The Overturning in the Subpolar North Atlantic Program (OSNAP) observing system, which was launched in the summer of 2014 comprises an integrated coast-to-coast array of two sections: OSNAP West, extending from the southeastern Labrador shelf to the southwestern tip of Greenland, and OSNAP East, extending from the southeastern tip of Greenland to the Scottish shelf.... Continue Reading →
The Atlantic Meridional Overturning Circulation (AMOC) is the Atlantic component of the global ocean conveyor belt, which is a large-scale ocean circulation system that connects the Arctic, Atlantic, Indian, and Pacific Oceans via the Southern Ocean. Predominantly driven by deep convection in the high-latitude North Atlantic Ocean, the AMOC carries heat, salt, carbon, and other... Continue Reading →
Online document-sharing service has revolutionized the way scientists share documents and interact with collaborators. Google Docs is probably the most widely used online document-sharing service. I use it almost every day for work and to share scientific paper drafts with coauthors. It is very convenient and facilitates collaboration between co-authors. For instance, a co-author can... Continue Reading →
Atlantic Niño, characterized by warm sea surface temperature (SST) anomalies in the eastern equatorial Atlantic, is the Atlantic counterpart of the Pacific El Niño. Due to its smaller size in zonal extent, it is often referred to as El Niño’s little brother. It was previously thought to have a limited regional influence on rainfall variability... Continue Reading →
Ice sheet melting from Greenland's glaciers accounts for an increasing proportion of global sea level rise, losing ~330 billion tonnes of ice per year during 2006-2018 (compared to ~120 billion tonnes of ice per year during 1901-1990). A new study published in Nature Communications examined recent changes at K.I.V Steenstrups Nordre Bræ (66.53°N, 34.57°W), a... Continue Reading →
As the surface ocean warms and polar ice sheets melt due to increasing anthropogenic greenhouse gases in the atmosphere, near-surface stratification is increasing almost everywhere, including the major deep water formation regions in the high-latitude North Atlantic and around Antarctica. As a result, the global Meridional Overturning Circulation (MOC), also known as the global ocean... Continue Reading →
Zhang, R., Sun, S., Chen, Z., Yang, H., & Wu, L. (2023). Rapid 21st century weakening of the Agulhas current in a warming climate. Geophys. Res. Lett., 50, e2022GL102070. https://doi.org/10.1029/2022GL102070: The Agulhas current is projected to slow down and become shallower during the rest of the 21st century, partly in response to the slowdown of... Continue Reading →
The Antarctic Bottom Water (AABW) is the densest water mass of the global ocean that covers about 30 ~ 40% of the global ocean volume with temperatures ranging from -0.8 to 2°C and salinities from 34.6 to 34.7 psu. It forms around Antarctica and spreads into the Southern Ocean and then into the Atlantic, Indian,... Continue Reading →
As a career scientist, I review scientific papers regularly, at least once every month. For instance, I reviewed a total of 18 papers in 2021, and many of them 2 ~ 3 times for revisions. I think I can speak for almost everyone that nobody really enjoys reviewing papers. We do it because it is... Continue Reading →
There are many siblings, cousins, and distant relatives of El Niño spanning the Pacific, Atlantic, and Indian Oceans who share a feature in common: ocean surface temperature anomalies along eastern boundaries linked to changes in the upwelling of cooler water from below. So far, climate scientists have identified a total of 14 members of this... Continue Reading →
Ocean to Climate 