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Chinese Science Bulletin, Volume 61, Issue 24: 2659-2662(2016) https://doi.org/10.1360/zk2016-61-24-2659

对话张人禾: 2016年上半年中国南方强降水与超强厄尔尼诺

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Abstract

There is no abstract available for this article.


Funded by

中国科学院科技服务网络计划(STS计划(KFJ-EW-STS-074)

中国科学院战略先导专项(B类(XDB03030100)

国家自然科学基金重大项目(41190081)

“第三极环境(TPE”国际计划)


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  • Figure 1

    Monthly rainfall anomalies averaged in (a) 2015/2016 winter (December 2015–February 2016), (b) 2016 spring (March–May) and (c) monthly rainfall anomalies in June of 2016 over eastern China (mm) based on the monthly rainfall data observed from 160 stations in China. The climatology is taken to be the average in 1981–2010

  • Figure 2

    Sea surface temperature anomalies in eastern equatorial Pacific Nino3 region (90°–150°W, 5°S–5°N) (red line), tropical Indian Ocean (20°S–20°N, 55°–100°E) (blue line) and tropical northern Atlantic Ocean (0°–20°N, 30°–80°W) (black line) (°C). The data used is the OISST from NOAA, and the climatology is taken to be the average in 1982–2010

  • Figure 3

    Anomalous outgoing longwave radiation (OLR) (shadings, W/m2) and 850 hPa winds (vectors, m/s) in (a) 2015/2016 winter (December 2015–February 2016), (b) 2016 spring (March–May) and (c) June of 2016. The winds and OLR data are from NCEP/NCAR reanalysis and NOAA, respectively, and the climatology is taken to be the average in 1981–2010

  • 张人禾

    中国科学院院士

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