Mystakidis, S., Davin, E. L., Gruber, N. and Seneviratne, S. I. (2016), Constraining
future terrestrial carbon cycle projections using observation - based water and carbon flux estimates.
Not exact matches
Vulnerability of anaerobically protected
carbon to
future climate or land use change thus constitutes a yet unrecognized soil
carbon - climate feedback that should be incorporated into
terrestrial ecosystem models.»
This study highlights the key role of vegetation in controlling
future terrestrial hydrologic response and emphasizes that the continental
carbon and water cycles are intimately coupled over land and must be studied as an interconnected system.
It's possible that
terrestrial sinks could continue to sop up and sequester some anthropogenic
carbon, but there's an owful lot of near - surface
carbon and if that get's oxidized at some point in the
future, then we could be in even hotter water.
Wårlind, D., Smith, B., Hickler, T., and Arneth, A.: Nitrogen feedbacks increase
future terrestrial ecosystem
carbon uptake in an individual - based dynamic vegetation model, Biogeosciences, 11, 6131 - 6146, doi: 10.5194 / bg -11-6131-2014, 2014 link
Future productivity and
carbon storage limited by
terrestrial nutrient availability.
Evaluation of the
terrestrial carbon cycle,
future plant geography and climate -
carbon cycle feedbacks using five Dynamic Global Vegetation Models (DGVMs)
While ocean models disagree about
future carbon uptake rates,
terrestrial models do not even agree about the sign of
future carbon exchange, with some showing continued uptake, and others indicating weakening uptake or even transitioning to sources.
The research needs for predicting — across multiple scales — the impact of land use change and management practices to the
future of
terrestrial carbon storage and CDR potential
Topics that I work on or plan to work in the
future include studies of: + missing aerosol species and sources, such as the primary oceanic aerosols and their importance on the remote marine atmosphere, the in - cloud and aerosol water aqueous formation of organic aerosols that can lead to brown
carbon formation, the primary
terrestrial biological particles, and the organic nitrogen + missing aerosol parameterizations, such as the effect of aerosol mixing on cloud condensation nuclei and aerosol absorption, the semi-volatility of primary organic aerosols, the importance of in - canopy processes on natural
terrestrial aerosol and aerosol precursor sources, and the mineral dust iron solubility and bioavailability + the change of aerosol burden and its spatiotemporal distribution, especially with regard to its role and importance on gas - phase chemistry via photolysis rates changes and heterogeneous reactions in the atmosphere, as well as their effect on key gas - phase species like ozone + the physical and optical properties of aerosols, which affect aerosol transport, lifetime, and light scattering and absorption, with the latter being very sensitive to the vertical distribution of absorbing aerosols + aerosol - cloud interactions, which include cloud activation, the aerosol indirect effect and the impact of clouds on aerosol removal + changes on climate and feedbacks related with all these topics In order to understand the climate system as a whole, improve the aerosol representation in the GISS ModelE2 and contribute to
future IPCC climate change assessments and CMIP activities, I am also interested in understanding the importance of natural and anthropogenic aerosol changes in the atmosphere on the
terrestrial biosphere, the ocean and climate.