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1	Regeneration patterns in the Mountain hemlock zone Klinka, Karel, Brett, Bob, Chourmouzis, Christine January 1997 (has links) The Mountain Hemlock (MH) zone includes all subalpine forests along British Columbia’s coast. It occurs at elevations where most precipitation falls as snow and the growing season is less than 4 months long. The zone includes the continuous forest of the forested subzones and the tree islands of the parkland subzones (Figure 1). Old-growth stands are populated by mountain hemlock, Pacific silver fir, and Alaska yellow-cedar, and are among the least-disturbed ecosystems in the world. Canopy trees grow slowly and are commonly older than 600 years, while some Alaska yellow-cedars may be up to 2000 years old. Understanding regeneration patterns in the MH zone has become increasingly important as logging continues towards higher elevations of the zone where snowpacks are deeper. Alaska yellow-cedar Canopy trees Forest regeneration Gap dynamics Mountain hemlock Pacific silver fir Snow Stand structure Subalpine fir Subalpine forest Tree-island model Western hemlock
2	Determining and Comparing Hydraulic Behavior among Trees with Differing Wood Types in a Temperate Deciduous Forest Bryant, Kelsey N. 25 May 2021 (has links) No description available. Physiology Plant Sciences Ecology Environmental Science Climate Change Forestry Wood Tree physiology Xylem anatomy Ring-porous Diffuse-porous Sap flux Hydraulic behavior Isohydric continuum Tree size Temperate forests Deciduous forests Vapor pressure deficit Leaf water potential Mature trees Canopy trees

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Regeneration patterns in the Mountain hemlock zone

Determining and Comparing Hydraulic Behavior among Trees with Differing Wood Types in a Temperate Deciduous Forest