| 热带和中纬太平洋海温异常对东北夏季低温冷害影响的诊断分析研究 |
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| 引用本文： | 郑维忠,倪允琪.热带和中纬太平洋海温异常对东北夏季低温冷害影响的诊断分析研究[J].应用气象学报,1999,10(4):394-401. |
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| 作者姓名： | 郑维忠 倪允琪 |
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| 作者单位： | 1.南京大学大气科学系!南京210093(郑维忠)，中国气象科学研究院!北京100081(倪允琪) |
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| 摘 要： | 利用1995~1997年东北地区23个测站的地面气温资料、1950~1996年太平洋地区月平均海温资料以及1980~1994年全球月平均风场资料，分析了东北夏季低温冷害的时空特征和变化规律，探讨了太平洋各区域的海温异常与低温冷害之间的可能联系及其影响机理。结果表明，用EOF分解得到的前三个特征向量（占总方差的84.28%）基本表示了东北夏季气温的变化，用这三个特征向量重建的气温距平场，存在着3~4年、6~8年和准16年的主周期，其中6~8年的主分量信号最强。在年代际尺度上，在1979年前后发生了由气温偏冷向偏暖的突变。热带西太平洋暖池（140°E~180°，10°S~10°N）是影响东北夏季气温的关键海域，那里前期冬季海表温度变化是预测东北夏季低温冷害的强信号。另一个关键海域是中纬西太平洋（130°E~180°，10~30°N），前期春季的海温变化也与东北夏季低温有较密切的联系。
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| 关 键 词： | 海温异常 东北夏季低温 诊断分析 影响机理 |
Diagnostic Study on Impact of Sea Surface Temperature Anomalies over Tropical and Mid-latitude Pacific on Summer Low Temperature Cool Damage in Northeast China |
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| Zheng Weizhong.Diagnostic Study on Impact of Sea Surface Temperature Anomalies over Tropical and Mid-latitude Pacific on Summer Low Temperature Cool Damage in Northeast China[J].Quarterly Journal of Applied Meteorology,1999,10(4):394-401. |
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| Authors: | Zheng Weizhong |
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| Affiliation: | 1.1) (Department of Atmospheric Science, Nanjing University, Nanjing 210093); 2) (Chinese Academy of Meteorological Sciences, Beijing 100081) |
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| Abstract: | By using the data set of the surface air temperature of 23 stations in Northeast China during the period of 1951—1997, mean monthly sea surface temperature (SST) in Pacific from 1950 to 1996 and global mean monthly wind fields from 1980 to 1994, the spatial and temporal features and its variations for summer low temperature cool damage in Northeast China are analyzed. The possible relationship and the mechanism of impact between SST anomalies in the regions of Pacific and the low temperature cool damage are also studied. The results show that the first three eigenvalues obtained by the EOF analysis (84.28% of the total variance) can basically explain the summer temperature anomalies in Northeast China. The temperature anomalies reconstructed by those three eigenvalues have three dominant scales on 3—4 years, 6—8 years and quasi-16 years. Among them, 6—8 years’ oscillation is the strongest. On inter-decadescale, three appears a jump of the temperature from cooler to warmer around 1997. The warm pool of tropical West Pacific (140° E—180°, 10° S—10° N) is a key area that affects the summer low temperature in Northeast China. The SST anomalies in last winter over that is a strong signal which could be used to predict the summer low temperature cool damage. Another key area is mid-latitude West Pacific (130° E—180°, 10°—30° N) where the SST anomalies in last spring are also closely related with summer low temperature in Northeast China. |
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| Keywords: | SST anomaly Northeast China Summer low temperature Diagnostic analysis Mechanism of impact |
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