1956
DOI: 10.2307/1943287
|View full text |Cite
|
Sign up to set email alerts
|

Climate as a Determinant of Vegetation Distribution in Eastern Washington and Northern Idaho

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

2
49
0
1

Year Published

1968
1968
2017
2017

Publication Types

Select...
6
2
1

Relationship

0
9

Authors

Journals

citations
Cited by 66 publications
(52 citation statements)
references
References 62 publications
2
49
0
1
Order By: Relevance
“…If this is so, then the cause of its limitation could not be identified by indirect methods, such as: (i), the correlation of distribution with isometric lines of climate, e.g. Salisbury (1926), Enquist (1929), Iversen (1944), Dahl (1951) and Daubenmire (1956); (2) (3), by determining physiological responses to climate and failing to take into account the effect of climate on the overall growth processes of the plant, e.g. Wager (1941), Stocker (i960) and Mooney and Billings (1961).…”
Section: Reproductive Developmentmentioning
confidence: 99%
“…If this is so, then the cause of its limitation could not be identified by indirect methods, such as: (i), the correlation of distribution with isometric lines of climate, e.g. Salisbury (1926), Enquist (1929), Iversen (1944), Dahl (1951) and Daubenmire (1956); (2) (3), by determining physiological responses to climate and failing to take into account the effect of climate on the overall growth processes of the plant, e.g. Wager (1941), Stocker (i960) and Mooney and Billings (1961).…”
Section: Reproductive Developmentmentioning
confidence: 99%
“…Within this mostly forested region, topography and elevation create steep gradients of temperature and precipitation, over which major tree species are predictably stratified (Daubenmire 1956;Rehfeldt et al 2008). Human-induced climate change over recent decades has already been implicated in the distributional contraction of some Rocky Mountain tree species (Michaelian et al 2011;Gitlin et al 2006;Shaw et al 2005;Bell et al 2014a), and a consensus of global circulation models predict further increases in air temperatures and decreases in plant available moisture during the growing season throughout the region (Boisvenue and Running, 2010).…”
Section: Introductionmentioning
confidence: 99%
“…It has been reported that the α-diversity reaches its maximum in the most mesic part of moisture gradient (Daubenmire and Daubenmire, 1968;Glenn-Lewin, 1975;Terborgh, 1973) or has its optimum in the middle parts of the gradient (Auclair and Goff, 1971;Monk, 1965Monk, , 1967Whittaker, 1956;Whittaker and Niering, 1965). Furthermore, most xeric habitats have been documented to be least diverse (Daubenmire and Daubenmire, 1968;Moral, 1972) but the opposite trend has also been observed, i.e.…”
Section: α-Diversity Relationship With Moisture Gradientmentioning
confidence: 99%