Uwe Mikolajewicz
Biographic Data
| ID | 5628793 |
|---|---|
| NAME | Uwe Mikolajewicz |
| GIVEN NAMES | Uwe |
| FAMILY NAME | Mikolajewicz |
| SIGNATURE | MIKOLAJEWICZ U |
| AFFILIATIONS | Max Planck Institute for Meteorology |
| VERIFIED | No |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 4 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2003 |
| LATEST PUBLICATION YEAR | 2021 |
| H-INDEX | 0 |
Massive deposition of Sahelian dust on the Canary Island Lanzarote during North Atlantic Heinrich Events
New IRSL ages of eolianites close to Muñique (Lanzarote) demonstrate the influence of millennial scale climatic variability on the sedimentary dynamics on the Canary Islands during the last glacial cycle. The repetitive succession of interstadial and stadial climatic conditions formed multiple sequences of eolian deposits, each in general comprising three depositional types. DepoType 1 and DepoType 2 consist mainly of marine biogenic carbonate de…
Vegetation context and climatic limits of the Early Pleistocene hominin dispersal in Europe
Atmospheric Lifetime of Fossil Fuel Carbon Dioxide
CO 2 released from combustion of fossil fuels equilibrates among the various carbon reservoirs of the atmosphere, the ocean, and the terrestrial biosphere on timescales of a few centuries. However, a sizeable fraction of the CO 2 remains in the atmosphere, awaiting a return to the solid earth by much slower weathering processes and deposition of CaCO 3 . Common measures of the atmospheric lifetime of CO 2 , including the e-folding time scale, dis…
Simulating near-equilibrium climate and vegetation for 6000 cal. years BP
The response of a coupled atmosphere-ocean general circulation model to insolation representative of 6000 years ago has been studied with a set of 1000-year quasi-equilibrium simulations. Comparison with similar experiments with an uncoupled atmosphere general circulation model demonstrates the importance of an interactive ocean for the climate signal. The model simulates an intensification of the African and Asian monsoons and a warming at high …
No prominent works on this page.
Simulating near-equilibrium climate and vegetation for 6000 cal. years BP
The response of a coupled atmosphere-ocean general circulation model to insolation representative of 6000 years ago has been studied with a set of 1000-year quasi-equilibrium simulations. Comparison with similar experiments with an uncoupled atmosphere general circulation model demonstrates the importance of an interactive ocean for the climate signal. The model simulates an intensification of the African and Asian monsoons and a warming at high …
Atmospheric Lifetime of Fossil Fuel Carbon Dioxide
CO 2 released from combustion of fossil fuels equilibrates among the various carbon reservoirs of the atmosphere, the ocean, and the terrestrial biosphere on timescales of a few centuries. However, a sizeable fraction of the CO 2 remains in the atmosphere, awaiting a return to the solid earth by much slower weathering processes and deposition of CaCO 3 . Common measures of the atmospheric lifetime of CO 2 , including the e-folding time scale, dis…
Vegetation context and climatic limits of the Early Pleistocene hominin dispersal in Europe
Massive deposition of Sahelian dust on the Canary Island Lanzarote during North Atlantic Heinrich Events
New IRSL ages of eolianites close to Muñique (Lanzarote) demonstrate the influence of millennial scale climatic variability on the sedimentary dynamics on the Canary Islands during the last glacial cycle. The repetitive succession of interstadial and stadial climatic conditions formed multiple sequences of eolian deposits, each in general comprising three depositional types. DepoType 1 and DepoType 2 consist mainly of marine biogenic carbonate de…
Climate change (3 works) · Climatology (3 works) · Geography (3 works) · Geology (3 works) · Geology and Paleoclimatology Research (3 works) · Oceanography (3 works) · Paleontology (3 works) · Atmospheric sciences (2 works) · Deposition (geology) (2 works) · Ecology (2 works)