HIGHLIGHTS
SUMMARY
A leading hypothesis is that changes in deep-water and/or ocean circulation have played a key role in MCV (for review, see McManus et_al, 2004; Alley, 2007; Henry et_al, 2016; Lynch-Stieglitz, 2017; Menviel et_al, 2020). Climate models of varying complexity have simulated millennial oscillations when forced by freshwater fluxes from melting ice (Stocker and Johnsen, 2003; Ganopolski and Rahmstorf, 2001; Timmermann et_al, 2003; Rahmstorf et_al, 2005), whereas others have emphasized the role of sea ice (Gildor and Tziperman, 2001; Sevellec and Fedorov, 2015; Li et_al, 2005, 2010) and/or ice shelf dynamics . . .
If you want to have access to all the content you need to log in!
Thanks :)
If you don't have an account, you can create one here.