Understanding carbon pooling in the stratified boundary layer of the Arctic atmosphere |
Mark Schlutow
,
Mathias Göckede
,
Kai U. Totsche
,
Christoph Gerbig
|
Project descriptionHigh-latitude ecosystems play a pivotal role in the global carbon cycle. Approximately 50 % of the global below-ground carbon reservoir is stored in northern permafrost soils, an amount three times as large as currently contained in the atmosphere. Future climate change threatens to destabilize these reservoirs, with the potential to trigger strong feedback processes between climate and the carbon cycle that further amplify climate change. A key uncertainty in the context of monitoring the Arctic carbon are the night-time fluxes of greenhouse gases.During the day, the atmospheric dynamics are typically driven by convection in the boundary layer. The latter is therefore well mixed due to turbulence. At night, in contrast, radiative cooling gives rise to a stably stratified atmosphere which inhibits vertical mixing and causes pools of, e.g., carbon dioxide or methane that are released from the soil. This phenomenon poses eminent difficulties for flux measurements of greenhouse gases. Our project aims at improving our understanding of night-time carbon fluxes. Research program
Working group & planned collaborationsThe successful PhD candidate will join the European Research Council Synergy Project Q-ARCTIC group and be affiliated with the Department of Biogeochemical Signals at the Max Planck Institute for Biogeochemistry. Collaborations with our partners from Max Planck Institute for Meteorology in Hamburg are planned. For further information, please contact Mark Schlutow).RequirementsApplications to the IMPRS-gBGC are open to well-motivated and highly-qualified students from all countries. Prerequisites for this PhD project are:
![]() The Atmospheric Boundary Layer (Source), stable stratification indicated by dark grey area. |