Reconstructing a climate process in both space and time from incomplete instrumental and
climate proxy time series is a problem with clear societal relevance that poses both scientific …

TEX 86 is an important proxy for constraining ocean temperatures in the Earth's past.
Current calibrations, however, feature structured residuals indicative of a spatially-varying …

Additional analyses, reconstructions and description of the data. The document (a pdf-file)
includes an analysis of the Gaussian response model and its parameters, reference records …

Estimating chronological uncertainty is a critical but often neglected prerequisite in
palaeoclimatological reconstructions and core comparisons. We describe a hierarchical …

Reconstructions of past climatic changes from borehole temperature profiles are important
independent estimates of temperature histories over the last millennium. There remain …

We propose a method to merge several paleoclimate time series into one that exhibits a
consensus on the features of the individual times series. The paleoclimate time series can …

We identify two issues with the reverse regression approach as implemented in several
classic reconstructions of past climate fluctuations from dendroclimatologcical data series …

Permafrost consists of soil and rocks that remain at 0° C or below for at least two consecutive
years. In mountains, permafrost ground ice acts like cement, stabilizing rock walls. Its …

An important statistical challenge lies in the specification of flexible spatio-temporal models
capable of capturing complex, nonstationary dependence structure in the underlying …

The rising temperature of the earth due to climate change has shown to alter the variations
of hydro-climate variables, including their intensities, frequencies and durations. Extreme …