摘要
通过对某超高层玻璃幕墙建筑外表面的微气候参数的监测,发现高度是影响各参数垂直变化的主因。随着高度的增加,温度和湿度的变化均呈多"S"型变化,且为互补,顶层的温度较高而湿度最低;11∶00时建筑外表面垂直温差最大为6.7℃,而16∶00时垂直温差最小为0℃,测量时间段内平均垂直温差为2.7℃。随着高度的增加,建筑外表面的贴附气流速度逐渐增加,直至顶层有所回落,在建筑高度85%左右的平均风速最大,约为地面风速的7倍。温湿度和风速之间存在相互影响,较大的风速可以强化热湿交换,利于湿热地区夏季的通风降温和除湿。
It's observed that the height is a major reason for vertical variation of microclimateparameters by continuous monitoring of the super high-rise glass curtain wall building: With the increase ofheight, the changes of both temperature and humidity present multi-S type and they are complementary. Theroof has a higher temperature but lower humidity. The maximum, minimum and average vertical temperaturedifferences are 6.7 ℃(obtained at 11:00), 0 ℃(Obtained at 16:00) and 2.7℃ respectively. The vertical windvelocity outside the building increases always and decreases at the roof. The maximum wind speed appearsin the 85% height of building, which is approximately seven times of suface wincl speed. Temperature,humidity and speed velocity humive interactions. A higher wind velocity will enhance the heat and moistureexch(mge, which favors condensation and dehumidification by ventilation for hot and humid areas.
出处
《建筑节能》
CAS
2016年第6期49-52,72,共5页
BUILDING ENERGY EFFICIENCY
基金
宁波市建设科技项目(甬建发2015-34号)
国家自然科学基金(51506102)
浙江省自然科学基金项目(LY15E080016)
关键词
超高层建筑
微气候
温湿度
风速
热湿交换
super high-rise building
microclimate
temperature and humidity
wind velocity
heat and moisture exchange