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1)  winter ventilation design temperature
冬季通风室外计算温度
1.
In this paper,based on the original meteorological data,the winter ventilation design temperature in Code for Design of Heating Ventilation and Air Conditioning(GBJ 19-87) was firstly discussed.
本文以原始气象数据为基础,首先对《采暖通风与空气调节设计规范》(GBJ 19-87)室外空气计算参数中冬季通风室外计算温度的统计方法进行了讨论研究,对可能存在的3种不同方法进行了数据对比。
2)  outdoor design temperature
室外计算温度
1.
The article reviewed the history of outdoor design temperature for heating.
文章回顾了采暖室外计算温度的发展历史,比较了前苏联、美国、加大以及我国制定方法。
3)  Winter temperature
冬季温度
1.
Recently,many studies have described the relationship between winter temperature in China and some climate systems including the Siberian high(SH),the Arctic Oscillation(AO),ENSO and the western Pacific teleconnection pattern(WP).
综合分析了西伯利亚高压、北极涛动、ENSO和西太平洋遥相关型(WP)在年际和年代际时间尺度上对中国冬季温度的影响,结果表明在年际尺度上,WP和西伯利亚高压都对温度有显著影响,WP的影响主要存在于中国东部从东北南部至广东沿海一带大陆边缘区,而西伯利亚高压的影响范围则大得多,几乎涵盖了除黄河长江上游部分地区外的整个中国。
2.
warmer,normal and colder categories)is proposed based on the winter temperature data observed at 565 stations in China during 1956-2005,where the IWWI is defined as the ratio of the station number of warmer category over the total number of stations.
结果表明:暖冬指数与中国冬季温度的变暖趋势相一致,并表现出显著的年代际变化特征,其变率分别为10%/10a和0。
4)  outdoor computational temperature during heating period
采暖室外计算温度
1.
The value of outdoor computational temperature during heating period influences correctness of design load for heating,and that influences thermal comfort of heating system,energy consumption and building investment.
采暖室外计算温度的合理确定直接影响采暖设计热负荷的计算准确度,进而影响暖系统的热舒适性、能耗及投资情况。
5)  Indian winter monsoon
印度冬季风
1.
1 and the distributions of heat source calculated by NCEP/NCAR(version 1) reanalysis datasets,the impact of atmospheric cold(heat) source distribution over Asia and the Southern Hemisphere in January on East Asian winter monsoon and Indian winter monsoon are investigated.
1模式及NCEP/NCAR(version 1)再分析资料计算出来的几种现实大气热源分布情况,分别讨论亚洲各地区和南半球上空冬季1月份大气冷(热)源对东亚冬季风环流系统和印度冬季风环流系统形成的影响。
2.
The impact of atmospheric cold(heat) source distribution over Asia and the Southern Hemisphere in January on the East Asian winter monsoon and Indian winter monsoon is simulated with the NCAR CAM3.
1模式及NCEP/NCAR(version 1)再分析资料计算了几种现实大气热源分布情况,讨论了亚洲各地区和南半球上空冬季1月大气冷(热)源对东亚冬季风环流系统和印度冬季风环流系统形成的影响。
6)  Winter solar greenhouse
冬季日光温室
补充资料:冬季
一年的第四季,我国习惯指立冬到立春的三个月时间。也指农历‘十、十一、十二 ’三个月。参看〖四季 〗。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条