Clifford A Barnes
Biographic Data
| ID | 10830416 |
|---|---|
| NAME | Clifford A Barnes |
| GIVEN NAMES | Clifford A |
| FAMILY NAME | Barnes |
| SIGNATURE | BARNES C A |
| AFFILIATIONS | Instituto Español de Oceanografía |
| VERIFIED | No |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 4 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1961 |
| LATEST PUBLICATION YEAR | 2001 |
| H-INDEX | 0 |
Vaudeville
The Movement of Atlantic Water in the Arctic Ocean
Re-evaluates sixty years' oceanographic data from the Arctic Ocean, examining nearly 300 deep-water stations, and using the "core-layer" method of Wust to interpret the movement of the Atlantic layer. Stations are grouped in 16 areas and the average curve for each group plotted on a temperature-salinity diagram. Temperature and salinity changes which take place in the Atlantic water while and entity in the Arctic Basin are graphed. The temperatur…
Surface Water in the Eurasian Basin of the Arctic Ocean
Reports results of re-appraisal and interpretation of data from 74 oceanographic stations (of >400 occupied), listed according to vessel and source. Surface water occupies the uppermost 200 m It is almost continuously supplied by continental runoff from Siberia which mixes with and collects saline water, to a few hundred times its original volume, as it crosses the arctic shelf seas. The surface water then flows directly to the exit from the basi…
The Contribution of Bering Sea Water to the Arctic Ocean
Summarizes the characteristics, especially temperature-salinity of these waters as they flow north through Bering Strait, and as they modify the surface water, deeper water, and ice cover of the western Arctic Ocean. Analysis of about 200 deep-water stations reveals regularity in the vertical distribution of temperature and salinity. The shallow 75-100 m depth, temperature maximum observed in the western as distinct from the eastern Arctic Basin …
No prominent works on this page.
The Contribution of Bering Sea Water to the Arctic Ocean
Summarizes the characteristics, especially temperature-salinity of these waters as they flow north through Bering Strait, and as they modify the surface water, deeper water, and ice cover of the western Arctic Ocean. Analysis of about 200 deep-water stations reveals regularity in the vertical distribution of temperature and salinity. The shallow 75-100 m depth, temperature maximum observed in the western as distinct from the eastern Arctic Basin …
Surface Water in the Eurasian Basin of the Arctic Ocean
Reports results of re-appraisal and interpretation of data from 74 oceanographic stations (of >400 occupied), listed according to vessel and source. Surface water occupies the uppermost 200 m It is almost continuously supplied by continental runoff from Siberia which mixes with and collects saline water, to a few hundred times its original volume, as it crosses the arctic shelf seas. The surface water then flows directly to the exit from the basi…
The Movement of Atlantic Water in the Arctic Ocean
Re-evaluates sixty years' oceanographic data from the Arctic Ocean, examining nearly 300 deep-water stations, and using the "core-layer" method of Wust to interpret the movement of the Atlantic layer. Stations are grouped in 16 areas and the average curve for each group plotted on a temperature-salinity diagram. Temperature and salinity changes which take place in the Atlantic water while and entity in the Arctic Basin are graphed. The temperatur…
Vaudeville
Arctic (3 works) · Arctic and Antarctic ice dynamics (3 works) · Geological Studies and Exploration (3 works) · Geology (3 works) · Geology (3 works) · Oceanography (3 works) · Oceanography (3 works) · Salinity (3 works) · Advection (2 works) · Circumpolar deep water (2 works)