Area of research
Atmospheric Science · Global and Planetary Change
Research interest
Research interests include Geology, Ice core, Firn, Climatology, Deglaciation, and Oceanography.
The Greenland spatial fingerprint of Dansgaard–Oeschger events in observations and models
Bipolar impact and phasing of Heinrich-type climate variability
Gas isotope thermometry in the South Pole and Dome Fuji ice cores provides evidence for seasonal rectification of ice core gas records
Antarctic surface temperature and elevation during the Last Glacial Maximum
Abrupt Heinrich Stadial 1 cooling missing in Greenland oxygen isotopes
Surface Mass Balance Controlled by Local Surface Slope in Inland Antarctica: Implications for Ice‐Sheet Mass Balance and Oldest Ice Delineation in Dome Fuji
Evolution of mean ocean temperature in Marine Isotope Stage 4
Preindustrial 14CH4 indicates greater anthropogenic fossil CH4 emissions
An 83 000-year-old ice core from Roosevelt Island, Ross Sea, Antarctica
The SP19 chronology for the South Pole Ice Core – Part 2: gas chronology, Δage, and smoothing of atmospheric records
The SP19 chronology for the South Pole Ice Core – Part 1: volcanic matching and annual layer counting
Perfluorocyclobutane (PFC-318, <i>c</i> -C <sub>4</sub> F <sub>8</sub> ) in the global atmosphere
The Ross Sea Dipole – temperature, snow accumulation and sea ice variability in the Ross Sea region, Antarctica, over the past 2700 years
Firn Model Intercomparison Experiment (FirnMICE)
Minimal geological methane emissions during the Younger Dryas–Preboreal abrupt warming event
Synchronous volcanic eruptions and abrupt climate change ∼17.7 ka plausibly linked by stratospheric ozone depletion
Deglacial temperature history of West Antarctica
The WAIS Divide deep ice core WD2014 chronology – Part 1: Methane synchronization (68–31 ka BP) and the gas age–ice age difference
Consistent evidence of increasing Antarctic accumulation with warming
Observing and modeling the influence of layering on bubble trapping in polar firn
Centennial-scale changes in the global carbon cycle during the last deglaciation
Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104 ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprint
Greenland temperature response to climate forcing during the last deglaciation
Radiometric <sup>81</sup> Kr dating identifies 120,000-year-old ice at Taylor Glacier, Antarctica
A first chronology for the North Greenland Eemian Ice Drilling (NEEM) ice core
Gas transport in firn: multiple-tracer characterisation and model intercomparison for NEEM, Northern Greenland