Jeffrey P Severinghaus
Datos Biográficos
| ID | 5597261 |
|---|---|
| NOMBRE | Jeffrey P Severinghaus |
| NOMBRES | Jeffrey P |
| APELLIDO | Severinghaus |
| FIRMA | SEVERINGHAUS J P |
| AFILIACIONES | Scripps Institution of Oceanography |
| ORCID | 0000-0001-8883-3119 |
| VERIFICADO | Sí |
| TOTAL DE OBRAS | 2 |
| TOTAL DE CITAS | 1 |
| TOTAL COMO AUTOR | 2 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 1996 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2007 |
| ÍNDICE H | 1 |
Pleistocene ice and paleo-strain rates at Taylor Glacier, Antarctica
Ice exposed in ablation zones of ice sheets can be a valuable source of samples for paleoclimate studies and information about long-term ice dynamics. We report a 28-km long stable isotope sampling transect along a flowline on lower Taylor Glacier, Antarctica, and show that ice from the last glacial period is exposed here over tens of kilometers. Gas isotope analyses on a small number of samples confirm our age hypothesis. These chronostratigraph…
Transect Along 24°n Latitude of 14 C in Dissolved Inorganic Carbon in the Subtropical North Atlantic Ocean
The distribution of bomb-produced 14 C in the ocean provides a powerful constraint for circulation models of upper ocean mixing. We report 14 C measurements from an east-west section of the main thermocline at 24°N latitude in the subtropical North Atlantic Ocean in summer 1992, and one profile from the Gulf of Mexico in 1993. Observed gradients reflect the transient invasion of bomb 14 C into the thermocline via mixing along isopycnals from the …
Transect Along 24°n Latitude of 14 C in Dissolved Inorganic Carbon in the Subtropical North Atlantic Ocean
The distribution of bomb-produced 14 C in the ocean provides a powerful constraint for circulation models of upper ocean mixing. We report 14 C measurements from an east-west section of the main thermocline at 24°N latitude in the subtropical North Atlantic Ocean in summer 1992, and one profile from the Gulf of Mexico in 1993. Observed gradients reflect the transient invasion of bomb 14 C into the thermocline via mixing along isopycnals from the …
Transect Along 24°n Latitude of 14 C in Dissolved Inorganic Carbon in the Subtropical North Atlantic Ocean
The distribution of bomb-produced 14 C in the ocean provides a powerful constraint for circulation models of upper ocean mixing. We report 14 C measurements from an east-west section of the main thermocline at 24°N latitude in the subtropical North Atlantic Ocean in summer 1992, and one profile from the Gulf of Mexico in 1993. Observed gradients reflect the transient invasion of bomb 14 C into the thermocline via mixing along isopycnals from the …
Pleistocene ice and paleo-strain rates at Taylor Glacier, Antarctica
Ice exposed in ablation zones of ice sheets can be a valuable source of samples for paleoclimate studies and information about long-term ice dynamics. We report a 28-km long stable isotope sampling transect along a flowline on lower Taylor Glacier, Antarctica, and show that ice from the last glacial period is exposed here over tens of kilometers. Gas isotope analyses on a small number of samples confirm our age hypothesis. These chronostratigraph…
Climatology (2 obras) · Geology and Paleoclimatology Research (2 obras) · Transect (2 obras) · Climate change (1 obras) · Cryosphere (1 obras) · Cryospheric studies and observations (1 obras) · Geology (1 obras) · Geology (1 obras) · Glacial period (1 obras) · Glacier (1 obras)