Oxygen isotope records from stalagmites in Northern Borneo reflect changes in tropical Pacific hydrology on millennial timescales over the past 27,000 years. The records indicate that the tropical Pacific hydrological cycle is sensitive to high-latitude climate processes in both hemispheres, as well as to external radiative forcing, and that it may have played an important role in abrupt climate change events.
- Judson W. Partin
- Kim M. Cobb
- Diego P. Fernandez
