Figures and movies from the first paper:

BCabsoptdaily.gif is an animation of the smoke distribution as it is spread around the world by the winds.  The smoke is heated by absorbing sunlight, lofted into the upper stratosphere, and blown into the Southern Hemisphere.

BCabsopred.gif is the same animation as BCabsoptdaily.gif, but in red.

BCabsoptdailyheight.gif contains the same animation as BCabsoptdaily.gif, but also includes a graph at the side that shows the vertical distribution of the smoke.  Within the first week the smoke in the troposphere, the lowest atmospheric layer, is lofted or washed out, and the remaining smoke is lofted well into the stratosphere, removed from weather where it can remain for years.  The black horizontal line at about 150 mb marks the boundary between the troposphere and stratosphere, at about 12 km (7 miles).  The top of the stratosphere (at 50 km or 30 miles) has a pressure of about 1 mb.

Fig3TempPrecip.jpg  Time variation of global average net surface shortwave radiation, surface air temperature, and precipitation changes for the 5 Tg standard case.  The global average precipitation in the control case is 3.0 mm/day, so the changes in years 2-4 represent a 9% global average reduction in precipitation.  The precipitation recovers faster than the temperature, but both lag the forcing.  For comparison the global average net surface shortwave forcing from a model simulation of the 1991 Mt. Pinatubo eruption is shown.  By contrast, volcanic particle last for a much shorter time in the atmosphere, as they are not lofted by solar absorption.

Fig5SummerTempMap.jpg  Surface air temperature changes for the 5 Tg standard case averaged for June, July, and August of the first year following the smoke injection.  Effects are largest over land, but there is substantial cooling over tropical oceans, too.  The warming over Antarctica is for a small area, is part of normal winter interannual variability, and is not significant.

Fig9GISStemperatures.jpg  Global average surface air temperature change from the 5 Tg standard case (red) in the context of the climate change of the past 125 years.  Observations are from the NASA Goddard Institute for Space Studies analysis (Hansen et al., 2001, updated at http://data.giss.nasa.gov/gistemp/2005/).

Fig10HockeyStick.jpg  Northern Hemisphere average surface air temperature change from 5 Tg standard case (red) in the context of the climate change of the past 1000 years.  Black curve is from Mann et al. (1999), and the blue curve is from the latest data from the Climatic Research Unit website (http://www.cru.uea.ac.uk/cru/data/temperature/).

Fig11GrowingSeason.jpg  Change in growing season (period with freeze-free days) in the first year following the 5 Tg standard case smoke injection. 

References

Hansen, J. E., et al., 2001: A closer look at United States and global surface temperature change, J. Geophys. Res., 106, 23,947-23,963, doi:10.1029/2001JD000354.

Mann, M. E., R. S. Bradley, and M. K. Hughes, 1999: Northern Hemisphere temperatures during the past millennium: Inferences, uncertainties, and limitations, Geophys. Res. Lett., 26, 759-762.