Characteristics of summer regional rainfall events over Ili River Valley in Northwest China

2020 ◽  
Vol 243 ◽  
pp. 104996 ◽  
Author(s):  
Liangliang Li ◽  
Jian Li ◽  
Rucong Yu
2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Wen-Wen Li ◽  
Li-Qiang Liu ◽  
Qiu-Ping Zhang ◽  
Wei-Quan Zhou ◽  
Guo-Quan Fan ◽  
...  

AbstractTo clarify the phytogeography of Prunus armeniaca L., two chloroplast DNA fragments (trnL-trnF and ycf1) and the nuclear ribosomal DNA internal transcribed spacer (ITS) were employed to assess genetic variation across 12 P. armeniaca populations. The results of cpDNA and ITS sequence data analysis showed a high the level of genetic diversity (cpDNA: HT = 0.499; ITS: HT = 0.876) and a low level of genetic differentiation (cpDNA: FST = 0.1628; ITS: FST = 0.0297) in P. armeniaca. Analysis of molecular variance (AMOVA) revealed that most of the genetic variation in P. armeniaca occurred among individuals within populations. The value of interpopulation differentiation (NST) was significantly higher than the number of substitution types (GST), indicating genealogical structure in P. armeniaca. P. armeniaca shared genotypes with related species and may be associated with them through continuous and extensive gene flow. The haplotypes/genotypes of cultivated apricot populations in Xinjiang, North China, and foreign apricot populations were mixed with large numbers of haplotypes/genotypes of wild apricot populations from the Ili River Valley. The wild apricot populations in the Ili River Valley contained the ancestral haplotypes/genotypes with the highest genetic diversity and were located in an area considered a potential glacial refugium for P. armeniaca. Since population expansion occurred 16.53 kyr ago, the area has provided a suitable climate for the population and protected the genetic diversity of P. armeniaca.


2018 ◽  
Vol 10 (5) ◽  
pp. 781-793 ◽  
Author(s):  
Wei Jiao ◽  
Yaning Chen ◽  
Weihong Li ◽  
Chenggang Zhu ◽  
Zhi Li

2018 ◽  
Vol 38 (13) ◽  
pp. 4979-4989 ◽  
Author(s):  
Weihua Yuan ◽  
Hang Xu ◽  
Rucong Yu ◽  
Jian Li ◽  
Yingxin Zhang ◽  
...  

2020 ◽  
Vol 54 (7-8) ◽  
pp. 3245-3258
Author(s):  
Xuelin Hu ◽  
Weihua Yuan ◽  
Rucong Yu ◽  
Minghua Zhang

Author(s):  
Guo jing ◽  
Zhang renping ◽  
Wang ranghui ◽  
Yusupujiang aimaiti ◽  
Asiyemu tuerdi ◽  
...  

2020 ◽  
Author(s):  
Xuelin Hu

<p>Accurate simulation and prediction of intense precipitation events require better understanding of their physical mechanisms. This study uses Yaan—a place with regional maximum rainfall in central China—to investigate the cause and process of intense precipitation. Hourly rain gauge records and the new ERA5 reanalysis are used to characterize the evolution process of warm season intense regional rainfall events (RREs) in Yaan and its associated three-dimensional circulation. Results show that before the start of the Yaan intense RREs, moderate rainfall amount (frequency) appears northeast of the key region. The rainfall then moves southward in the following several hours along the eastern periphery of the Tibetan Plateau where it reaches peak. It then moves to and end up in the south and southeast Sichuan Basin. The progression of the RREs is found to be associated with a counter-clockwise rotation of anomalous surface winds associated with a developing mesoscale surface low-pressure center, which is further associated with the southeastward progression of a large-scale synoptic scale wave. The easterly phase of the winds in the counter-clockwise rotation causes upslope motion perpendicularly toward the terrain that leads to maximum rainfall. The findings illustrate how large-scale circulations, mesoscale systems, and specific topographic features interact to create the RREs evolution in Yaan.</p>


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