Penobscot Experimental Forest boundary, roads, trails, management units, and permanent sample plot locations (2nd Edition)

Author(s):  
Liam F. Kenefic ◽  
Bethany L. Muñoz Delgado ◽  
Nicole S. Rogers ◽  
Andrew R. Richley
Ecology ◽  
2011 ◽  
Vol 92 (6) ◽  
pp. 1376-1376 ◽  
Author(s):  
Raphaël Pélissier ◽  
Jean-Pierre Pascal ◽  
N. Ayyappan ◽  
B. R. Ramesh ◽  
S. Aravajy ◽  
...  

2010 ◽  
Vol 259 (3) ◽  
pp. 573-582 ◽  
Author(s):  
Sanna Härkönen ◽  
Antti Mäkinen ◽  
Timo Tokola ◽  
Jussi Rasinmäki ◽  
Jouni Kalliovirta

Author(s):  
Tyler Searls ◽  
Xinbiao Zhu ◽  
D.W. McKenney ◽  
Rony Mazumder ◽  
James Steenberg ◽  
...  

Climate has a considerable influence on tree growth. Forest managers benefit from the empirical study of the historic relationship between climatic variables and tree growth to support forest management frameworks which are to be applied under scenarios of climate change. Through this research, we have utilized long-term permanent sample plot records, historic climate datasets, and linear mixed modelling techniques to evaluate the historic influence of climatic variables on the growth rates of major boreal tree species in Newfoundland and Labrador, Canada. For the commercially significant spruce and fir forests of the province, we found growing degree days (GDD) to negatively correlate with tree productivity in warmer regions, such as much of Newfoundland (±1,350 GDD), but positively correlate with growth in cooler regions, such as those in Labrador (±750 GDD). With respect to precipitation, environmental moisture was not on average a limiting factor to species productivity in the province. These dynamics have implications for the productivity of the spruce-fir forests of the study area when considered alongside contemporary climate projections for the region, which generally entail both a warmer and wetter growing environment.


2004 ◽  
pp. 63-75
Author(s):  
Martin Bobinac

The effects of selection thinning were analyzed at a permanent sample plot in the artificially established spruce stand aged 32 years, on the site of mountain beech. The state in the 32-year-old stand was as follows: 3911 trees per ha, basal area 57.5 m2ha-1 and volume 378.3 m3ha-1. Selection thinning removed 1378 tree per ha (35.2%) and 110 m3ha-1 (29.2%), and in the period between the ages of 32 and 40 years, predominantly because of mortality, another 550 trees per ha and 21.8 m3ha-1. On the remaining trees during the period between the ages of 32 and 40 years, basal area increased by 33%, and volume by 67%. Current volume increment was 20.7 m3ha-1 and it was concentrated on the future trees (28% of the total number of trees produces 52% of volume increment). The disproportion in the intensity of diameter and height increment after the thinning resulted in the increase of form quotient.


2005 ◽  
Vol 20 (sup6) ◽  
pp. 94-101 ◽  
Author(s):  
Ahto Kangur ◽  
Henn Korjus ◽  
Kalev Jõgiste ◽  
Andres Kiviste

2012 ◽  
Vol 68 (1) ◽  
pp. 3-16 ◽  
Author(s):  
Eileen L. Jones ◽  
Lori D. Daniels

1988 ◽  
Vol 18 (10) ◽  
pp. 1255-1260 ◽  
Author(s):  
D. E. Tait ◽  
C. J. Cieszewski ◽  
I. E. Bella

A general stand model is fitted to a set of permanent sample plot data for lodgepole pine in Alberta. The model represents a site-specific, variable-density stand model for volume growth and mortality of lodgepole pine. The structure of the model provides a general framework for examining volume growth and mortality in lodgepole pine. The model's performance is compared with the Alberta Forest Service yield tables and with the results of an experimental thinning study.


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