Mid-holocene climate change over the Maritime Continent : impact, attribution and mechanisms
Speleothem oxygen stable isotope (δ18O) records suggest that precipitation over the Maritime Continent changed significantly during the Mid-Holocene, a time interval about 6,000 years ago. These precipitation proxy datasets show that climatic conditions over the northern part of the region (e.g., Bo...
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| Other Authors: | |
| Format: | Theses and Dissertations |
| Language: | English |
| Published: |
2019
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| Online Access: | https://hdl.handle.net/10356/106426 http://hdl.handle.net/10220/47949 |
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| Institution: | Nanyang Technological University |
| Language: | English |
