Sea-ice meltwater and excess alkalinity in the East Greenland Current
By: F.C. Tan
Contributors: Dyrssen, D.; Strain, P. M.
Published: 1983
Language: eng
Number of pages: 283
Description: Relationship assessed by means of oxygen isotope method. Results indicate sea ice contributes only 25% of excess alkalinity (compared to 100% in West Spitsbergen Current). Principle source must be river inputs to Arctic Ocean.
Notes: References:p.288.