Mooring temperature, salinity, fluor data from the Georges Crest mooring on Georges Bank from Oct. 1994 - Jan. 1995
Citable URI
https://hdl.handle.net/1912/24947As published
https://lod.bco-dmo.org/id/dataset/2507Date Created
2005-06-14Location
Georges Bank, Gulf of Maine, Northwest Atlantic Oceanwestlimit: -67.5423; southlimit: 41.4077; eastlimit: -67.5423; northlimit: 41.4077
DOI
10.1575/1912/bco-dmo.2507.1Abstract
Mooring temperature, salinity, fluor data from the Georges Crest mooring on Georges Bank from Oct. 1994 - Jan. 1995
For a complete list of measurements, refer to the full dataset description in the supplemental file 'Dataset_description.pdf'. The most current version of this dataset is available at: https://www.bco-dmo.org/dataset/2507
Description
Dataset: CR1994_T_S
Suggested Citation
Dataset: Irish, Jim, "Mooring temperature, salinity, fluor data from the Georges Crest mooring on Georges Bank from Oct. 1994 - Jan. 1995", 2019-12-06, DOI:10.1575/1912/bco-dmo.2507.1, https://hdl.handle.net/1912/24947
Except where otherwise noted, this item's license is described as Creative Commons Attribution 4.0
Related items
Showing items related by title, author, creator and subject.
-
Community production modulates coral reef pH and the sensitivity of ecosystem calcification to ocean acidification
(John Wiley & Sons, 2017-01-31)Coral reefs are built of calcium carbonate (CaCO3) produced biogenically by a diversity of calcifying plants, animals, and microbes. As the ocean warms and acidifies, there is mounting concern that declining calcification ... -
Mass coral mortality under local amplification of 2°C ocean warming
(Nature Publishing Group, 2017-03-23)A 2°C increase in global temperature above pre-industrial levels is considered a reasonable target for avoiding the most devastating impacts of anthropogenic climate change. In June 2015, sea surface temperature (SST) of ... -
Biomass offsets little or none of permafrost carbon release from soils, streams, and wildfire : an expert assessment
(IOPScience, 2016-03-07)As the permafrost region warms, its large organic carbon pool will be increasingly vulnerable to decomposition, combustion, and hydrologic export. Models predict that some portion of this release will be offset by increased ...
