Meridional Overturning Circulation Observed by the Overturning in the Subpolar North Atlantic Program (OSNAP) 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 publicati...
Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
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Other Authors: | , , |
Format: | Dataset |
Language: | unknown |
Published: |
Georgia Institute of Technology
2020
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Subjects: | |
Online Access: | http://hdl.handle.net/1853/63707 https://doi.org/10.35090/wa93-m688 |
Summary: | 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. NOTE: the corrected version of this dataset is available at https://doi.org/10.35090/gatech/65537 National Science Foundation OCE-1948335 |
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