The Mechanism of the 20°C Isotherm Depth Oscillations for the Bay of Bengal.

MLA

Sil, Sourav, and Arun Chakraborty. “The Mechanism of the 20°C Isotherm Depth Oscillations for the Bay of Bengal.” Marine Geodesy, vol. 35, no. 3, July 2012, pp. 233–45. EBSCOhost, https://doi.org/10.1080/01490419.2011.637865.

APA

Sil, S., & Chakraborty, A. (2012). The Mechanism of the 20°C Isotherm Depth Oscillations for the Bay of Bengal. Marine Geodesy, 35(3), 233–245. https://doi.org/10.1080/01490419.2011.637865

Chicago

Sil, Sourav, and Arun Chakraborty. 2012. “The Mechanism of the 20°C Isotherm Depth Oscillations for the Bay of Bengal.” Marine Geodesy 35 (3): 233–45. doi:10.1080/01490419.2011.637865.