2020
DOI: 10.5846/stxb201811262562
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Variation of leaf and root traits and ecological adaptive strategies along a precipitation gradient on Changtang Plateau

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Cited by 5 publications
(3 citation statements)
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“…Vegetative (especially leaves) and roots are essential for plants to acquire resources. Plant morphologically changes with the environmental gradient to obtain most of the resources and strategies ecologically to adapt to environmental changes [ 94 ]. Under both water and salt stress in the Qaseem region, the roots of A. lagopoides adopted a strategy of root development and expansion to obtain resources to improve their adaptive ability.…”
Section: Discussionmentioning
confidence: 99%
“…Vegetative (especially leaves) and roots are essential for plants to acquire resources. Plant morphologically changes with the environmental gradient to obtain most of the resources and strategies ecologically to adapt to environmental changes [ 94 ]. Under both water and salt stress in the Qaseem region, the roots of A. lagopoides adopted a strategy of root development and expansion to obtain resources to improve their adaptive ability.…”
Section: Discussionmentioning
confidence: 99%
“…In general, precipitation in northern Tibet decreased while temperature increased before the implementation of the Project (Fig. 6), causing the local environment to be drier, and the increase of evapotranspiration intensity was greater than that of precipitation, resulting in a decline in water conservation capacity (Lu et al, 2020; Zhao et al, 2020). Although the temperature in northern Tibet continued to rise slowly after the Project, an increase in rainfall offset the impact of the temperature rise (Du et al, 2008; Song et al, 2012; Yin et al, 2013; Shao et al, 2022).…”
Section: Discussionmentioning
confidence: 99%
“…The climate in north Tibet was typical plateau monsoon climate. The temperature in northern Tibet exhibits a gradient decline from south to north, annual average temperature in most places is below 0 °C, and the average temperature of the warmest month is less than 14 °C (Yang et al, 2003); the annual average precipitation is between 50mm and 700 mm, with the gradient decreasing gradient from southeast to northwest (Zhao et al, 2020). Most places in this region have annual sunshine hours more than 2500 h, the annual average wind speed is larger than 4 m s –1 , thus the annual evaporation is greater than 1800 mm, and the annual average aridity index (AI) is between 1.6 and 20.0 (Mao et al, 2006).…”
Section: Methodsmentioning
confidence: 99%