1. Diffusive vertical heat flux in the Canada Basin of the Arctic Ocean inferred from moored instruments. Issue 1 (22nd January 2014) Authors: Lique, Camille; Guthrie, John D.; Steele, Michael; Proshutinsky, Andrey; Morison, James H.; Krishfield, Richard Journal: Journal of geophysical research Issue: Volume 119:Issue 1(2014:Jan.) Page Start: 496 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
2. Proxy representation of Arctic ocean bottom pressure variability: Bridging gaps in GRACE observations. Issue 17 (14th September 2016) Authors: Peralta‐Ferriz, Cecilia; Morison, James H.; Wallace, John M. Journal: Geophysical research letters Issue: Volume 43:Issue 17(2016) Page Start: 9183 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
3. Revisiting internal waves and mixing in the Arctic Ocean. Issue 8 (22nd August 2013) Authors: Guthrie, John D.; Morison, James H.; Fer, Ilker Journal: Journal of geophysical research Issue: Volume 118:Issue 8(2013:Aug.) Page Start: 3966 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
4. Sea ice melt onset associated with lead opening during the spring/summer transition near the North Pole. Issue 4 (13th April 2016) Authors: Vivier, Frédéric; Hutchings, Jennifer K.; Kawaguchi, Yusuke; Kikuchi, Takashi; Morison, James H.; Lourenço, Antonio; Noguchi, Tomohide Journal: Journal of geophysical research Issue: Volume 121:Issue 4(2016:Apr.) Page Start: 2499 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗
5. Thermohaline staircases in the Amundsen Basin: Possible disruption by shear and mixing. Issue 10 (5th October 2017) Authors: Guthrie, John D.; Fer, Ilker; Morison, James H. Journal: Journal of geophysical research Issue: Volume 122:Issue 10(2017) Page Start: 7767 Record Type: Journal Article View Content: Available online (eLD content is only available in our Reading Rooms) ↗