J. M. Oberhuber

Publication List Details

Period

1992 - 2006

Number

14

Co-Authors

Potential feedback mechanism between phytoplankton and upper ocean circulation with oceanic radiative transfer processes influenced by phytoplankton - Numerical ocean, general circulation models and an analytical solution (2006)

Nakamoto, S., Kano, M., PrasannaKumar, S., Oberhuber, J.M., Muneyama, K., Ueyoshi, K., ...

Because of the diversity of the ecosystem in the earth, modeling of such an ecosystem cannot avoid arguing which ecosystem element should be included or excluded. It is demonstrated that views of...

A prognostic turbulence scheme for the nonhydrostatic plume model ATHAM (2003)

Herzog,Michael, Oberhuber,J. M., Graf,Hans F.

The presented turbulence scheme was developed for the Active Tracer High-Resolution Atmospheric Model (ATHAM) to parameterize the effect of subgrid-scale turbulence. In contrast to the commonly used...

Injection of gases into the stratosphere by explosive volcanic eruptions (2003)

Textor,Christiane, Graf,Hans F., Herzog,Michael, Oberhuber,J. M.

Explosive eruptions can inject large amounts of volcanic gases into the stratosphere. These gases may be scavenged by hydrometeors within the eruption column, and high uncertainties remain regarding...

A prognostic turbulence scheme for the nonhydrostatic plume model ATHAM (2003)

Herzog, Michael, Oberhuber, J. M., Graf, Hans F.

The presented turbulence scheme was developed for the Active Tracer High-Resolution Atmospheric Model (ATHAM) to parameterize the effect of subgrid-scale turbulence. In contrast to the commonly used...

Injection of gases into the stratosphere by explosive volcanic eruptions (2003)

Textor, Christiane, Graf, Hans F., Herzog, Michael, Oberhuber, J. M.

Explosive eruptions can inject large amounts of volcanic gases into the stratosphere. These gases may be scavenged by hydrometeors within the eruption column, and high uncertainties remain regarding...

Chlorophyll modulation of mixed layer thermodynamics in a mixed-layer isopycnal General Circulation Model - An example from Arabian Sea and equatorial Pacific (2002)

Nakamoto, S., PrasannaKumar, S., Oberhuber, J.M., Saito, H., Muneyama, K., Frouin, R.

Western tropical Indian Ocean, Arabian Sea, and the equatorial Pacific are known as regions of intense bio-chemical-physical interactions: the Arabian Sea has the largest phytoplankton bloom with...

Upper ocean circulation modulation by phytoplankton concentration in the Equatorial Pacific and the Indian Ocean (2002)

Nakamoto, S., PrasannaKumar, S., Oberhuber, J.M., Sammarco, P., Muneyama, K., Sato, T., ...

Wind patterns in the equatorial Pacific and Indian oceans are the factors that regulate the chlorophyll pigment distributions in the equatorial region of these oceans. Trade winds and coastline of...

Response of the equatorial Pacific to chlorophyll pigment in a mixed layer isopycnal ocean general circulation model (2001)

Nakamoto, S., PrasannaKumar, S., Oberhuber, J.M., Ishizaka, J., Muneyama, K., Frouin, R.

The influence of phytoplankton on the upper ocean dynamics and thermodynamics in the equatorial Pacific is investigated using an isopycnal ocean general circulation model (OPYC) coupled with a mixed...

Chlorophyll modulation of mixed layer thermodynamics in a mixed-layer isopycnal general circulation model - An example from Arabian Sea and Equatorial Pacific (2000)

Nakamoto, S., PrasannaKumar, S., Oberhuber, J.M., Saito, H., Muneyama, K.

Western Tropical Indian Ocean, Arabian Sea and equatorial Pacific are known to be regions of intense bio-chemical-physical interactions with Arabian sea being largest in seasonal phytoplankton bloom...