@article {RN40,
	title = {Episodic Southern Ocean Heat Loss and Its Mixed Layer Impacts Revealed by the Farthest South Multiyear Surface Flux Mooring},
	journal = {Geophysical Research Letters},
	volume = {45},
	number = {10},
	year = {2018},
	pages = {5002-5010},
	type = {Journal Article},
	abstract = {The Ocean Observatories Initiative air-sea flux mooring deployed at 54.08{\textdegree}S, 89.67{\textdegree}W, in the southeast Pacific sector of the Southern Ocean, is the farthest south long-term open ocean flux mooring ever deployed. Mooring observations (February 2015 to August 2017) provide the first in situ quantification of annual net air-sea heat exchange from one of the prime Subantarctic Mode Water formation regions. Episodic turbulent heat loss events (reaching a daily mean net flux of -294 W/m2) generally occur when northeastward winds bring relatively cold, dry air to the mooring location, leading to large air-sea temperature and humidity differences. Wintertime heat loss events promote deep mixed layer formation that lead to Subantarctic Mode Water formation. However, these processes have strong interannual variability; a higher frequency of 2 σ and 3 σ turbulent heat loss events in winter 2015 led to deep mixed layers (>300 m), which were nonexistent in winter 2016.},
	issn = {0094-8276},
	doi = {10.1029/2017gl076909},
	url = {<Go to ISI>://WOS:000435262000052},
	author = {Ogle, S. E. and Tamsitt, V. and Josey, S. A. and Gille, S. T. and Cerovecki, I. and Talley, L. D. and Weller, R. A.}
}
