This contribution provides a review of the most recent wavelet applications in the field of
earth sciences and is devoted to introducing and illustrating new wavelet analysis methods …

This survey of the current status of research into Earth's orbitally forced paleoclimatic record
summarizes recent developments in the theory of Earth's orbital parameters, and reviews …

We analyze the stability properties of the Synchrosqueezing transform, a time-frequency
signal analysis method that can identify and extract oscillatory components with time-varying …

The Mid-Pleistocene Climate Transition (MPT) is the complex climatic change which brought
the Late Pleistocene ice ages. We explore the MPT in the time and frequency domains by …

Spectral estimation, and corresponding time‐frequency representation for nonstationary
signals, is a cornerstone in geophysical signal processing and interpretation. The last 10–15 …

An agemodel not relying upon orbital assumptions is estimated over the last 2Ma using
depth in marine sediment cores as a proxy for time. Agemodel uncertainty averages±10Ka …

A new chronology of glaciation, spanning the last 780,000 years, is estimated from 21
marine sediment cores using depth as a proxy for time. To avoid biasing this “depth‐derived” …

The complexity of climate variability on all time scales requires the use of several refined
tools to unravel its primary dynamics from observations. Indeed, ideas from the theory of …

We have applied the standard wavelet and the adaptive wavelet transform algorithms to the
record of the Central England Temperature (CET) from 1659–1990. Peaks in the CET …

The mid-Pleistocene climate transition is a complex global change leading to Late
Pleistocene ice ages with increased mean ice volume and dominant 100-ka cycle. A …