Four degrees and beyond: the potential for a global temperature increase of four degrees and its implications
The 1992 UN Framework Convention on Climate Change commits signatories to preventing
'dangerous anthropogenic interference with the climate system', leaving unspecified the …
'dangerous anthropogenic interference with the climate system', leaving unspecified the …
Long-term release of carbon dioxide from arctic tundra ecosystems in Alaska
Releases of the greenhouse gases carbon dioxide (CO 2) and methane (CH 4) from thawing
permafrost are expected to be among the largest feedbacks to climate from arctic …
permafrost are expected to be among the largest feedbacks to climate from arctic …
Reviews and syntheses: Recent advances in microwave remote sensing in support of terrestrial carbon cycle science in Arctic–boreal regions
Spaceborne microwave remote sensing (300 MHz–100 GHz) provides a valuable method
for characterizing environmental changes, especially in Arctic–boreal regions (ABRs) where …
for characterizing environmental changes, especially in Arctic–boreal regions (ABRs) where …
The ABCflux database: Arctic-Boreal CO2 flux observations and ancillary information aggregated to monthly time steps across terrestrial ecosystems
Past efforts to synthesize and quantify the magnitude and change in carbon dioxide (CO 2)
fluxes in terrestrial ecosystems across the rapidly warming Arctic-Boreal Zone (ABZ) have …
fluxes in terrestrial ecosystems across the rapidly warming Arctic-Boreal Zone (ABZ) have …
Deeper snow alters soil nutrient availability and leaf nutrient status in high Arctic tundra
PR Semenchuk, B Elberling, C Amtorp, J Winkler… - Biogeochemistry, 2015 - Springer
Nitrogen (N) mineralization, nutrient availability, and plant growth in the Arctic are often
restricted by low temperatures. Predicted increases of cold-season temperatures may be …
restricted by low temperatures. Predicted increases of cold-season temperatures may be …
Increased wintertime CO2 loss as a result of sustained tundra warming
Permafrost soils currently store approximately 1672 Pg of carbon (C), but as high latitudes
warm, this temperature‐protected C reservoir will become vulnerable to higher rates of …
warm, this temperature‐protected C reservoir will become vulnerable to higher rates of …
Seasonality of soil CO2 efflux in a temperate forest: Biophysical effects of snowpack and spring freeze–thaw cycles
C Wang, Y Han, J Chen, X Wang, Q Zhang… - Agricultural and Forest …, 2013 - Elsevier
Changes in characteristics of snowfall and spring freeze–thaw-cycle (FTC) events under the
warming climate make it critical to understand biophysical controls on soil CO2 efflux (RS) in …
warming climate make it critical to understand biophysical controls on soil CO2 efflux (RS) in …
Environmental drivers of increased ecosystem respiration in a warming tundra
Arctic and alpine tundra ecosystems are large reservoirs of organic carbon,. Climate
warming may stimulate ecosystem respiration and release carbon into the atmosphere,. The …
warming may stimulate ecosystem respiration and release carbon into the atmosphere,. The …
Persistent wind‐induced enhancement of diffusive CO2 transport in a mountain forest snowpack
DR Bowling, WJ Massman - Journal of Geophysical Research …, 2011 - Wiley Online Library
Diffusion dominates the transport of trace gases between soil and the atmosphere. Pressure
gradients induced by atmospheric flow and wind interacting with topographical features …
gradients induced by atmospheric flow and wind interacting with topographical features …
[HTML][HTML] Environmental controls of winter soil carbon dioxide fluxes in boreal and tundra environments
The carbon cycle in Arctic–boreal regions (ABRs) is an important component of the
planetary carbon balance, with growing concerns about the consequences of ABR warming …
planetary carbon balance, with growing concerns about the consequences of ABR warming …