Cruise report Chain 112, leg VI : 24 June - 9 July 1973
Citable URI
https://hdl.handle.net/1912/10751DOI
10.1575/1912/10751Abstract
Leg VI of CHAIN 112 was scheduled from 24 June to 9 July, St. Georges, Bermuda to Woods Hole. The original plans called for the following work: Recovery of sixteen intermediate moorings at the MODE site
(28° N., 69° 40'W.) Recovery of three subsurface moorings in the MODE area for
the University of Rhode Island. Launching of two new intermediate moorings at the MODE site. Bathymetric and meteorological observations in the MODE area. Bathymetry at Site D. Acoustic checks of three intermediate moorings at Site D. CTDs at each mooring recovery and setting
Collections
Suggested Citation
Heinmiller, R. H. (1973). Cruise report Chain 112, leg VI: 24 June - 9 July 1973. Woods Hole Oceanographic Institution. https://doi.org/10.1575/1912/10751Related items
Showing items related by title, author, creator and subject.
-
Ocean Network Information Center (OCEANIC) developing an online ocean information system
Churgin, James (IAMSLIC, 1989) -
Understanding the ocean carbon and sulfur cycles in the context of a variable ocean : a study of anthropogenic carbon storage and dimethylsulfide production in the Atlantic Ocean
Levine, Naomi M. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 2010-02)Anthropogenic activity is rapidly changing the global climate through the emission of carbon dioxide. Ocean carbon and sulfur cycles have the potential to impact global climate directly and through feedback loops. Numerical ... -
Air-sea CO2 fluxes and the controls on ocean surface pCO2 seasonal variability in the coastal and open-ocean southwestern Atlantic Ocean : a modeling study
Arruda, R.; Calil, Paulo H. R.; Bianchi, A. A.; Doney, Scott C.; Gruber, Nicolas; Lima, Ivan D.; Turi, G. (Copernicus Publications on behalf of the European Geosciences Union, 2015-10-12)We use an eddy-resolving, regional ocean biogeochemical model to investigate the main variables and processes responsible for the climatological spatio-temporal variability of pCO2 and the air-sea CO2 fluxes in the ...