Meridional Heat and Salinity Transports and the Surface Freshwater Exchange Derived from the OSNAP (Overturning in the Subpolar North Atlantic Program) Array between August 2014 and May 2018

Data from the full OSNAP array for the first 4 years between 2014 and 2018 have been used to produce the 30-day mean meridional heat (MHT) and salinity transports (MST), and the derived surface freshwater (FW) exchange time series.Related article: Observation-based estimates of heat and freshwater exchanges from the subtropical North Atlantic to the ArcticAn international effort, Overturning in the Subpolar North Atlantic Program (OSNAP), is a partnership among oceanographers from the US, UK, Germany, the Netherlands, Canada and China whose goal is to measure and understand what drives the subpolar overturning circulation and its associated property exchanges. OSNAP is consisted of more than 53 moorings that stretch from Labrador to Greenland to Scotland, providing a continuous record of the full water column, trans-basin velocity, temperature and salinity in the subpolar North Atlantic. Data from the full OSNAP array for the first 4 years between 2014 and 2018 have been used to produce the 30-day mean meridional heat (MHT) and salinity transports (MST), and the derived surface freshwater (FW) exchange time series.National Science Foundation Award Number 194833

Meridional Overturning Circulation Observed by the OSNAP (Overturning in the Subpolar North Atlantic Program) Array from August 2014 to May 2018 - Originally published data

Strength of the Meridional Overturning Circulation across the OSNAP array, defined as the maximum of the streamfunction in density space.The project scientists would appreciate it if you would use the data DOI https://doi.org/10.35090/wa93-m688 and add the following acknowledgement to any publication that use this data: “OSNAP data were collected and made freely available by the OSNAP (Overturning in the Subpolar North Atlantic Program) project and all the national programs that contribute to it (www.o-snap.org).”NOTE: This item is replaced by http://hdl.handle.net/1853/65537. An error was detected in this original dataset.An international effort, Overturning in the Subpolar North Atlantic Program (OSNAP), is a partnership among oceanographers from the US, UK, Germany, the Netherlands, Canada and China whose goal is to measure and understand what drives the Atlantic Meridional Overturning Circulation (MOC) and its variability. OSNAP is consisted of more than 53 moorings that stretch from Labrador to Greenland to Scotland, providing a continuous record of the full water column, trans-basin volume transports in the subpolar North Atlantic. The first 4 years of data (August 2014 - May 2018) from the full OSNAP array has been used to produce the 30-day mean estimates of the MOC at OSNAP. All data are freely available from www.o-snap.org. The corrected version of this dataset is available at https://doi.org/10.35090/gatech/65537National Science Foundation Award Number 194833

Meridional Overturning Circulation Observed by the OSNAP (Overturning in the Subpolar North Atlantic Program) Array from August 2014 to May 2018

This item replaces a previous published version of the data with persistent identifiers: http://hdl.handle.net/1853/63707 and https://doi.org/10.35090/wa93-m688The project scientists would appreciate it if you would use the data DOI https://doi.org/10.35090/gatech/65537 and add the following acknowledgement to any publication that use this data: “OSNAP data were collected and made freely available by the OSNAP (Overturning in the Subpolar North Atlantic Program) project and all the national programs that contribute to it (www.o-snap.org).”Strength of the Meridional Overturning Circulation across the OSNAP array, defined as the maximum of the streamfunction in density space.An international effort, Overturning in the Subpolar North Atlantic Program (OSNAP), is a partnership among oceanographers from the US, UK, Germany, the Netherlands, Canada and China whose goal is to measure and understand what drives the Atlantic Meridional Overturning Circulation (MOC) and its variability. OSNAP is consisted of more than 53 moorings that stretch from Labrador to Greenland to Scotland, providing a continuous record of the full water column, trans-basin volume transports in the subpolar North Atlantic. The first 4 years of data (August 2014 - May 2018) from the full OSNAP array has been used to produce the 30-day mean estiamtes of the MOC at OSNAP. All data are freely available from www.o-snap.org. item_description: Strength of the Meridional Overturning Circulation across the OSNAP array, defined as the maximum of the streamfunction in density space. The original version of this dataset is available at https://doi.org/10.35090/wa93-m688National Science Foundation Award No. 194833

Meridional overturning circulation observed by the OSNAP (Overturning in the Subpolar North Atlantic Program) array from August 2014 to May 2018

An international effort, Overturning in the Subpolar North Atlantic Program (OSNAP), is a partnership among oceanographers from the US, UK, Germany, the Netherlands, Canada and China whose goal is to measure and understand what drives the Atlantic Meridional Overturning Circulation (MOC) and its variability. OSNAP is consisted of more than 53 moorings that stretch from Labrador to Greenland to Scotland, providing a continuous record of the full water column, trans-basin volume transports in the subpolar North Atlantic. The first 4 years of data (August 2014 - May 2018) from the full OSNAP array has been used to produce the 30-day mean estimates of the MOC at OSNAP. All data are freely available from www.o-snap.org

Characteristics, management, and outcomes of patients with left‐sided infective endocarditis complicated by heart failure: a substudy of the ESC‐EORP EURO‐ENDO (European infective endocarditis) registry

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