1) winter temperature anomalies
冬季温度异常
1.
By using the data set of the mean monthly global sea surface temperature during the period of 1951~ 1997, mean monthly global wind fields, the surface air temperature of 100 stations in eastern China during the same period, the spatial and temporal features and its variations for winter temperature anomalies in eastern China are analyzed.
利用1951～1997年全球海温、风场月平均资料和我国东部地区100个测站的冬季地面气温等资料,分析了我国东部地区冬季温度异常的时空特征和变化规律,探讨了全球海温异常与我国东部地区冬季温度异常的关系。
3) winter(summer) air temperature anomaly
冬季(夏季)气温异常
5) 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。
补充资料：铂电阻温度表(见电阻温度表)
铂电阻温度表(见电阻温度表)
表。bod旧nZu wendubiao铂电阻温度表见电阻温
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