干旱气象 ›› 2019, Vol. 37 ›› Issue (3): 454-.

• 论文 • 上一篇    下一篇

1987—2016年安徽省暑期体感温度时空变化特征

姚镇海1,姚叶青1,王传辉1,樊凡2,施国萍3   

  1. 1.安徽省公共气象服务中心,安徽合肥230031;2.安徽省舒城县气象局,
    安徽舒城231300;3.南京信息工程大学地理科学学院,江苏南京210044
  • 出版日期:2019-06-28 发布日期:2019-07-01
  • 通讯作者: 姚叶青(1970— ),女,硕士研究生,高级工程师,主要从事专业气象服务研究.E-mail:zmhht@163.com。
  • 作者简介:姚镇海(1989— ),男,硕士研究生,工程师,主要从事公共气象服务.E-mail:1719690761@qq.com。
  • 基金资助:
    安徽省气象局科研项目(RC201804)和安徽省气象局预报员专项(kY201806)共同资助

Temporal and Spatial Characteristics of Somatosensory Temperature in Summer Holiday in Anhui Province During 1987-2016

YAO Zhenhai1, YAO Yeqing1, WANG Chuanhui1, FAN Fan2, SHI Guoping3   

  1. 1. Anhui Public Meteorological Service Center, Hefei 230031, China;
    2. Meteorological Bureau of Shucheng County of Anhui Province, Shucheng, 231300, Anhui, China;
    3. College of Geographical Science, Nanjing University of Information Science and Technology, Nanjing 210044, China
  • Online:2019-06-28 Published:2019-07-01

摘要: 基于安徽省1987—2016年81个国家站暑期7、8月逐日平均气温、最高最低气温差、平均相对湿度和平均风速,计算各站点体感温度,并分析其逐年变化特征。联合站点体感温度和DEM地形数据,建模并给出体感温度的空间分布;依据舒适度划分等级,得到安徽省暑期舒适度空间分布。结果表明:(1)安徽省近30 a暑期体感温度呈波动上升趋势;与平均气温、平均相对湿度呈正相关,与最高最低气温差、平均风速呈负相关;平均气温、平均相对湿度的上升,高低温差、平均风速的下降,使得体感温度呈上升趋势,其气候倾向率(0.0224 ℃·a-1)略高于平均气温的气候倾向率(0.016 ℃·a-1)。(2)体感温度随地形变化特征显著。沿淮部分地区与沿江大部平原地区普遍超过29.0 ℃;受海拔、植被覆盖、地形遮蔽效应影响,大别山、皖南山区大部体感温度低于27.0 ℃。(3)沿淮淮北、江淮大部、沿江等平原地区多为“较不舒适”地区;大别山、皖南山区均包含“最舒适”、“舒适”和“较舒适”地区。山区地形遮蔽效应与高植被覆盖为安徽省避暑旅游提供了良好的区域气候条件。

关键词: 安徽省, 体感温度, 时空变化特征

Abstract: The somatosensory temperature of each station was calculated and their annual variation characteristics were analyzed using daily average temperature, difference between maximum and minimum temperature, average relative humidity and wind speed of 81 national meteorological observation stations in Anhui Province from July to August during 1987-2016. Spatial distribution of somatosensory temperature in summer holiday was given through combining site average somatosensory temperature and DEM topographic data. According to the classification of comfort level, the comfort in summer holiday in Anhui Province was obtained. The results were as follows: (1) Somatosensory temperature in summer holiday in Anhui Province showed a fluctuating upward trend in recent 30 a. It was positively correlated with average temperature and average relative humidity, while negatively correlated with difference between maximum and minimum temperature and average wind speed. The increase of average temperature, average relative humidity and decrease of maximum and minimum temperature difference, average wind speed promoted the upward trend of somatosensory temperature with climate tendency rate (0.0224 ℃·a-1) slightly bigger than that (0.016 ℃·a-1) of average temperature. (2) Somatosensory temperature changed with topography significantly and it generally exceeded 29.0 ℃ in most plain areas along the Yangtze and Huaihe Rivers. Affected by elevation, vegetation cover and topographic shelter effect, somatosensory temperature in most areas of Dabie Mountains and Southern Anhui Mountains was below 27.0 ℃. (3) Plain areas along Huaibei, most of Jianghuai region and plain areas along the Yangtze River were mostly “less comfortable” areas. Both Dabie Mountains and Southern Anhui Mountains contained “most comfortable”, “comfortable” or “more comfortable” areas. The topographic shelter effect and high vegetation cover in mountainous areas provided resonable regional climate conditions for summer tourism in Anhui Province.

Key words: Anhui Province, somatosensory temperature, temporal and spatial characteristics

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