Biogeochemical evolution of the carbon dioxide system in the waters of long-lived mesoscale eddies in the Northeast Pacific Ocean
- 30 April 2005
- journal article
- Published by Elsevier BV in Deep Sea Research Part II: Topical Studies in Oceanography
- Vol. 52 (7-8), 955-974
- https://doi.org/10.1016/j.dsr2.2005.01.001
Abstract
No abstract availableKeywords
This publication has 52 references indexed in Scilit:
- Heat and fresh water transport by eddies into the Gulf of AlaskaDeep Sea Research Part II: Topical Studies in Oceanography, 2005
- The decline and fate of an iron-induced subarctic phytoplankton bloomNature, 2004
- Physical Characteristics of Haida EddiesJournal of Oceanography, 2002
- Mesoscale eddy aswirl with data in Gulf of AlaskaEos, 1999
- Atmospheric iron supply and enhanced vertical carbon flux in the NE subarctic Pacific: Is there a connection?Global Biogeochemical Cycles, 1998
- Modelling the seasonal course of the upper ocean pCO2 (II). Validation of the model and sensitivity studiesTellus B: Chemical and Physical Meteorology, 1995
- The role of pH measurements in modern oceanic CO2-system characterizations: Precision and thermodynamic consistencyDeep Sea Research Part II: Topical Studies in Oceanography, 1995
- Redfield ratios of remineralization determined by nutrient data analysisGlobal Biogeochemical Cycles, 1994
- Variability in the inorganic carbon system over the southeastern Bering Sea shelf during spring 1980 and spring—summer 1981Continental Shelf Research, 1986
- Alkalinity changes generated by phytoplankton growth1Limnology and Oceanography, 1976