting case studies

5 Approach Emission (SO 2 and NH 3 ) Deposition (dry and wet) Lab data Martin et al. (2003) CRH(x) SO 4 2- NH 4 + (NH 4 ) 3 H(SO 4 ) 2 (NH 4 ) HSO 4 (NH 4 ) 2 SO 4 DRH LET DRH AHS DRH AS aqueous solids Sulfate-water system Optical properties Wang & Martin (2007) Surface reflectance Koelemeijer et al. (2003) RTM (Fu & Liou, 1998) Forcing calculations GEOS-Chem CTM Park et al. (2003)

6 Model results % solids 23% 30% 45% 38% Global annual (natural + anthropogenic) burden: 1.938 mg SO 4 2- m -2 % of solids: 34%

7 13% 17% 29% 24% % solids Annual global: 0.017; solids: 21%. (natural + anthropogenic) sulfate aerosol optical thickness

8 optical thickness & full-sky forcing of anthropogenic aerosols Global & annual average of % Solids: 26% in , 31% in F clr, 37% in F fky. 16% 22% 36% 27% 26% 31% 47% 38% % solids

9 Sensitivity analysis to the hysteresis effect  : -14% F: -7%  : +10% F: +8%  : +5% F: +5%  : 19%  F: 12% (compared to base case; anthropogenic component only) Lower sideUpper side All aqueous “lower side” and “upper side” difference

10 Regional difference can be ~20%

11 Summary & Outlook Phase transition of sulfate aerosols is now developed in GEOS-Chem. For anthropogenic component only, solids contribute 26% to sulfate burden, 31% of clear-sky sulfate climate forcing, 37% of full-sky sulfate climate forcing, reflecting the correlation between solids and clear-sky conditions Hystereisis can result in the uncertainty in the forcing calculations by 12%. Using upper-side hysteresis loop overestimate forcing by +5%. Regional differences can be up to 20%. Future research is to look at the implication of modeled results for the study of cirrus cloud formation and modeling of O 3.

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13 Sensitivity to other compounded factors compositionhysteresis  F (NH 4 ) 2 SO 4 yes-2%+4% (NH 4 ) 2 SO 4 Upper side5%9% (NH 4 ) 2 SO 4 Upper side Backscattered fraction of aqueous = that of solids 5%25.9%

14 Full-sky (anthropogenic) sulfate direct climate forcing F fky = F clr × cloud fraction Annual global: 0.17 Wm -2 Solids: 37% F fky_sd /F clry_sd = 0.5 F fky_aq /F clr_aq = 0.4


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