Area of research
Atmospheric Science · Global and Planetary Change
Research interest
Research interests include Geology and Paleoclimatology Research, Atmospheric and Environmental Gas Dynamics, Cryospheric studies and observations, and Tree-ring climate responses.
Tree-ring stable isotopes from the European Alps reveal long-term summer drying over the Holocene
Recent human-induced atmospheric drying across Europe unprecedented in the last 400 years
Constraints for precise and accurate fluid inclusion stable isotope analysis using water-vapour saturated CRDS techniques
The unknown third - exploring the climatic and non-climatic signals of hydrogen isotopes in tree-ring cellulose across Europe
The unknown third – Hydrogen isotopes in tree-ring cellulose across Europe
The fingerprint of the summer 2018 drought in Europe on ground-based atmospheric CO <sub>2</sub> measurements
Spatio‐temporal patterns of tree growth as related to carbon isotope fractionation in European forests under changing climate
20th century changes in carbon isotopes and water-use efficiency: tree-ring-based evaluation of the CLM4.5 and LPX-Bern models
Using 81Kr and noble gases to characterize and date groundwater and brines in the Baltic Artesian Basin on the one-million-year timescale
Trophic state changes can affect the importance of methane-derived carbon in aquatic food webs
The 8.2‐ka BP event in north‐eastern North America: first combined oxygen and hydrogen isotopic data from peat in Newfoundland
Water-use efficiency and transpiration across European forests during the Anthropocene
Temperature reconstruction from 10 to 120 kyr b2k from the NGRIP ice core
Greenland temperature response to climate forcing during the last deglaciation
Spatial variability and temporal trends in water‐use efficiency of European forests
Simultaneous Determination of Stable Carbon, Oxygen, and Hydrogen Isotopes in Cellulose
An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka
Spatial gradients of temperature, accumulation and δ <sup>18</sup> O-ice in Greenland over a series of Dansgaard–Oeschger events
Carbon Isotope Constraints on the Deglacial CO <sub>2</sub> Rise from Ice Cores