@article{howell_dynamic_2019,
	title = {The Dynamic Response of Sea Ice to Warming in the Canadian Arctic Archipelago},
	volume = {46},
	url = {https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2019GL085116},
	doi = {https://doi.org/10.1029/2019GL085116},
	abstract = {Abstract Ice arches in the Canadian Arctic Archipelago ({CAA}) block the inflow of Arctic Ocean ice for the majority of the year. A 22 year record (1997–2018) of Arctic Ocean-{CAA} ice exchange was used to investigate the effect of warming on {CAA} sea ice dynamics. Larger ice area flux values were associated with longer flow duration and faster ice speed facilitated by increased open water leeway from the {CAA}'s transition to a younger and thinner ice regime, which together have contributed to a significant ice area flux increase (103 km2/year) from Arctic Ocean into the northern {CAA} from 1997 to 2018. Remarkably, the 2016 Arctic Ocean ice area flux into the {CAA} (161 × 103 km2) was 7 times greater than the 1997–2018 average (23 × 103 km2) and almost double the 2007 ice area flux into Nares Strait (87 × 103 km2). Continued warming may result in the {CAA} becoming a larger outlet for Arctic Ocean ice area loss.},
	pages = {13119--13125},
	number = {22},
	journaltitle = {Geophysical Research Letters},
	author = {Howell, Stephen E. L. and Brady, Mike},
	date = {2019-11-13},
	note = {\_eprint: https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL085116},
	keywords = {sea ice, area flux, dynamics, volume flux, Arctic Ocean, Canadain Arctic Archipelago},
}