This funding enabled the following published manuscripts in which we have developed models of direct relevance to ocean carbon sequestration and of the oceanic iron cycle, its connection to the global carbon cycle, and the sensitivity of atmospheric carbon dioxide to the external source of iron. As part of this process we have developed the adjoint of the MIT ocean biogeochemistry model which has enabled us to perform rigorous and efficient sensitivity studies
The first generation of open-ocean iron enrichments (1993 to 2005) have all had broadly the same des...
Numerical models of ocean biogeochemistry are relied upon to make projections about the impact of cl...
Author Posting. © American Geophysical Union, 2004. This article is posted here by permission of Am...
Under this grant, the authors investigated a range of issues associated with the proposal to fertili...
This final report summarizes research undertaken collaboratively between Princeton University, the N...
Recently, it was proposed (Baum, 1990 and Martin et al, 1990a, 1990b) that the southern ocean should...
The purpose of this workshop was to bring together the principal investigators of all the projects t...
Numerical models of ocean biogeochemistry are relied upon to make projections about the impact of cl...
This final report summarizes research undertaken collaboratively between Princeton University, the N...
Changes in the ocean iron cycle could help explain the low atmospheric CO2 during the Last Glacial M...
The role of iron in regulating the flux of carbon through the surface layer of the ocean has become ...
The ocean carbon cycle plays a fundamental role in the Earth’s climate system, on decadal to multi-m...
Marine biological production as well as the associated biotic uptake of carbon in many ocean regions...
I present a model investigation on the complex marine iron (Fe) cycle. Attention is put on regional ...
This paper briefly reviews the key processes that determine oceanic CO2 uptake and sets this descrip...
The first generation of open-ocean iron enrichments (1993 to 2005) have all had broadly the same des...
Numerical models of ocean biogeochemistry are relied upon to make projections about the impact of cl...
Author Posting. © American Geophysical Union, 2004. This article is posted here by permission of Am...
Under this grant, the authors investigated a range of issues associated with the proposal to fertili...
This final report summarizes research undertaken collaboratively between Princeton University, the N...
Recently, it was proposed (Baum, 1990 and Martin et al, 1990a, 1990b) that the southern ocean should...
The purpose of this workshop was to bring together the principal investigators of all the projects t...
Numerical models of ocean biogeochemistry are relied upon to make projections about the impact of cl...
This final report summarizes research undertaken collaboratively between Princeton University, the N...
Changes in the ocean iron cycle could help explain the low atmospheric CO2 during the Last Glacial M...
The role of iron in regulating the flux of carbon through the surface layer of the ocean has become ...
The ocean carbon cycle plays a fundamental role in the Earth’s climate system, on decadal to multi-m...
Marine biological production as well as the associated biotic uptake of carbon in many ocean regions...
I present a model investigation on the complex marine iron (Fe) cycle. Attention is put on regional ...
This paper briefly reviews the key processes that determine oceanic CO2 uptake and sets this descrip...
The first generation of open-ocean iron enrichments (1993 to 2005) have all had broadly the same des...
Numerical models of ocean biogeochemistry are relied upon to make projections about the impact of cl...
Author Posting. © American Geophysical Union, 2004. This article is posted here by permission of Am...