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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Bibliographic Details
Main Author: Djamil, Yudha Setiawan
Other Authors: Wang Xianfeng
Format: Theses and Dissertations
Language:English
Published: 2019
Subjects:
Online Access:https://hdl.handle.net/10356/106426
http://hdl.handle.net/10220/47949
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Institution: Nanyang Technological University
Language: English