Graham Shimmield
Biographic Data
| ID | 6378464 |
|---|---|
| NAME | Graham Shimmield |
| GIVEN NAMES | Graham |
| FAMILY NAME | Shimmield |
| SIGNATURE | SHIMMIELD G |
| AFFILIATIONS | University of Edinburgh |
| VERIFIED | No |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 6 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1992 |
| LATEST PUBLICATION YEAR | 2001 |
| H-INDEX | 1 |
Variability in the El Niño-Southern Oscillation Through a Glacial-Interglacial Cycle
The El Niño–Southern Oscillation (ENSO) is the most potent source of interannual climate variability. Uncertainty surrounding the impact of greenhouse warming on ENSO strength and frequency has stimulated efforts to develop a better understanding of the sensitivity of ENSO to climate change. Here we use annually banded corals from Papua New Guinea to show that ENSO has existed for the past 130,000 years, operating even during “glacial” times of s…
Environmental changes of the last three centuries indicated by siliceous microfossil records from the southwestern Baltic Sea
Four short sediment cores from the southwestern Baltic Sea were analysed with respect to their content of siliceous microfossils. The aim was to detect and date changes in the composition of the diatom flora and to link these changes to variations in the anthropogenic load of nutrients during the last century. The study shows that the most significant change in the diatom assemblages occurred 130-140 years ago. The change is recorded in the sedim…
Ocean Margin Processes in Global Change
Environmental changes of the last three centuries indicated by siliceous microfossil records from the southwestern Baltic Sea
Four short sediment cores from the southwestern Baltic Sea were analysed with respect to their content of siliceous microfossils. The aim was to detect and date changes in the composition of the diatom flora and to link these changes to variations in the anthropogenic load of nutrients during the last century. The study shows that the most significant change in the diatom assemblages occurred 130-140 years ago. The change is recorded in the sedim…
Ocean Margin Processes in Global Change
Ocean Margin Processes in Global Change
Environmental changes of the last three centuries indicated by siliceous microfossil records from the southwestern Baltic Sea
Four short sediment cores from the southwestern Baltic Sea were analysed with respect to their content of siliceous microfossils. The aim was to detect and date changes in the composition of the diatom flora and to link these changes to variations in the anthropogenic load of nutrients during the last century. The study shows that the most significant change in the diatom assemblages occurred 130-140 years ago. The change is recorded in the sedim…
Variability in the El Niño-Southern Oscillation Through a Glacial-Interglacial Cycle
The El Niño–Southern Oscillation (ENSO) is the most potent source of interannual climate variability. Uncertainty surrounding the impact of greenhouse warming on ENSO strength and frequency has stimulated efforts to develop a better understanding of the sensitivity of ENSO to climate change. Here we use annually banded corals from Papua New Guinea to show that ENSO has existed for the past 130,000 years, operating even during “glacial” times of s…
Climate change (3 works) · Geology and Paleoclimatology Research (3 works) · Climatology (2 works) · Environmental Science (2 works) · Geology (2 works) · Marine and environmental studies (2 works) · Oceanography (2 works) · Paleontology (2 works) · Biology (1 work) · Climate variability and models (1 work)