Vjeran’s publication on inverting past ice extents to constrain paleo-mass balances.

Congratulations to Vjeran! Here is the link.

With the conclusion of the Last Glacial Maximum (LGM), about 20 000 years ago, ended the most recent long-lasting cold phase in Earth history. This last glacial advance left a strong observable imprint on the landscape, such as moraines, trimlines and other glacial geomorphic features. These features reflect the extent of former glaciers and ice caps, which in turn provides information on past temperature and precipitation conditions. Here we present an inverse approach to reconstruct the equilibrium line altitudes (E) from observed ice extents. The ice-flow model is developed solving the mass conservation equation using the shallow ice approximation and implemented using Graphical Processing Units (GPUs). We present the theoretical basis of the inversion method, which relies on a Tikhonov regularization, and demonstrate its ability to constrain spatial variations in mass balance with idealized and real glaciers.

Introduction of a new thermochronometric method based on thermoluminescence

Rabiul published a paper on his methodological development of thermo-luminescence thermometry (TLT) in Earth and Planetary Science Letters: https://www.sciencedirect.com/science/article/pii/S0012821X18302334

This study builds on the suite of thermochronometric techniques we are developing in our laboratory. TLT enables us to target different traps that have different kinetic properties, and in turn gain more constraints on the recent (i.e., 10-100 ky) thermal histories of rocks.

The paper also proposes an alternative way to directly invert TLT data into exhumation rate histories using a Bayesian inverse approach.