Cite
Flow of the Ross Ice Shelf, Antarctica, is modulated by the ocean tide.
MLA
Brunt, Kelly M., et al. “Flow of the Ross Ice Shelf, Antarctica, Is Modulated by the Ocean Tide.” Journal of Glaciology, vol. 56, no. 195, Feb. 2010, pp. 157–61. EBSCOhost, https://doi.org/10.3189/002214310791190875.
APA
Brunt, K. M., King, M. A., Fricker, H. A., & Macayeal, D. R. (2010). Flow of the Ross Ice Shelf, Antarctica, is modulated by the ocean tide. Journal of Glaciology, 56(195), 157–161. https://doi.org/10.3189/002214310791190875
Chicago
Brunt, Kelly M., Matt A. King, Helen Amanda Fricker, and Douglas R. Macayeal. 2010. “Flow of the Ross Ice Shelf, Antarctica, Is Modulated by the Ocean Tide.” Journal of Glaciology 56 (195): 157–61. doi:10.3189/002214310791190875.