globalchange  > 气候变化与战略
CSCD记录号: CSCD:5226014
论文题名:
重庆雾日的气候特征及变化
其他题名: Impact of Climate Change on Fog Days in Chongqing
作者: 张天宇; 孙佳; 王勇; 白莹莹; 程炳岩; 李永华
刊名: 西南大学学报. 自然科学版
ISSN: 1673-9868
出版年: 2014
卷: 36, 期:7, 页码:1170-1178
语种: 中文
中文关键词: 重庆 ; 雾日 ; 气温 ; 湿度
英文关键词: Chongqing ; fog day ; temperature ; humidity
WOS学科分类: METEOROLOGY ATMOSPHERIC SCIENCES
WOS研究方向: Meteorology & Atmospheric Sciences
中文摘要: 利用重庆地区1973-2010年气象观测资料,分析了重庆雾日的时空分布特征,探讨了重庆雾日与气候变化的关系,结果表明:重庆雾日时间上秋冬多,春夏少;空间上中西部多,东南东北少,西部以北多于西部以南.重庆(34个气象站)雾日的时间演变分成Ⅰ区(包括中部、主城、西部和西南部地区,20个站,代表站北碚)、Ⅱ区(包括东南部和东北部以西地区,9个站,代表站万州)、Ⅲ区(东北部以东地区,5个站,代表站云阳).全区平均与Ⅰ区和Ⅱ区的变化趋势是基本一致的,与Ⅰ区一致性好于Ⅱ区,而与Ⅲ区的变化趋势基本不一致.近38年来全区、Ⅰ区、Ⅱ区平均年雾日整体呈显著线性减少趋势,分别为-2.9 d/10 a、-3.2 d/10 a、-3.9 d/10 a.全区平均年雾日的阶段变化为先增后减,在20世纪90年代转为减少趋势.全区平均四季雾日的阶段变化与年雾日比较一致,总体都呈线性减少趋势,夏季减少相对最显著.温度和湿度变化与重庆地区雾日变化的关系密切.气温越高雾日越少, 平均气温升高1℃,重庆大部分地区雾日减幅在1~30 d,中北部减幅相对大,东北部减幅相对小;全区平均将减少8 d.湿度越大雾日越多,平均相对湿度增加1%,重庆大部分地区雾日增幅在1~6 d,西北部和中北部增幅相对大,东北部和东南部增幅相对小;全区平均将增加3 d.
英文摘要: The long-term meteorological data of Chongqing in the period of 1973-2010 are used to analyze the spatial and temporal distribution of fog days and the influence of climate change on them.The results show that,temporally,autumn and winter have more fog days than spring and summer in Chongqing and,spatially, the mid-west of the municipality has more fog days than its southeast and northeast regions.As for its west region,the north part has more fog days than the south part.Based on the temporal evolution of fog days,the 34 meteorological stations of Chongqing are divided into 3 districts,i.e.District I,including 20 stations in the main urban area and middle,west and southwest regions,with the Beibei Station as their representative, District II,including 9 stations in the areas west to its southeast and northeast regions,with the Wanzhou Station as their representative,and District III,including 5 stations in the areas east to its northeast region,with the Yunyang Station as their representative.The average data of Chongqing can perfectly represent the changing trend of DistrictⅠand can represent DistrictⅡ nicely,but cannot represent DistrictⅢ.In the recent 38 years,the average fog days in the whole region,DistrictⅠand DistrictⅡshow a significant linear decrease trend,at a rate of-2.9 d/10 a,-3.2 d/10 a,and -3.9 d/10 a,respectively.The average annual fog days show an increasing trend before the 1990's and decrease after that.The phase changes of fog days during the four seasons and the annual fog days are consistent.The fog days in the four seasons are generally in a linear decreasing trend,the fog days in summer are reducing significantly compared to the other seasons.Changes in temperature and humidity in Chongqing are closely related to variations in fog days.Fog days are in a negative correlation with temperature.Whenever the average temperature rises by 1℃,the fog days in most parts of Chongqing are reduced by 1-30 d.The reducing range in the middle and the northern regions is more significant than that in the northeastern region;the average fog days may be reduced by about 8 d in the whole region.Fog days are in a positive correlation with humidity.Whenever the average relative humidity increases by 1%,fog days in most parts of Chongqing may increase by 1-6 d,the range of increase is greater in the northwestern and northern regions than in the northeastern and southeastern regions,and the fog days in the whole Chongqing area will be increased by 3 d on the average.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/148517
Appears in Collections:气候变化与战略

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作者单位: 重庆市气候中心, 重庆 401147, 中国

Recommended Citation:
张天宇,孙佳,王勇,等. 重庆雾日的气候特征及变化[J]. 西南大学学报. 自然科学版,2014-01-01,36(7):1170-1178
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