@article {2965,
	title = {In-phase millennial-scale glacier changes in the tropics and North Atlantic regions during the HoloceneAbstract},
	journal = {Nature Communications},
	volume = {13},
	year = {2022},
	month = {Jan-12-2022},
	abstract = {Based on new and published cosmic-ray exposure chronologies, we show that glacier extent in the tropical Andes and the north Atlantic regions (TANAR) varied in-phase on millennial timescales during the Holocene, distinct from other regions. Glaciers experienced an early Holocene maximum extent, followed by a strong mid-Holocene retreat and a re-advance in the late Holocene. We further explore the potential forcing of TANAR glacier variations using transient climate simulations. Since the Atlantic Meridional Overturning Circulation (AMOC) evolution is poorly represented in these transient simulations, we develop a semi-empirical model to estimate the {\textquotedblleft}AMOC-corrected{\textquotedblright} temperature and precipitation footprint at regional scales. We show that variations in the AMOC strength during the Holocene are consistent with the observed glacier changes. Our findings highlight the need to better constrain past AMOC behavior, as it may be an important driver of TANAR glacier variations during the Holocene, superimposed on other forcing mechanisms.},
	doi = {10.1038/s41467-022-28939-9},
	url = {https://www.nature.com/articles/s41467-022-28939-9},
	author = {Jomelli, V. and Swingedouw, D. and Vuille, M. and Favier, V. and Goehring, B. and Shakun, J. and Braucher, R. and Schimmelpfennig, I. and Menviel, L. and Rabatel, A. and Martin, L. C. P. and Blard, P.-H. and Condom, T. and Lupker, M. and Christl, M. and He, Z. and Verfaillie, D. and Gorin, A. and Auma{\^\i}tre, G. and Bourles, D. L. and Keddadouche, K.}
}
@article {2538,
	title = {Deepwater Formation in the North Pacific During the Last Glacial Termination},
	journal = {Science},
	volume = {329},
	year = {2010},
	month = {Sep-07-2010},
	pages = {200 - 204},
	abstract = {Between ~17,500 and 15,000 years ago, the Atlantic meridional overturning circulation weakened substantially in response to meltwater discharges from disintegrating Northern Hemispheric glacial ice sheets. The global effects of this reorganization of poleward heat flow in the North Atlantic extended to Antarctica and the North Pacific. Here we present evidence from North Pacific paleo surface proxy data, a compilation of marine radiocarbon age ventilation records, and global climate model simulations to suggest that during the early stages of the Last Glacial Termination, deep water extending to a depth of ~2500 to 3000 meters was formed in the North Pacific. A switch of deepwater formation between the North Atlantic and the North Pacific played a key role in regulating poleward oceanic heat transport during the Last Glacial Termination.},
	issn = {0036-8075},
	doi = {10.1126/science.1190612},
	url = {http://www.sciencemag.org/cgi/doi/10.1126/science.1190612},
	author = {Okazaki, Y. and Timmermann, A. and Menviel, L. and Harada, N. and Abe-Ouchi, A. and Chikamoto, M. O. and Mouchet, A. and Asahi, H.}
}
