【摘要】 <正>为了弄清上海城市热岛效应,应用了下列资料: (1) 1955年上海外滩、徐家汇(这两站代表市区)和松江(代表远郊)的全年观测资料。 (2) 1956、1957两年上海徐家汇(市区)、龙华(城市边缘)和松江(远郊)观测资料。 (3) 1959年8月9—11日,由上海气象局、华东师范大学和同济大学等单位用阿斯曼通风干湿表,对上海市区进行了33个定点(测点位置分布见图1)、逐时四层次(20、50、更多还原

【Abstract】 Shanghai is the biggest and most important industrial and commerical center inChina. Multiple observations show that the urban area is nearly always wanner. Forexample, on Dec. 13, 1979 at 8pm. (a calm dear night) the warmest temperature isotherms (8.5°) were associated with the highest density urban dwellings (fig 2). Some ave-rage records in the coldest temp., annual temp., the number of coldest days and hottestdays all indicated the urban heat effect as shown in table 1-2.The diurnal variation, annual variation and local difference of urban heat islandintensities for Shanghai were shown in fig. 4-5 and table 3-6 as examples.The urban heat island has a number of consequences. During the maximum deve-lopment of an urban heat island, the temperature field often induces a ’’ country breeze’’.There are more thunderstorm days, and heavy rainy days in Shanghai city comparedwith its nearby counties due to the rising current above the heat island. Except themean value of absolute humidity and relative humidity are lower, all the mean tempe-rature value of the coldest month, the hottest month and the annual are higher in urbandistricts compared to the rural areas in average, (table 7-8).更多还原