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...
| Main Author: | |
|---|---|
| Other Authors: | |
| Format: | Thesis |
| Language: | English |
| Published: |
2019
|
| Subjects: | |
| Online Access: | https://hdl.handle.net/10356/106426 http://hdl.handle.net/10220/47949 |