Modeling the effects of climate change and management on the dead wood dynamics in boreal forest plantations

2013 ◽  
Vol 133 (3) ◽  
pp. 405-421 ◽  
Author(s):  
Adriano Mazziotta ◽  
Mikko Mönkkönen ◽  
Harri Strandman ◽  
Johanna Routa ◽  
Olli-Pekka Tikkanen ◽  
...  
Silva Fennica ◽  
2019 ◽  
Vol 53 (4) ◽  
Author(s):  
Panu Halme ◽  
Jenna Purhonen ◽  
Emma-Liina Marjakangas ◽  
Atte Komonen ◽  
Katja Juutilainen ◽  
...  

Dead wood profile of a forest is a useful tool for describing forest characteristics and assessing forest disturbance history. Nevertheless, dead wood profiles, including both coarse and fine dead wood, are rare as well as studies on the effect of sampling intensity on the dead wood estimates. In a semi-natural boreal forest, we measured every dead wood item over 2 cm in diameter from 80 study plots. From eight plots, we further recorded dead wood items below 2 cm in diameter. Based on these data we constructed the full dead wood profile, i.e. the overall number of dead wood items and their distribution among different tree species, volumes of different size and decay stage categories. We discovered that while the number of small dead wood items was immense, their number dropped drastically from the diameter below 1 cm to diameters 2-3 cm. Different tree species had notably different abundance-diameter distribution patterns: spruce dead wood comprised mainly of the smallest diameter fractions, whereas aspen dead wood had larger share of large-diameter items. Considering volume, most dead wood was large (>10 cm in diameter), out of which 62% was birch. We also observed that the variation in the dead wood estimates was small for the numerically dominant tree species and smallest diameter categories, but high for the sub-dominant tree species and larger size categories. In conclusion, the more the focus of the dead wood inventory is on rare tree species and large dead wood items, the more comprehensive should the sampling be.


PMLA ◽  
1937 ◽  
Vol 52 (4) ◽  
pp. 1183-1190
Author(s):  
George W. Whiting

To the student of writing and literature few inquiries are more interesting and valuable than that into an author's practices in revising his own work. To observe the various stages in the evolution of the final version, to note carefully an artist at his work of pruning the dead wood, adding fresh material, smoothing away harsh phrases, selecting just words, and letting light into obscure places—to do this is to come somewhat nearer to an understanding of what in spite of all analysis will remain essentially a mystery. Especially fascinating and instructive is the study of Conrad's revision, for here one sees a supreme artist at work. In his vigorous hewing and rebuilding there is conclusive proof of the artist's untiring industry and consummate skill. Conrad's revision of Nostromo is of particular interest, for this novel occupies a critical place in the evolution of Conrad's prose. Mr. Richard Curie has justly characterized the change that came over Conrad's prose—a change perceptible in the “Amy Foster” of Typhoon and fully marked in from Under Western Eyes onward. This evolution has smoothed away the cadence, has concentrated the manner, has toned down the style of Conrad's former exuberance. At first glance the later and the earlier Conrad appear two totally different men. The unruly splendor of the one has given way to the subtle and elastic suavity of the other … His earlier prose is sometimes uncertain, sometimes exaggerated, but his later prose has the uniform temper of absolute mastery.


2017 ◽  
Vol 106 (3) ◽  
pp. 977-990 ◽  
Author(s):  
Yan Boulanger ◽  
Anthony R. Taylor ◽  
David T. Price ◽  
Dominic Cyr ◽  
Guillaume Sainte-Marie
Keyword(s):  

2007 ◽  
Vol 250 (1-2) ◽  
pp. 77-88 ◽  
Author(s):  
I. Vanha-Majamaa ◽  
S. Lilja ◽  
R. Ryömä ◽  
J.S. Kotiaho ◽  
S. Laaka-Lindberg ◽  
...  

1998 ◽  
Vol 28 (4) ◽  
pp. 524-533 ◽  
Author(s):  
J Renée Brooks ◽  
Lawrence B Flanagan ◽  
James R Ehleringer

Spatial distribution and species composition of the boreal forest are expected to change under predicted climate change scenarios. Current research indicates that water limitations control the southern boundary of the central Canadian boreal forest and temperature limitations control the northern boundary. As part of Boreal Ecosystem - Atmosphere Study (BOREAS), we examined this idea by comparing annual variation in tree-ring widths and carbon isotope ratios ( delta 13C) of tree-ring cellulose with annual climatic parameters in the northern and southern boreal forest. Contrary to expectations, climate correlations with ring widths at the northern and southern sites were similar in black spruce (Picea mariana (Mill.) BSP). Annual growth was favored by cooler and wetter conditions. For jack pine (Pinus banksiana Lamb.), increased temperature and spring precipitation favored annual growth at both sites. In the north, annual growth was negatively correlated with winter precipitation. The delta 13C - climate correlations in Pinus banksiana followed current distribution theories. In the south, potential evapotranspiration explained significant annual delta 13C variation, whereas in the north, winter and growing season precipitation influenced annual delta 13C variations. Our data support the concept that moisture limits the southern range of Pinus banksiana and cold soil temperatures limit the northern extent. However, colder, wetter conditions favored growth of Picea mariana throughout its range. These observations strengthen the concept that species respond individually to climate change, not as a cohesive biome.


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