Variation and abrupt change of climate in Ili River Basin, Xinjiang

2010 ◽  
Vol 20 (5) ◽  
pp. 652-666 ◽  
Author(s):  
Huilan Sun ◽  
Yaning Chen ◽  
Weihong Li ◽  
Feng Li ◽  
Yapeng Chen ◽  
...  
2017 ◽  
Vol 2017 ◽  
pp. 1-13 ◽  
Author(s):  
Xiaojing Shen ◽  
Xu Wu ◽  
Xinmin Xie ◽  
Zhenzhen Ma ◽  
Meijian Yang

The monthly accumulated precipitation and monthly average temperature of 117 meteorological stations in Song-Liao River Basin (SLRB) were used to calculate the Standardized Precipitation Evapotranspiration Indices (SPEI) to analyze the drought characteristics, including long-term trends, drought affected area, climate abrupt change, intensive drought occurrence regions, and drought durations during 1964–2013 with the support of GIS. The Area Drought Severity (ADS), a comprehensive index, is proposed to assess both the variations of drought degree and the extent of the drought affected area. The results revealed that (1) the drought happening probability and degree are rising and the affected areas of all degrees of drought have an increasing trend during the last 50 years; (2) there is a climate abrupt change which occurred in around 1994, and the area with declining SPEI is larger than that with declining SPI, which could be due to the rising temperature after the climate abrupt change; (3) all degrees of drought occurrence probability increased, and the intensive drought occurrence regions altered from the northern SLRB to the southwestern SLRB after the climate abrupt change; (4) the drought duration increased from 1994, and the increased drought durations occurred in most parts of SLRB.


2014 ◽  
Vol 28 (10) ◽  
pp. 2851-2866 ◽  
Author(s):  
Mingyong Cai ◽  
Shengtian Yang ◽  
Hongjuan Zeng ◽  
Changsen Zhao ◽  
Shudong Wang

Author(s):  
Huashan Xu ◽  
Yufen Ren ◽  
Hua Zheng ◽  
Zhiyun Ouyang ◽  
Bo Jiang

During the past decades, runoff has been highly influenced by climate change and human activities in Haihe River basin, and it is important to analyze the runoff trends and the drivers of its change to guide water resources management. The Mann–Kendall method and Pettitt test were conducted to analyze the hydrological and climate trends. Data from six sub-basins were used, including runoff at six representative hydrological stations and precipitation and air temperature at 49 meteorological stations. We used multiple-regression analysis and policy review to explore the influence of climate change and human activities on the runoff change at six sub-basins. According to the results, annual runoff showed a significant downward trend at six hydrological stations (p < 0.05), and the most probable change points at all stations showed up during the period from the late 1970s to the early 1980s. Moreover, the middle and late 1990s could be another probable abrupt change point at Luan River and Chaobai River. The declining trend of the annual mean precipitation at the six sub-basins was insignificant (p > 0.05), and there were no significant abrupt change points except the Zhang River area (p < 0.05). Compared with the precipitation trend, the annual mean air temperature exhibited a significant increasing trend at all stations, and the period from the late 1980s to the early 1990s might be the most probable abrupt change points at all four sub-basins. The trend analysis and the abrupt change point analysis suggest that mean air temperature is the main climate factor that will lead to the decline in the runoff time-series, while the insignificant downward trend of the precipitation might accelerate the downward trend of the runoff data. Through elevant policy measures, including land-use reform and the construction of the Three-North (north, northeast, and northwest China) Shelter Forest, China started to implement a family-contract responsibility system and initiated the first stage of construction of the Three-North Shelter Forest Program in 1978. The land-use reform policies greatly stimulated the peasants’ initiative for land management and significantly changed the land use pattern and water use quantity in the Haihe River basin in a short time. Besides, the precipitation decreased and the air temperature rose, so an abrupt change in runoff occurred from the late 1970s to the early 1980s. The abrupt change in the runoff in the middle and late 1990s highly tallied with the construction time of the Three-North Shelter Forest Program. After near 20 years of construction of the Three-North Shelter Forest Program, the forest area increased, the forest quality had been improved, and the vegetation coverage on the underlying surface had been changed significantly, so the construction of the Three-North Shelter Forest Program was an important cause of runoff change in the middle and late 1990s. Also, change in precipitation and air temperature enlarged the effect of change in the runoff.


Water ◽  
2019 ◽  
Vol 11 (4) ◽  
pp. 861
Author(s):  
Steven G. Pueppke ◽  
Qingling Zhang ◽  
Sabir T. Nurtazin

In the published article [...]


2015 ◽  
Vol 2015 ◽  
pp. 1-12 ◽  
Author(s):  
Junli Xu ◽  
Shiyin Liu ◽  
Wanqin Guo ◽  
Zhen Zhang ◽  
Junfeng Wei ◽  
...  

The Ili River originates in the Tian Shan Mountains of Northwest China before flowing into Kazakhstan and Lake Balkash. Melting snow and ice are its major contributors. We analyzed glacial changes in the upper Ili River basin between the 1960s and 2007/2009 using topographic maps and satellite imagery from a Landsat TM. The relationships between glacial changes and glacial size, topographic factors, and debris cover were examined. Our results found that total glacial area decreased by 485 ± 177.3 km2(24.2% ± 8.8%) during the study period, and there were no advancing glaciers. Additionally, 331 glaciers disappeared and 18 disintegrated into two or three smaller glaciers. This study demonstrated a linear relationship between glacial area change and elevation. Changes in glaciers smaller than 1 km2were affected by both glacial size and topographic factors, while larger ones were affected by size only. Area losses in debris-covered glaciers were smaller by 2.5% to 7.5% compared to clean ice of the same size in this basin. As in other glaciated regions, glacial retreat in the Ili River basin is attributed to global warming. The slightly increasing precipitation over the study period could not offset the ice melting.


2019 ◽  
Vol 5 (1) ◽  
pp. 50-76
Author(s):  
Cmr. Zhuangsheng

In the sixteenth century, the Sibe people emerged as a unique ethnic group, and they remained a unique ethnic group after their migration to the Ili River basin. In the Republic of China, a time when many ethnic systems were created, the Sibe gained official recognition for being an independent ethnic group. Although the creation of a written script is an act of ethnic construction, the Sibe written language could never break free of its close relation to the Manchu written language. The construction of ethnic groups and the creation of written scripts stimulated vigorous development of ethnic histories compiled by the Sibe scholars, and it is their textual research of ethnic origin that best illustrates the birth of this new ethnic group.


1987 ◽  
Vol 24 (11) ◽  
pp. 2130-2140 ◽  
Author(s):  
Daniel E. Kerr

This paper describes the principal glaciolacustrine deposits of a sequence of overlapping ice-marginal lakes known as glacial Lake Richardson and its transition to a postglacial sea following the retreat of a lobe of the Laurentide ice sheet from the Richardson and Rae River basin. The glaciolacustrine to marine transition is characterized by an upward-fining sequence of facies deposited in proglacial lacustrine environments, succeeded by an upward-coarsening trend corresponding to a regressive marine sequence. A composite stratigraphic section includes (a) basal diamicton, (b) stratified subaqueous sand and gravel, (c) glaciolacustrine silty clay rhythmites, (d) massive marine silty clay, and (e) littoral marine sands. The sudden passage from lacustrine to marine environments is reflected in the abrupt change in depositional mechanisms. Turbidity currents prevailed in the proglacial lake as inferred from thick sequences of varve-like couplets, whereas the salinity of marine waters, impeding the sedimentation of fines by density underflows, led to the deposition of massive structureless marine silty clays by flocculation.


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