Living wall systems are a relatively new form of façade cladding treatment on buildings. Bringing a host of benefits such as added biodiversity, they also have the potential to aid the …
Soils in Arctic and boreal ecosystems store twice as much carbon as the atmosphere, a portion of which may be released as high-latitude soils warm. Some of the uncertainty in the …
The resilience and vulnerability of permafrost to climate change depends on complex interactions among topography, water, soil, vegetation, and snow, which allow permafrost to …
G Grosse, J Harden, M Turetsky… - Journal of …, 2011 - Wiley Online Library
This synthesis addresses the vulnerability of the North American high‐latitude soil organic carbon (SOC) pool to climate change. Disturbances caused by climate warming in arctic …
Peatlands have acted as net CO2 sinks over millennia, exerting a global climate cooling effect. Rapid warming at northern latitudes, where peatlands are abundant, can disturb their …
Carbon release from thawing permafrost soils could significantly exacerbate global warming as the active‐layer deepens, exposing more carbon to decay. Plant community and soil …
As permafrost degrades, the amount of organic soil carbon (C) that thaws during the growing season will increase, but decomposition may be limited by saturated soil conditions common …
DM Lawrence, AG Slater, SC Swenson - Journal of Climate, 2012 - journals.ametsoc.org
Simulation of Present-Day and Future Permafrost and Seasonally Frozen Ground Conditions in CCSM4 in: Journal of Climate Volume 25 Issue 7 (2012) Jump to Content …
There is a growing body of empirical evidence documenting the expansion of shrub vegetation in the circumpolar Arctic in response to climate change. Here, we conduct a …