De rol van terrestrisch sub-Antarctica binnen het klimaatsonderzoek op wereldvlak
Climate change in the past is studied in terrestrial, deep ocean and ice cores. For the last ten years, climatological research has been focused on climatic connections between data from different sources and environments on earth and on the driving mechanims behind this climatic connections. The No...
| Main Author: | |
|---|---|
| Other Authors: | |
| Format: | Article in Journal/Newspaper |
| Language: | Dutch |
| Published: |
2006
|
| Subjects: | |
| Online Access: | https://biblio.ugent.be/publication/624398 http://hdl.handle.net/1854/LU-624398 |
| Summary: | Climate change in the past is studied in terrestrial, deep ocean and ice cores. For the last ten years, climatological research has been focused on climatic connections between data from different sources and environments on earth and on the driving mechanims behind this climatic connections. The North Atlantic region is the best known region only because of the many palaeoclimatological data present in this area. Past climate change in the Southern Hemisphere has been attained especially by research of Antarctic ice cores. The number of studies of terrestrial and oceanic cores in the Southern Hemisphere is lower than in the north. The significance of the sub-Antarctic region for the palaeoclimatological discussion has been rather “neglected” in the past. However, the restricted published data and our own research shows that sub-Antarctic islands have a great potential for high resolution terrestrial palaeoclimatological research. Moreover, these islands represent the only terrestrial archives in the circum-Antarctic ocean. |
|---|