J4 ›› 2003, Vol. 21 ›› Issue (3): 63-68.

• 论文 • 上一篇    下一篇

北京市城、郊气候要素对比研究

宋艳玲1董文杰1张尚印1张德宽1王守荣1胡宝昆2   

  1. 1.国家气候中心北京100081 ;2.北京市气象局北京100089
  • 收稿日期:2003-07-31 修回日期:2003-09-18 出版日期:2003-09-30 发布日期:2003-09-30
  • 作者简介:宋艳玲(1974),女,河北省秦皇岛市人,硕士研究生,主要从事气候变化的研究和评价工作
  • 基金资助:

    本文得到国家重点科技项目《中国短期气候预测系统研究》加强课题的支持

Study on Characteristics of Climate Dements in Beijing

SONG Yan-Ling1, DONG Wen-Jie1, ZHANG Chang-Yi1, ZHANG De-Kuan1, WANG Shou-Rong1, HU Bao-Hun2   

  1. 1 .National Climate Center .Beijing  100081 ,China;2.Beijing Meteorological Bureau ,Beijing  100089 ,China
  • Received:2003-07-31 Revised:2003-09-18 Online:2003-09-30 Published:2003-09-30

摘要:

利用北京市市区4个站点和郊区3个站点40a的气候资料,分析了北京市城、郊平均气温、降水、日照、能见度和相对湿度的变化特征。研究发现:40a来北京市城、郊年平均气温明显上升,城区气温平均升温幅度为0. 43 0C/ 10a,郊区气温平均升温幅度为0. 21 0C/ 10a。北京市热岛效应明显增强,城、郊气温年代变化特征中,城、郊温差20世纪60年代最小,90年代最大;在城、郊气温年际变化特征中,1961^-1977年城、郊温差较小,1978^-2000年城、郊温差较大。在城、郊气温季变化特征中,冬季城、郊季平均气温温差最大,春季城、郊季平均气温温差最小。近几年虽然高温( X35 0C}日数明显增多,但是年最高气温变化小大,只有1997年、1999年和2000年年最高气温超过38℃。北京市年日照时数呈明显下降趋势,城区40a来日照时数下降幅度为78.9h/l0a,城、郊日照时数差异随季节有小同的变化,并且秋季最大,1961^-2000年秋季郊区日照时数比如区平均多0.34h0 40a来北京市年降水量略有减少,且年降水量变化幅度很大,城区40a来降水量减少幅度为45. 2mm/ 10a,由于城市化影响,下垫面性质改变,城区<10 mm的降雨日数远远小于郊区,40a间城区

关键词: 热岛效应, 高温日数, 年代际变化特征

Abstract:

Variations of mean temperature in Beijing city are analyzed in this paper by using climatological data of 4 stations in city and 3 stations in suburb.  We found that the difference of temperature was great in daily.seasonal.annual and decade.the difference of temperature between city and suburb was largest in winter and the mean seasonal temperature in city was higher 1 .11 0Cthan that in suburb .while the difference was smallest in firing;For the inter一annual variability of temperature .the difference was little from 1961 to 1977 .while the difference was great from 1978 to 2000.so the heat island effect was reinforced from 1978 to 2000;the did ference of temperature was least in 1960's .whereas the difference was maximal in 1990's;the number of high temperature day() 35冯was going up obviously ,but the highest temperature was not changed greatly .the mean annual temperature was increasing apparently during last 40 years .and it was increasing by 0. 43/10a in city and 0.21/10a in suburb. the sunshine time decreased obvr
ously in Beijing .and the decreasing range was 78. 9 hours 10a during the last 40 years.and the difference in autumn between city and suburb
was largest in whole year.  The precipitation also reduced recent years .furthermore the change of yearly precipitation was great .and the d}
creasing range of precipitation was 45. 2mm/ 10a in Beijing city.  Following the development of city.the days when the precipitation was less
than lOmm were more in city than in suburb.  The visibility was great in February.May.September and October in B句ing.the number of
low visibility(< 4km) was increasing ,the visibility was decreasing in recent years and the visibility in city was obviously lower than in sulr
urb.  The relative humidity was also decreasing in recent years in city .and the decreasing range was 1.6%for every 10 years.further rrxrre
the relative humidity in city was less than in suburb .it showed dry island effect.

Key words: the heat island effect , the number of high temperature day , inter一annual change