Not exact matches
The team discovered that the human
impact on biogenic methane and nitrous oxide emissions far outweighed the human
impact on the
terrestrial uptake of
carbon dioxide, meaning that humans have caused the
terrestrial biosphere to further contribute to warming.
«(C) the
carbon cycle, including
impacts related to the thawing of permafrost, the frequency and intensity of wildfire, and
terrestrial and ocean
carbon sinks;
These correlations were negative, suggesting that when average fire weather seasons are longer - than - normal or when long seasons
impacted more global burnable area, net global
terrestrial carbon uptake is reduced.
Impact of
terrestrial biosphere
carbon exchanges on the anomalous CO2 increase in 2002â??
Several other groups have evaluated the
impact of coupling specific models of
carbon to climate models but clear results are difficult to obtain because of inevitable biases in both the
terrestrial and atmospheric modules (e.g., Delire et al., 2003).
We introduce a
carbon cycle model that would explain the PETM by global warming following a bolide
impact, leading to the oxidation of
terrestrial organic
carbon stores built up during the late Paleocene.
«(C) the
carbon cycle, including
impacts related to the thawing of permafrost, the frequency and intensity of wildfire, and
terrestrial and ocean
carbon sinks;
Even a small increase in soil
carbon could have a big
impact on
carbon dioxide pollution levels, particularly in rangelands, which span a quarter of the earth's land surface and store about a third of all
terrestrial soil
carbon.
Disturbances such as Superstorm Sandy and Hurricane Katrina cause large
impacts to the
terrestrial carbon cycle, forest tree mortality and CO2 emissions from decomposition, in addition to significant economic
impacts.
This created a qualitative transformation in Homo sapiens»
impact on earth system trends: levels of
carbon dioxide, nitrous oxide, methane, stratospheric ozone, surface ocean temperature, ocean acidification, marine fish capture, coastal nitrogen, tropical forest depletion, land domestication and
terrestrial biosphere degradation.
I slagged you off at my blog because you posted a comment at WUWT that was irrelevant and misleading: the old
carbon effect in aquatic mosses has no
impact on the radiocarbon dates of
terrestrial mosses.
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
The team studying the data - drawn from expert fields across the globe - was attempting to assess the
impact of climate change one of the planet's largest
terrestrial stores of
carbon.
For example, The
impact of Miocene atmospheric
carbon dioxide fluctuations on climate and the evolution of
terrestrial ecosystems by Wolfram M. Kurschner, Zlatko Kvacek, and David L. Dilcher, PNAS January 15, 2008 vol.
Multiscale modelling of permafrost
carbon feedbacks and
impacts on climate, modeling of the
terrestrial biosphere, biogeochemistry, land - atmosphere interactions, remote sensing applications
Impacts of large - scale and persistent changes in the MOC are likely to include changes to marine ecosystem productivity, fisheries, ocean
carbon dioxide uptake, oceanic oxygen concentrations and
terrestrial vegetation [Working Group I Fourth Assessment 10.3, 10.7; Working Group II Fourth Assessment 12.6, 19.3].
Studies also suggest there could be
impacts on the
carbon cycle (Zickfeld et al, 2008) and on soil moisture and primary productivity of the
terrestrial vegetation (Vellinga and Wood, 2002).»
Climate change
impacts on ecosystems and the
terrestrial carbon sink: a new assessment.
Then note that even at current levels of CO2, we are back to Miocene conditions, The
impact of Miocene atmospheric
carbon dioxide fluctuations on climate and the evolution of
terrestrial ecosystems Wolfram M. Kürschner, Zlatko Kvaček, and David L. Dilcher http://www.pnas.org/content/105/2/449.long with sea highstands ~ 60 meters above current sea levels.
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.