2021
DOI: 10.1016/j.gecco.2021.e01698
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Vegetation responses to climate change in the Qilian Mountain Nature Reserve, Northwest China

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Cited by 43 publications
(38 citation statements)
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“…When the vegetation cover degree was high, NDVI and SPEI were negatively correlated; i.e., aridification promoted vegetation growth [63]. Guo et al [64] studied the response of vegetation with high coverage to precipitation and temperature in China's Qilian Mountain Nature Reserve, and the results show that there is a significant positive correlation between NDVI and temperature on an annual scale. This result is completely consistent with the results of this study on the NDVI of high-coverage vegetation with climate change.…”
Section: Impact Of Human Activities On Ndvimentioning
confidence: 99%
“…When the vegetation cover degree was high, NDVI and SPEI were negatively correlated; i.e., aridification promoted vegetation growth [63]. Guo et al [64] studied the response of vegetation with high coverage to precipitation and temperature in China's Qilian Mountain Nature Reserve, and the results show that there is a significant positive correlation between NDVI and temperature on an annual scale. This result is completely consistent with the results of this study on the NDVI of high-coverage vegetation with climate change.…”
Section: Impact Of Human Activities On Ndvimentioning
confidence: 99%
“…For example, the lower limit of J. przewalskii occurs at 2600 m in the Qilian Mountains [79], whereas its higher distribution range in southeastern Tibet (4200-4700 m a.s.l) [19] suggests a correlation with the higher elevation occurrence of BP there. In addition, our results demonstrated that the higher habitat suitability of EP and BP is strongly influenced by the temperature of the warmest month and annual mean temperature, respectively (Figure 4), which might be explained by the fact that temperature directly affects the distributional and seasonal changes of vegetation and then indirectly affects the potential distribution of Galliformes in the QMNNR [55,69]. There is a significant positive correlation between temperature and NDVI in the vegetation-climate relationship [69].…”
Section: Discussionmentioning
confidence: 70%
“…Similarly, we also assessed a monthly change in the number of different group sizes captured for each month in which camera traps were active. Based on the breeding phenology of the two target species [17,58] and local climate characteristics in the QMNNR [55,69], we divided the year into breeding (from April to July), non-breeding (from August to October) and winter seasons (from November to March). To explore if the degree of interspecific overlap in activity between EP and BP changes across seasons, we estimated the diel activity for both species by fitting a non-parametric circular kernel density estimation function [39] to the radian-transformed occurrence records, regarded as a random sampling from 24 h per day reflecting the animals' maximum true diel activity pattern [39].…”
Section: Data Analysesmentioning
confidence: 99%
“…The dynamic pattern of vegetation in the different elevation zones of Heihe River Basin is important to consider when explicating the differences of vegetation distribution and their responses to climate change from the gradient perspective [36]. On the basis of the DEM data and the spatial data of vegetation in the 1980s and 2010s, as well as by operating the ArcGIS software, this study classified the vertical distribution into six elevation zones, which considered the horizontal and vertical characteristics of vegetation distribution and climate elements in Heihe River Basin [14,[37][38][39][40]. Among them, oasis farmland and desert zone is located in the area of elevation less than 1700 m, desert steppe zone is distributed in the elevation range from 1700 to 2100 m, dry scrub-grassland zone is distributed in the elevation range from 2100 to 2500 m, mountain forest-steppe zone is located in the elevation range from 2500 to 3300 m, subalpine scrub-meadow zone is distributed in the elevation range from 3300 to 3800 m, and alpine cold desert-meadow zone is located in the area of elevation more than 3800 m.…”
Section: Classification Of the Vertical Vegetation Zonementioning
confidence: 99%