https://link.springer.com/article/10.1007/s00382-023-06799-3
This new paper in Climate Dynamics is relevant to stratospheric sulfate aerosol geoengineering. The interhemispheric difference in forcing causes a sure signal in tropical monsoon systems. Some of you may be already well aware of this. In this new paper, we quantified this sensitivity for stratospheric sulfate aerosol loading. The northern hemispheric monsoon index changes by ~7% per 0.1 change in the AOD difference between the hemispheres and ~ 6% per 1 K change in temperature difference between the hemispheres. With Best Wishes, ------------------------------------------------------------------- G. Bala Professor Center for Atmospheric and Oceanic Sciences Indian Institute of Science Bangalore - 560 012 India Tel: +91 80 2293 3428; +91 80 2293 2505 Fax: +91 80 2360 0865; +91 80 2293 3425 Email: [email protected]; [email protected] Google Scholar <https://scholar.google.com/citations?user=eurjQPwAAAAJ> ------------------------------------------------------------------- -- You received this message because you are subscribed to the Google Groups "geoengineering" group. To unsubscribe from this group and stop receiving emails from it, send an email to [email protected]. To view this discussion on the web visit https://groups.google.com/d/msgid/geoengineering/CAD7fhVknfsmwjp928vREiCLdQmZ8k7RYD-BfD75paheXYip0mQ%40mail.gmail.com.
