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Bengtsson, Carl

by Carl Bengtsson - July 17, 2020

in Year of Methane   NDIR 0

FLUXNET-CH4 Synthesis Activity: Objectives, Observations, and Future Directions

by Gavin McNicol - August 8, 2019

Over the past decades, the eddy covariance (EC) community has clearly demonstrated the power of networks; regional networks and FLUXNET have shown us that combining data across multiple sites creates… More

in Homepage, Sites, Year of Methane   carbon flux synthesis, scaling; biogeochemistry; wetland; spatial heterogeneity; synthesis, Year of Methane 0

GUNTURU, Vamsi Krishna

by GUNTURU VAMSI KRISHNA - December 17, 2018

in Year of Methane   0

Orchidee-Peat (Revision 4596), A Model For Northern Peatland Co≪Sub≫2≪/Sub≫, Water, And Energy Fluxes On Daily To Annual Scales

by - June 19, 2018

Peatlands store substantial amounts of carbon and are vulnerable to climate change. We present a modified version of the Organising Carbon and Hydrology In Dynamic Ecosystems (ORCHIDEE) land surface model… More

in    0

Methane Fluxes During The Initiation Of A Large-Scale Water Table Manipulation Experiment In The Alaskan Arctic Tundra

by Fianna O'Brien - January 31, 2017

Much of the 191.8 Pg C in the upper 1 m of Arctic soil of Arctic soil organic mater is, or is at risk of, being released to the atmosphere… More

in    0

Light-Stress Avoidance Mechanisms In A Sphagnum-Dominated Wet Coastal Arctic Tundra Ecosystem In Alaska

by Fianna O'Brien - January 30, 2017

The Arctic experiences a high-radiation environment in the summer with 24-hour daylight for more than two months. Damage to plants and ecosystem metabolism can be muted by overcast conditions common… More

in    0

Increased CO2 Loss From Vegetated Drained Lake Tundra Ecosystems Due To Flooding

by Fianna O'Brien - January 25, 2017

Tundra ecosystems are especially sensitive to climate change, which is particularly rapid in high northern latitudes resulting in significant alterations in temperature and soil moisture. Numerous studies have demonstrated that… More

in    0
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