@article{mcgee_he_2020, title={Mesoscale and submesoscale mechanisms behind asymmetric cooling and phytoplankton blooms induced by hurricanes: a comparison between an open ocean case and a continental shelf sea case (vol 68, pg 1443, 2018)}, volume={70}, ISSN={["1616-7228"]}, url={https://doi.org/10.1007/s10236-020-01371-7}, DOI={10.1007/s10236-020-01371-7}, abstractNote={The original version of this article unfortunately contained a mistake. The following data attribution statement per our research sponsors requirement has been omitted.}, number={6}, journal={OCEAN DYNAMICS}, publisher={Springer Science and Business Media LLC}, author={McGee, Laura and He, Ruoying}, year={2020}, month={Jun}, pages={843–843} }
 @article{mcgee_he_2018, title={Mesoscale and submesoscale mechanisms behind asymmetric cooling and phytoplankton blooms induced by hurricanes: a comparison between an open ocean case and a continental shelf sea case}, volume={68}, url={https://doi.org/10.1007/s10236-018-1203-3}, DOI={10.1007/s10236-018-1203-3}, abstractNote={Right-side bias in both sea surface cooling and phytoplankton blooms is often observed in the wake of hurricanes in the Northern Hemisphere. This idealized hurricane modeling study uses a coupled biological-physical model to understand the underlying mechanisms behind hurricane-induced cooling and phytoplankton bloom asymmetry. Both a deep ocean case and a continental shelf sea case are considered and contrasted. Model analyses show that while right-side asymmetric mixing due to inertial oscillations and restratification from strong right-side recirculation cells contributes to bloom asymmetry in the open ocean, the well-mixed condition in the continental shelf sea inhibits formation of recirculation cells, and the convergence of water onto the shelf is a more important process for bloom asymmetry.}, number={11}, journal={Ocean Dynamics}, publisher={Springer Science and Business Media LLC}, author={McGee, Laura and He, Ruoying}, year={2018}, month={Nov}, pages={1443–1456} }