@article {2523,
	title = {Constraining Holocene 10Be production rates in Greenland},
	journal = {Journal of Quaternary Science},
	volume = {27},
	year = {2012},
	month = {Jan-01-2012},
	pages = {2 - 6},
	abstract = {The absence of a production rate calibration experiment on Greenland has limited the ability to link 10Be exposure dating chronologies of ice-margin change to independent records of rapid climate change. We use radiocarbon age control on Holocene glacial features near Jakobshavn Isbr{\ae}, western Greenland, to investigate 10Be production rates. The radiocarbon chronology is inconsistent with the 10Be age calculations based on the current globally averaged 10Be production rate calibration data set, but is consistent with the 10Be production rate calibration data set from north-eastern North America, which includes a calibration site nearby on north-eastern Baffin Island. Based on the best-dated feature available from the Jakobshavn Isbr{\ae} forefield, we derive a 10Be production rate value of 3.98 {\textpm} 0.24 atoms g a-1, using the {\textquoteleft}St{\textquoteright} scaling scheme, which overlaps with recently published reference 10Be production rates. We suggest that these 10Be production rate data, or the very similar data from north-eastern North America, are used on Greenland. Copyright {\textcopyright} 2011 John Wiley \& Sons, Ltd.},
	doi = {10.1002/jqs.1562},
	url = {http://doi.wiley.com/10.1002/jqs.1562},
	author = {Briner, Jason P. and Young, {\'a}s E. and Goehring, Brent M. and Schaefer, Joerg M.}
}
@article {2524,
	title = {Response of a marine-terminating Greenland outlet glacier to abrupt cooling 8200 and 9300 years ago},
	journal = {Geophysical Research Letters},
	volume = {38},
	year = {2011},
	month = {Apr-12-2013},
	pages = {n/a - n/a},
	abstract = {Long-term records of Greenland outlet-glacier change extending beyond the satellite era can inform future predictions of Greenland Ice Sheet behavior. Of particular relevance is elucidating the Greenland Ice Sheet{\textquoteright}s response to decadal- and centennial-scale climate change. Here, we reconstruct the early Holocene history of Jakobshavn Isbr{\ae}, Greenland{\textquoteright}s largest outlet glacier, using 10Be surface exposure ages and 14C-dated lake sediments. Our chronology of ice-margin change demonstrates that Jakobshavn Isbr{\ae} advanced to deposit moraines in response to abrupt cooling recorded in central Greenland ice cores ca. 8,200 and 9,300 years ago. While the rapid, dynamically aided retreat of many Greenland outlet glaciers in response to warming is well documented, these results indicate that marine-terminating outlet glaciers are also able to respond quickly to cooling. We suggest that short lag times of high ice flux margins enable a greater magnitude response of marine-terminating outlets to abrupt climate change compared to their land-terminating counterparts.},
	doi = {10.1029/2011GL049639},
	url = {http://doi.wiley.com/10.1029/2011GL049639},
	author = {Young, {\'a}s E. and Briner, Jason P. and Axford, Yarrow and Csatho, Beata and Babonis, Greg S. and Rood, Dylan H. and Finkel, Robert C.}
}
