近50年新疆地区降水变化及天气分型
[Abstract]:Under the background of global climate change, it is of great scientific and social significance to study the regional characteristics of precipitation changes and the weather situation affecting precipitation in Xinjiang. In this paper, the daily precipitation data of 47 meteorological stations in Xinjiang from 1961 to 2013 are selected to analyze the temporal and spatial distribution of precipitation in Xinjiang, and the climatic zoning of summer precipitation in Xinjiang is carried out by using EOF,REOF method. The results show that the precipitation in Xinjiang region shows a continuous increasing trend from 1961 to 2013. After 1987, the precipitation is on the high side. Summer is the season that contributes most to the annual precipitation in Xinjiang in one year, which dominates the spatial distribution of annual precipitation and the changing trend of annual precipitation. The annual precipitation in Xinjiang is more and less in the north and south, and the precipitation in the whole of Xinjiang is rising. The four modes of EOF reflect the consistency of the summer precipitation changes in Xinjiang, and the blocking of the Tianshan Mountains causes the difference between the changes in the south and the north of Xinjiang, and the four modes of EOF reflect the consistency of the summer precipitation in Xinjiang. There are inverse variations of summer precipitation in eastern and western Xinjiang, central Tianshan mountain area and other areas. The REOF results further show the sensitive areas of summer precipitation anomaly in Xinjiang, which can be divided into five regions. The average annual precipitation of the five regions all showed an increasing trend, with the largest increasing trend in summer, the largest average annual precipitation in the two regions, the third in the fifth region and the fastest in the fifth region. The SOM neural network algorithm is used to classify the daily sea level pressure field from May to September from 1961 to 2013 in the study area including Xinjiang, and 35 types of weather patterns are obtained. Combined with precipitation data, the main weather systems affecting summer precipitation in Xinjiang, especially in northern Xinjiang, are the frontal systems which occur before the surface cyclones and surface high in May, July and September. The contribution of each climate type to the annual precipitation indicates that nearly 50% of the expected annual precipitation in Xinjiang is concentrated in the 13 nodes which contribute more to the precipitation in Xinjiang. NAO is one of the important factors in the inter-annual variation of precipitation in Xinjiang. The NAO index is negatively correlated with the annual precipitation in Xinjiang and negatively correlated with the annual precipitation increment. The SOM weather classification is of great importance to the study of precipitation in Xinjiang. In the year of NAO anomaly, the intensity anomaly of Icelandic low and North Atlantic high influenced the precipitation activity in Xinjiang by cooperating with the development and movement of high altitude and surface weather system. Therefore, it is of great significance to master the abnormal variation law and forecast of NAO index for precipitation forecast in Xinjiang.
【学位授予单位】:南京大学
【学位级别】:硕士
【学位授予年份】:2017
【分类号】:P426.6
【参考文献】
相关期刊论文 前10条
1 刘焕才;李曼;石培宏;刘力;孙建勇;;NAO对青藏高原中东部夏季降水双极振荡模态影响的时间尺度厘定[J];高原气象;2015年03期
2 胡钰玲;王遂缠;王式功;尚可政;宁贵财;康彩燕;;2012年初夏西北干旱区罕见区域性大暴雨天气过程分析[J];干旱气象;2015年01期
3 慈晖;张强;张江辉;白云岗;刘剑宇;;1961-2010年新疆极端降水过程时空特征[J];地理研究;2014年10期
4 赵直;徐晗;;新疆开都河流域近50a径流量年际年内变化及其对气候变化的响应分析[J];干旱区资源与环境;2014年10期
5 戴新刚;汪萍;张凯静;;近60年新疆降水趋势与波动机制分析[J];物理学报;2013年12期
6 毛炜峄;樊静;沈永平;杨青;高前兆;王国亚;王顺德;吴素芬;;近50a来新疆区域与天山典型流域极端洪水变化特征及其对气候变化的响应[J];冰川冻土;2012年05期
7 张延伟;魏文寿;姜逢清;刘明哲;王雯雯;白磊;韩茜;洪雯;陆恒;李雪梅;;近50年新疆气温和降水量变化及其与NAO指数的交叉小波谱分析[J];高原气象;2012年04期
8 陈春艳;孔期;李如琦;;天山北坡一次特大暴雨过程诊断分析[J];气象;2012年01期
9 代倩;段善旭;蔡涛;陈昌松;陈正洪;邱纯;;基于天气类型聚类识别的光伏系统短期无辐照度发电预测模型研究[J];中国电机工程学报;2011年34期
10 李剑锋;张强;陈晓宏;白云岗;;新疆极端降水概率分布特征的时空演变规律[J];灾害学;2011年02期
,本文编号:2459115
本文链接:https://www.wllwen.com/shoufeilunwen/benkebiyelunwen/2459115.html