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1998年以来中国气温持续极端偏暖的事实
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科技导报 | 气象问题研究专题 2006,24(0604): 37-40
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科技导报 |气象问题研究专题 2006 , 24 (0604) : 37 -40
1998年以来中国气温持续极端偏暖的事实
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李庆祥1,3,李伟2,鞠晓慧 1
作者信息
    1. 国家气象信息中心 北京 2南京信息工程大学地理系 南京3. 中国气象局气候研究开放实验室 北京
通讯作者:
李庆祥
Analysis on the Persistent Extreme Warm Period over China since 1998
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    出版时间: 2006-04-10
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    利用国内地面气温观测资料,首先对数据进行了质量控制,考虑了序列的均一性和空间抽样误差问题,计算了近55年来(1951-2005)中国地面平均气温的变化幅度。结果显示,1998年为中国气温近55年之最暖年份,大约偏暖1.10℃(相对于1971-2000年间30年气候平均状况);自1998-2005年8年间,除2000年全国平均气温距平约在0.29℃外,其余7年相对于1971-2000年气候标准值均高出0.60℃以上,从最热年1998年开始依次排列为:1998年(1.10℃)、2002年(0.88℃)、1999年(0.86℃)、2004年(0.86℃)、2005年(0.72℃)、2003年(0.68℃)、2001年(0.63℃),这一事实值得引起人们深入关注。
    均一性  /  最暖年份  /  气候数据  /  气温
    Surface Air Temperature (SAT) data over China were used. Quality control process were applied to them, and the homogeneity of the series and the spatial sample errors were taken into consideration. The amplitude of China climate warming in recent 55 years was calculated. The results show: 1998 is the warmest year during the period, the SAT anomaly reached 1.10 ℃ (based on the climatology during 1971-2000, the same with the following text). In addition, the following 8 years saw 7 warmest years during 1951-2005, which are 2002(0.88℃),1999 (0.86℃),2004 (0.86℃),2005 (0.72℃),2003 (0.68℃),2001 (0.63℃), which deserves more attention.
    李庆祥;李伟;鞠晓慧. 1998年以来中国气温持续极端偏暖的事实. 科技导报, 2006 , 24 (0604) : 37 -40 .
    . Analysis on the Persistent Extreme Warm Period over China since 1998[J]. Science & Technology Review, 2006 , 24 (0604) : 37 -40 .

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    • 接收时间:2009-05-05
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    2种不同金属材料的力学参数

    Family
    属数
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    genus
    种数
    Number of
    species
    占总种数比例
    Percentage of
    total species (%)

    Genus
    种数
    Number of
    species
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    Percentage of total
    species (%)
    鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
    小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
    多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
    红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
    小菇属 Mycena 11 5.26
    光柄菇属 Pluteus 5 2.39
    红菇属 Russula 17 8.13
    栓菌属 Trametes 5 2.39
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