摘要
基于1961-2014年岷江上游及其周边地区20个气象站点的观测资料,运用Mann-Kendal非参数检验方法分析了研究区近50 a的气候突变,结合DEM、土壤、水系、土地利用等数据构建了干旱河谷典型特征的诊断指标体系,准确地界定了岷江上游干旱河谷的范围并分析了其气候突变前后的变化。结果表明:(1)研究区气候突变的时间节点为1981年,当前气候条件(1982-2014年)下,岷江上游干旱河谷总长度约为151.63 km,面积约705.62 km^2(占区域总面积的2.94%),主要分布于松潘镇江关以下,经茂县凤仪镇至汶川县绵褫间的岷江干流,以及黑水河谷和杂谷脑河谷等岷江支流的两侧。(2)当前气候条件下干旱河谷较气候突变前(1961-1980年)覆盖河道两岸更宽的范围且向北延伸,长度增加20.87 km,面积增加81.61 km^2;(3)气候变暖和土地利用方式的改变是引起岷江上游干旱河谷范围扩大的主要原因。
Arid valley is characterized by fragile and sensitive ecological environment. According to the climat- ic, vegetation and soil features, arid valley can be divided into three types： arid hot valley, arid warm valley and arid genial valley. The arid valley in the upper reaches of Minjiang River, Sichuan Province, China, belongs to the typical arid warm valley. It is also the center of regional population distribution and the core area of social economy and culture development. So, the spatial definition of arid valley is the basis for ecological and geo- graphical research in the area. However, there is not a mature and complete system to define the range of arid val- ley. In view of this, firstly, based on the meteorological observation data from 1961 to 2014, as well as DEM, soil type, land use data, etc., this paper built an index system for diagnosing the characteristics of arid valley. Then, us- ing Mann-Kendal nonparametric test method, the abrupt climate change in the study area was analyzed in nearly 50 years. Finally, the AHP method and linear weighted summation method were adopted to calculate the index for reflecting the characteristics of the arid valley. According to the calculated index, the spatial rang of the arid valley in the upper reaches of Minjiang River were quantitatively defined. What＇s more, its range variation of the two periods before and after the climate change was analyzed. The results showed as follows： （ 1 ） Under current climatic conditions （ 1982 to 2014）, the total length of the arid valley of the upper reaches of Minjiang River was about 151.63 km, and the total area was about 705.62 km2, which was accounting for 2.94% of the administrative area. The arid valley was mainly distributed on the both sides of the main stream and the tributary of Minjiang River. （2） In 1981, the climate changed abruptly in this area. The total area of the arid valley in the period before the abrupt climate change （1961 to 1980） was about 624.02 km2. The total area increased 81.61 km2 in the next period after the climate change, and the length increased 20.87 km. Compared to the spatial range of two periods, the arid valley broadened its range and expanded to the north in current 30 years. （3） The arid valley in the upper reaches of Minjiang River was mainly covered by shrub woodland and moderate-high grassland. Compared to 1986, the area of farmland and construction land had increased 11.37 km： and 9.86 km2 respectively in 2014. Global warming and human activity jointly caused the expanding of the arid valley. （4） Compared to the result of field stLrveys by Institute of Mountain Hazards and Environment, CAS, the difference of the calculated area of ar- id valley in this paper was 14.38 km2, and the relative error was 2.00 percent. So, setting up an index system for diagnosing the characteristics of arid valley to define its spatial range was feasible. The result of arid valley range displayed high accuracy. It could provide a new idea and method for defining the range of the arid valley. Further- more, it laid the foundation data for ecological research in the arid valley area.
出处
《干旱区地理》
CSCD
北大核心
2017年第3期541-548,共8页
Arid Land Geography
基金
国家自然科学基金项目(41301653)
关键词
干旱河谷
空间界定
范围变化
气候突变
岷江上游
arid valley
spatial definition
range Variation
abrupt climate change
the upper reaches of Minjiang River
