G Raisbeck
Biographic Data
| ID | 7515432 |
|---|---|
| NAME | G Raisbeck |
| GIVEN NAMES | G |
| FAMILY NAME | Raisbeck |
| SIGNATURE | RAISBECK G |
| AFFILIATIONS | Laboratoire des Sciences du Climat et l'Environnement/Institut Pierre Simon Laplace, CEA-CNRSâ UniversiteÌ de Versailles Saint-Quentin en Yvelines, CE Saclay, 91191, Gif-sur-Yvette, France. |
| VERIFIED | No |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 3 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1989 |
| LATEST PUBLICATION YEAR | 2007 |
| H-INDEX | 0 |
Orbital and Millennial Antarctic Climate Variability over the Past 800,000 Years
A high-resolution deuterium profile is now available along the entire European Project for Ice Coring in Antarctica Dome C ice core, extending this climate record back to marine isotope stage 20.2, â 1⁄4800,000 years ago. Experiments performed with an atmospheric general circulation model including water isotopes support its temperature interpretation. We assessed the general correspondence between Dansgaard-Oeschger events and their smoothed Ant…
A Comparison of Deep Antarctic Ice Cores and Their Implications for Climate Between 65,000 and 15,000 Years Ago
Three ice cores drilled in the central part of the Antarctic continent extend back to the last glacial period: one from West Antarctica (Byrd) and two from East Antarctica (Vostok and Dome C). This period is also partly covered by a few cores from the coastal areas. In these cores, climatic information is mostly derived from the isotopic profiles (δD or δ 18 O) from which surface temperature and, more indirectly, precipitation rate can be estimat…
Global change over the last climatic cycle from the vostok ice core record (Antarctica)
No prominent works on this page.
A Comparison of Deep Antarctic Ice Cores and Their Implications for Climate Between 65,000 and 15,000 Years Ago
Three ice cores drilled in the central part of the Antarctic continent extend back to the last glacial period: one from West Antarctica (Byrd) and two from East Antarctica (Vostok and Dome C). This period is also partly covered by a few cores from the coastal areas. In these cores, climatic information is mostly derived from the isotopic profiles (δD or δ 18 O) from which surface temperature and, more indirectly, precipitation rate can be estimat…
Global change over the last climatic cycle from the vostok ice core record (Antarctica)
Orbital and Millennial Antarctic Climate Variability over the Past 800,000 Years
A high-resolution deuterium profile is now available along the entire European Project for Ice Coring in Antarctica Dome C ice core, extending this climate record back to marine isotope stage 20.2, â 1⁄4800,000 years ago. Experiments performed with an atmospheric general circulation model including water isotopes support its temperature interpretation. We assessed the general correspondence between Dansgaard-Oeschger events and their smoothed Ant…
Climatology (3 works) · Geology and Paleoclimatology Research (3 works) · Climate change (2 works) · Cryosphere (2 works) · Cryospheric studies and observations (2 works) · Geography (2 works) · Geology (2 works) · Glacial period (2 works) · Ice core (2 works) · Ice sheet (2 works)