Calibrating climate-d18O regression models for the interpretation of high-resolution speleothem d18O time series
Providing estimates of past climate changes on interannual-millenial timescales requires suitable regression models between climate and climate proxies. Many proxies appear to show relationships with climate that are timescale dependent. Any proxy-climate model should be able to replicate the major patterns that are observed at multiple timescales. Here we develop a new climate-isotope regression model for speleothems from a middle latitude site. In the low to middle latitudes, daily variation...[Show more]
|Collections||ANU Research Publications|
|Source:||Journal of Geophysical Research|
|01_Fischer_Calibrating_climate-d18O_2008.pdf||565.12 kB||Adobe PDF||Request a copy|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.