Variations in suspended and dissolved matter fluxes from glacial and non-glacial catchments during a melt season at Urumqi River, eastern Tianshan, central Asia

CATENA ◽  
2012 ◽  
Vol 95 ◽  
pp. 42-49 ◽  
Author(s):  
Zhongqin Li ◽  
Wenhua Gao ◽  
Mingjun Zhang ◽  
Wenyu Gao
The Holocene ◽  
2020 ◽  
pp. 095968362097026
Author(s):  
Jiangsong Zhu ◽  
Jian Ma ◽  
Fan Zhang ◽  
Yinqiu Cui ◽  
Marcella Festa ◽  
...  

Andronovo has been regarded as one of the most powerful cultures in Central Asia, which reflected frequent cultural interflow, people migration, and technique diffusion on the Bronze Age Eurasian steppes. In the past decade, many new discoveries in Xinjiang, such as Adunqiaolu and Jartai, have drawn broad attention to the communication of the Andronovo culture in the central Tianshan Mountains. However, systematic study is still insufficient on the communication and influence of the Andronovo culture or the “Andronovo phenomenon” along the Tianshan Mountains. Based on our comprehensive investigation of tomb structure, funeral rituals and assemblages, this article reclassifies relevant Andronovo remains in Xinjiang into five categories. Two categories represented by the Xiabandi cemetery and the Adunqiaolu show clear resemblance to those at Semirech’ye in all aspects, which indicated people in these regions may have maintained close and consistent interaction. Other three categories in the Kuokesuxi and Tangbalesayi cemetery have different tomb structures and funeral rituals from those typical discoveries of the Andronovo cultures in Central Asia in spite of the their similarity in pottery and bronze ornaments, which can be considered as the result of product exchange or technical communication, rather than population migration. New discovery of the Baigetuobie cemetery with evidence of tomb structure, dating, and human genetic features in the Balikun grassland suggested that there might be a small group of people, probably came from the central Tianshan Mountains or Semirech’ye or further west, had migrated to the Eastern Tianshan Mountains about 1600 BC, which was likely facilitated by the relatively warm and humid environment. They had preserved their traditional tomb architecture and were not active in cultural interaction and population fusion with people of Hami Oasis in the south. Due to some reason unknown, people of Baigetuobie had faded away from Balikun grassland after a short time.


2011 ◽  
Vol 66 (1) ◽  
pp. 265-273 ◽  
Author(s):  
Puyu Wang ◽  
Zhongqin Li ◽  
Huilin Li ◽  
Min Cao ◽  
Wenbin Wang ◽  
...  

2009 ◽  
pp. n/a-n/a ◽  
Author(s):  
Zhongqin Li ◽  
Wenbin Wang ◽  
Mingjun Zhang ◽  
Feiteng Wang ◽  
Huilin Li

Atmosphere ◽  
2020 ◽  
Vol 11 (10) ◽  
pp. 1079
Author(s):  
Yufeng Jia ◽  
Zhongqin Li ◽  
Chunhai Xu ◽  
Shuang Jin ◽  
Haijun Deng

Precipitation is a key process in the hydrologic cycle. However, accurate precipitation data are scarce in high mountainous areas, mainly restricted by complex topography, solid precipitation and sparse recording stations. In order to evaluate the quality of precipitation measurement, this study conducted a comparison campaign of precipitation measurements with the PWS100 laser sensor and the Geonor T-200B rain gauge for an entire year from 30 April 2018 to 1 May 2019 at an elevation of 3835 m in a nival glacial zone in eastern Tianshan, Central Asia. The results show that the daily precipitation values recorded by Geonor T-200B and PWS100 are well correlated and the annual precipitation amounts recorded by the two instruments differ by 7%, indicating good capabilities of both instruments in solid precipitation measurement. However, the amount of precipitation measured by Geonor T-200B was 36 mm lower in June to August and 120 mm higher in the remaining months compared with the values measured by PWS100. Our study indicated that Geonor T-200B is more efficient than PWS100 in terms of catching solid precipitation measurements. According to the PWS100 data, the experiment site was dominated by solid precipitation particles, accounting for 60% of total precipitation particles. Based on the precipitation particle and in-situ air temperature measurements, a set of temperature thresholds were established to discriminate rain, sleet and snow. The threshold temperature of rainfall and snowfall is −1.5 and 8 °C, respectively. When air temperature ranges from −1.5 to 8 °C, sleet occurs, meanwhile the ratio of rain to snow depends on air temperature.


2012 ◽  
Vol 57 (34) ◽  
pp. 4505-4509 ◽  
Author(s):  
KeQin Duan ◽  
TanDong Yao ◽  
NingLian Wang ◽  
HuanCai Liu

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