J.H. McCaughey

TL;DR: In this article, the authors summarize more than 180 site years of eddy covariance measurements of carbon dioxide flux made at forest chronosequences in North America and show that carbon loss from all ecosystems following a stand-replacing disturbance, becoming a carbon sink by 20 years for all ecosystems and by 10 years for most.

TL;DR: In this article, the Boreal Ecosystem Research and Monitoring Sites (BERMS) in central Saskatchewan, Canada were used for measuring carbon fluxes to boreal forest stands between 10 and 50 years of age.

TL;DR: In this article, the authors analyzed 5 years of EC carbon dioxide, water vapor, and sensible heat flux measurements from three mature boreal forest stands in central Saskatchewan, Canada, and derived an analogous FNEE ''closure fraction'' CF NEE by normalizing measured FNEE against estimates from an empirical model.

TL;DR: In this paper, the authors used the eddy covariance (EC) technique to measure carbon exchange at three boreal forest mature sites including Southern Old Aspen (SOA), Southern Old Black Spruce (SOBS), and Southern Old Jack Pine (SOJP) in 2000.

TL;DR: In this paper, the authors synthesize energy balance measures from 22 sites in Alaska, Saskatchewan and Manitoba collected between 1998 and 2004 for a 150-year boreal forest chronosequence.