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Interannual Variability of Antarctic Intermediate Water in the Tropical North Atlantic

Published in Journal of Geophysical Research: Oceans, 2019

This paper highlights the role of western boundary current system in the interannual variability of the Antarctic Intermediate Water in the tropical Northwestern Atlantic.

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A stable Atlantic Meridional Overturning Circulation in a changing North Atlantic since the 1990s

Published in Science Advances, 2020

The Atlantic Meridional Overturning Circulation (AMOC) and water mass property changes in the north Atlantic are jointly studied using a compilation of hydrographic section data, array observation, satellite altimetry, and ocean syntheses pruduct. The results indicate that water mass property and overturning circulation do not vary at the same pace, suggesting a higher degree of decoupling between the two processes than we previously expect.

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Representation of the mean Atlantic Subtropical Cells in CMIP6 models

Published in Journal of Geophysical Research: Oceans, 2022

The Atlantic Subtropical Cells (STCs) consist of poleward Ekman transport in the surface layer, subduction in the subtropics, and equatorward transport in the thermocline layer that largely compensates the surface Ekman divergence and closes the STCs via equatorial upwelling. As a result, the STCs play an important role in connecting the tropical and subtropical Atlantic Ocean, in terms of heat, freshwater, oxygen, and nutrients exchange. In this study, we evaluated the performance of CMIP6 climate models in simulation the Atlantic STCs…

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Seasonality of the Meridional Overturning Circulation in the Subpolar North Atlantic

Published in Communications Earth & Environment, 2023

Understanding the variability of the Atlantic Meridional Overturning Circulation is essential for better predictions of our changing climate. Here we present an updated time series (August 2014 to June 2020) from the Overturning in the Subpolar North Atlantic Program (OSNAP). The 6-year time series allows us to observe the seasonality of the subpolar overturning and meridional heat and freshwater transports. The overturning peaks in late spring and reaches a minimum in early winter, with a peak-to-trough range of 9.0 Sv. The overturning seasonal timing can be explained by winter transformation and the export of dense water, modulated by a seasonally varying Ekman transport.

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Talk 1 on Relevant Topic in Your Field

Published: March 01, 2012

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Tutorial 1 on Relevant Topic in Your Field

Published: March 01, 2013

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Talk 2 on Relevant Topic in Your Field

Published: February 01, 2014

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Conference Proceeding talk 3 on Relevant Topic in Your Field

Published: March 01, 2014

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Teaching experience 1

Undergraduate course, University 1, Department, 2014

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Teaching experience 2

Workshop, University 1, Department, 2015

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