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  1. Home

AmeriFlux in 48 U.S. states – new interactive map!

by Christin Buechner - June 27, 2025

The AmeriFlux network aims to ensure the availability of continuous, long-term ecosystem measurements necessary to build effective models and multisite syntheses, as well as provide immediate insights. AmeriFlux sites span… More

in Homepage   0

Representativeness Of Eddy-Covariance Flux Footprints For Areas Surrounding Ameriflux Sites

by Housen Chu - March 18, 2021

Large datasets of greenhouse gas and energy surface-atmosphere fluxes measured with the eddy-covariance technique (e.g., FLUXNET2015, AmeriFlux BASE) are widely used to benchmark models and remote-sensing products. This study addresses… More

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Bengtsson, Carl

by Carl Bengtsson - July 17, 2020

in Year of Methane   NDIR 0

GUNTURU, Vamsi Krishna

by GUNTURU VAMSI KRISHNA - December 17, 2018

in Year of Methane   0

Temporal Dynamics Of Aerodynamic Canopy Height Derived From Eddy Covariance Momentum Flux Data Across North American Flux Networks

by Housen Chu - October 4, 2018

Aerodynamic canopy height (ha) is the effective height of vegetation canopy for its influence on atmospheric fluxes and is a key parameter of surface‐atmosphere coupling. However, methods to estimate ha… More

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Rapid And Transient Response Of Soil Respiration To Rain

by Fianna O'Brien - January 31, 2017

The influence of rainstorm on soil respiration of a mixed forest in southern New England, USA was investigated with eddy covariance, rain simulation and laboratory incubation. Soil respiration is shown… More

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Anthropogenic Emission Of Mercury To The Atmosphere In The Northeast United States

by Fianna O'Brien - January 30, 2017

The severity and spatial extent of the health impact of anthropogenic mercury (Hg) emission to the atmosphere depend on the emission rate and chemical form of the emitted species. The… More

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A Model For Scalar Advection Inside Canopies And Application To Footprint Investigation

by Fianna O'Brien - January 30, 2017

In this paper, a model is presented for scalar advection inside canopies. A key result is an advection/diffusion equation that captures the persistence effect of the diffusion plume from elevated… More

in    0
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