@article {RN126,
	title = {USING AUTHENTIC DATA FROM NSF{\textquoteright}S OCEAN OBSERVATORIES INTIATIVE IN UNDERGRADUATE TEACHING An Invitation},
	journal = {Oceanography},
	volume = {33},
	number = {1},
	year = {2020},
	pages = {62-73},
	type = {Journal Article},
	abstract = {There are many benefits to using real data in undergraduate science education, including building analytical and problem-solving skills and visualizing concepts through real-world examples. The Ocean Observatories Initiative (OOI) provides a unique source of continuous, long-term oceanographic data from multiple locations in the world ocean. Each of these arrays hosts a suite of co-located instruments that measure physical, chemical, geological, and biological properties. Existing educational resources derived from OOI data can be leveraged for undergraduate teaching activities in and beyond the classroom. We provide example applications of the use of OOI resources in lesson plans and in research experiences for undergraduates. There are also abundant opportunities for new resources to be developed by the community. Our goal is to guide educators in determining appropriate OOI data sets and applications for their own needs.

},
	issn = {1042-8275},
	doi = {10.5670/oceanog.2020.103},
	author = {Greengrove, C. and Lichtenwalner, C. S. and Palevsky, H. I. and Pfeiffer-Herbert, A. and Severmann, S. and Soule, D. and Murphy, S. and Smith, L. M. and Yarincik, K.}
}
@article {RN21,
	title = {The North Atlantic Biological Pump INSIGHTS FROM THE OCEAN OBSERVATORIES INITIATIVE IRMINGER SEA ARRAY},
	journal = {Oceanography},
	volume = {31},
	number = {1},
	year = {2018},
	pages = {42-49},
	type = {Journal Article},
	abstract = {The biological pump plays a key role in the global carbon cycle by transporting photosynthetically fixed organic carbon into the deep ocean, where it can be sequestered from the atmosphere over annual or longer time scales if exported below the winter ventilation depth. In the subpolar North Atlantic, carbon sequestration via the biological pump is influenced by two competing forces: a spring diatom bloom that features large, fast-sinking biogenic particles, and deep winter mixing that requires particles to sink much further than in other ocean regions to escape winter ventilation. We synthesize biogeochemical sensor data from the first two years of operations at the Ocean Observatories Initiative Irminger Sea Array of moorings and gliders (September 2014{\textendash}July 2016), providing the first simultaneous year-round observations of biological carbon cycling processes in both the surface ocean and the seasonal thermocline in this critical but previously undersampled region. These data show significant mixed layer net autotrophy during the spring bloom and significant respiration in the seasonal thermocline during the stratified season (~5.9 mol C m{\textendash}2 remineralized between 200 m and 1,000 m). This respired carbon is subsequently ventilated during winter convective mixing (>1,000 m), a significant reduction in potential carbon sequestration. This highlights the importance of year-round observations to accurately constrain the biological pump in the subpolar North Atlantic, as well as other high-latitude regions that experience deep winter mixing.},
	issn = {1042-8275},
	doi = {10.5670/oceanog.2018.108},
	url = {<Go to ISI>://WOS:000427367300008},
	author = {Palevsky, H. I. and Nicholson, D. P.}
}
