Moored Buoys

The Southwest Atlantic Meridional Overturning Circulation (SAM) project collects measurements of the ocean boundary currents in the western South Atlantic Ocean.  This project is the cornerstone of an international trans-basin array measuring key flows associated with climate impact on heatwaves, droughts, hurricane intensification and more. The Southwest Atlantic MOC project serves the following data products produced […]

This page hosted by PMEL allows you to view customized plots or download data from Ocean Climate Stations that include GOMO-supported KEO and Papa moorings. The Kuroshio Extension Observatory (KEO) is located in the North Pacific’s western boundary current region, which is characterized by extremely large ocean heat losses to the atmosphere, and carbon dioxide

This page provides real-time data from the California Current Ecosystem 1 (CCE2) Mooring located on the shelf break on the California Coast.

This page provides real-time data from the California Current Ecosystem 1 (CCE1) Mooring located 250 km southwest of Point Conception California.

As part of the Eastern Pacific Investigation of Climate (EPIC) program, the UOP group has undertaken a study of Long-Term Evolution and Coupling of the Boundary layers in the Stratus Deck regions of the eastern tropical Pacific. The goal of the Stratus project is to observe and understand air-sea interactions and the surface forcing in

The Northwest Tropical Atlantic Station (NTAS) project for air-sea flux measurement was conceived in order to investigate surface forcing and oceanographic response in a region of the tropical Atlantic with strong SST anomalies and the likelihood of significant local air-sea interaction. This page provides access to real-time and archived data of in-situ fluxes of heat,

In cooperation with the Hawaii Ocean Timeseries (HOT) project, the UOP Group has undertaken moored observations of surface forcing in the central Pacific. The primary intent of the WHOI HOT Station (WHOTS) is to provide long-term, high-quality air-sea fluxes as a coordinated part of the HOT program, and contribute to the HOT goals of observing