40 results on '"Schwander, Jakob"'
Search Results
2. Stable Carbon Cycle: Climate Relationship during the Late Pleistocene
3. Atmospheric Methane and Nitrous Oxide of the Late Pleistocene from Antarctic Ice Cores
4. Ice-core data used for the construction of the Greenland Ice-Core Chronology 2005 and 2021 (GICC05 and GICC21).
5. Progress of the RADIX (Rapid Access Drilling and Ice eXtraction) fast-access drilling system.
6. Responses to rapid warming at Termination 1a at Gerzensee (Central Europe): Primary succession, albedo, soils, lake development, and ecological interactions
7. High-resolution late-glacial chronology for the Gerzensee lake record (Switzerland): δ18O correlation between a Gerzensee-stack and NGRIP
8. Toward a radiometric ice clock: uranium ages of the Dome C ice core
9. Progress of the RADIX fast access drilling system.
10. Glacial–interglacial and millennial-scale variations in the atmospheric nitrous oxide concentration during the last 800,000 years
11. The glacial inception as recorded in the NorthGRIP Greenland ice core: timing, structure and associated abrupt temperature changes
12. What was the surface temperature in central Antarctica during the last glacial maximum?
13. Quantification of biotic responses to rapid climatic changes around the Younger Dryas — a synthesis
14. Isotope signature of the Younger Dryas and two minor oscillations at Gerzensee (Switzerland): palaeoclimatic and palaeolimnologic interpretation based on bulk and biogenic carbonates
15. Oxygen isotopes of lake marl at Gerzensee and Leysin (Switzerland), covering the Younger Dryas and two minor oscillations, and their correlation to the GRIP ice core
16. Tropospheric observations of CFC-114 and CFC-114a with a focus on long-term trends and emissions.
17. Climatic and insolation control on the high-resolution total air content in the NGRIP ice core.
18. Atmospheric abundance and global emissions of perfluorocarbons CF4, C2F6 and C3F8 since 1800 inferred from ice core, firn, air archive and in situ measurements.
19. Drilling into debris-rich basal ice at the bottom of the NEEM (Greenland) borehole.
20. Newly detected ozone-depleting substances in the atmosphere.
21. Improved method to determine radio-echo sounding reflector depths from ice-core profiles of permittivity and conductivity.
22. Temporal and spatial variation of stable-isotope ratios and accumulation rates in the hinterland of Neumayer station, East Antarctica.
23. Change in CO2 concentration and O2/N2 ratio in ice cores due to molecular diffusion.
24. Formal definition and dating of the GSSP (Global Stratotype Section and Point) for the base of the Holocene using the Greenland NGRIP ice core, and selected auxiliary records.
25. Atmospheric Trends and Radiative Forcings of CF4 and C2F6 Inferred from Firn Air.
26. Marine Isotope Stage (MIS) 8 millennial variability stratigraphically identical to MIS 3.
27. Supporting evidence from the EPICA Dronning Maud Land ice core for atmospheric CO2 changes during the past millennium.
28. Evidence for stratigraphic distortion in the Greenland Ice Core Project (GRIP) ice core during Event 5e1 (120 kyr BP) from gas isotopes.
29. N2O and CH4 variations during the last glacial epoch: Insight into global processes.
30. A tentative reconstruction of the last interglacial and glacial inception in Greenland based on new gas measurements in the Greenland Ice Core Project (GRIP) ice core.
31. A tentative chronology for the EPICA Dome Concordia Ice Core.
32. Delta 15N measurements as a calibration tool for the paleothermometer and gas-ice age differences: A case study for the 8200 B.P. event on GRIP ice.
33. Changes in the atmospheric CH4 gradient between Greenland and Antarctica during the Holocene.
34. Processes affecting the CO2 concentrations measured in Greenland ice.
35. Outline of the Little Dome C deep drilling operation.
36. Atmospheric nitrous oxide during the last 140,000years
37. Evidence from firn air for recent decreases in non-methane hydrocarbons and a 20th century increase in nitrogen oxides in the northern hemisphere
38. CO2 and O2/N2 variations in and just below the bubble–clathrate transformation zone of Antarctic ice cores
39. Isotope calibrated Greenland temperature record over Marine Isotope Stage 3 and its relation to CH4
40. Evidence for substantial accumulation rate variability in Antarctica during the Holocene, through synchronization of CO2 in the Taylor Dome, Dome C and DML ice cores
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