首页> 外文期刊>Urban Forestry & Urban Greening >Seasonal variations in the cooling effect of urban green areas on surrounding urban areas.
【24h】

Seasonal variations in the cooling effect of urban green areas on surrounding urban areas.

机译:城市绿地对周围市区的降温效果的季节性变化。

获取原文
获取原文并翻译 | 示例
           

摘要

We measured air temperature in an urban green area that includes forest and grassland and in the surrounding urban area for a full year in Nagoya, central Japan, to elucidate seasonal variations of the difference in air temperature between urban and green areas. We determined the range of the "cool-island" effect as well as the relationship between vegetation cover and air temperature throughout the year. The temperature difference between urban and green areas was large in summer and small in winter. The maximum air temperature difference was 1.9 degrees C in July 2007, and the minimum was -0.3 degrees C in March 2004. The difference was larger during the day than during the night in summer, whereas in winter the opposite relationship was true. However, winter diurnal variation was not particularly noticeable, a behaviour thought to be related to reduced shading by deciduous trees in the green area. During the night, the cooling effect of the green area reached 200-300 m into the urban area. During the day, the cooling effect between August and October 2006 exceeded 300 m and varied widely, although there was no correlation beyond 500 m. The correlation between air temperature and forest-cover ratio within a radius of 200 m from each measurement site was significant from 16:00 to 19:00. There was also a correlation during the night; this correlation was weakest in the early morning. The effect of the forest-cover ratio on air temperature was most pronounced in August 2006 and June 2007.
机译:在日本中部名古屋,我们测量了包括森林和草地在内的城市绿地以及周围城市地区全年的气温,以阐明城市和绿地之间气温差异的季节性变化。我们确定了“冷岛”效应的范围以及全年植被覆盖与气温之间的关系。夏季城市和绿地之间的温差较大,冬季则较小。 2007年7月的最高气温差为1.9摄氏度,2004年3月的最低气温为-0.3摄氏度。白天的气温差异大于夏季的夜晚,而冬季则相反。但是,冬季的昼夜变化并不是特别明显,这种行为被认为与绿地中落叶乔木的阴影减少有关。夜间,绿化区域的降温效果达到了市区200-300 m。白天,2006年8月至2006年10月的降温效果超过300 m,并且变化很大,尽管500 m以上没有相关性。从每个测量点开始,在200 m半径范围内,空气温度与森林覆盖率之间的相关性在16:00至19:00之间很明显。夜间也有相关性。这种相关性在清晨最弱。 2006年8月和2007年6月,森林覆盖率对气温的影响最为明显。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号