Hu Ting, Zhou Jiangxing, Dai Kan. Application of USCRN station density strategy to China climate reference network. J Appl Meteor Sci, 2012, 23(1): 40-46.
Citation: Hu Ting, Zhou Jiangxing, Dai Kan. Application of USCRN station density strategy to China climate reference network. J Appl Meteor Sci, 2012, 23(1): 40-46.

Application of USCRN Station Density Strategy to China Climate Reference Network

  • Received Date: 2011-06-03
  • Rev Recd Date: 2011-11-08
  • Publish Date: 2012-02-29
  • The US Climate Reference Network (USCRN) consists of 114 stations developed, deployed, managed, and maintained by the National Oceanic and Atmospheric Administration (NOAA) in the continental United States for the express purpose of detecting the national signal of climate change, focusing solely on precipitation and temperature. The vision of the USCRN program is to reduce uncertainty and error range envelopes in producing the most precise in situ precipitation and temperature records possible, and to do it with the fewest possible stations located in areas of minimal human disturbance and with the least likelihood of human development over the coming 50—100 years. And the key goal of USCRN is to reduce climate uncertainty at the national level to a statistically insignificant level. That is, for precipitation climate uncertainty should be reduced by 95% and for temperature climate uncertainty at the national level should be reduced by 98%.China is in great need of a sustainable high-quality and long-term climate observation network, especially for areas without observations or with little information. Given the complexity of the network development, the overall structure of the climate network should be analyzed first. Therefore, the minimum number of sites and locations which are able to represent national climate characteristics of China are proposed, on the basis of the equilateral triangular mesh employed by the USCRN, in order to provide preliminary advice for adjustment and optimization of China Climate Reference Network. For the purpose of assessing the performance of the network in addressing this goal, the coefficient of determination (r2) is used as the performance measure (PM). This PM is an assessment of how closely the current and past configuration of the network captures the true national temperature and precipitation signal as defined by an area-averaged time series of annual temperature and precipitation derived from 2416 China observing stations scattered across the continental China. The result is an explained variance that measures how closely the network's time series follows the true time series.Employing the USCRN standard that coefficient of determination exceeds 98% for precipitation and exceeds 95% for temperature, the 2416 stations in the conterminous China are investigated over the period of 1966—1995. Results indicate that China Climate Observing System should consist of at least 103 quasi-uniformly distributed stations on a 3.0° equilateral triangular grid in order to reproduce inter-annual variability in temperature and precipitation all over China. And on this structure, the new network will be established after surveys, approval or disapproval assessment, test and evaluation periods for each site at each geographic location. On the other hand, China Climate Reference Network may be adjusted and improved on the basis of the existing observing systems. The optimized network consists of 229 quasi-uniformly distributed stations on a 2.0° triangular grid, founded by the existing 199 stations and 30 new-established stations. The expected new-established stations are mainly located in the southwestern part of the Qinghai-Tibet Plateau, where will be the key areas in the network establishment. Based on the actual history of USCRN establishment, the final climate observing network of China may be formed by less than 103 or 229 stations.
  • Fig. 1  Comparison of annual precipitation (a) and temperature (b) from all 2416 stations in China to those from China Climate Reference Network with 143 stations

    Fig. 2  Layout of China Climate Reference Network with 143 stations

    Fig. 3  Layout of new-established China Climate Reference Network

    Fig. 4  Layout of complement China Climate Reference Network

    Fig. 5  Explained variances vs number of stations for different precipitation series

    Table  1  USCRN annual reduction in climate uncertainty

    截止时间 USCRN
    站点数
    降水量
    解释方差
    气温
    解释方差
    2000年[13] 2
    2001年[13] 8
    2002年9月[13] 23 74% 74%
    2003年10月[13] 40 大约80% 大约80%
    2004年10月[14] 58 90.20% 96.7%
    2005年10月[15] 72 91.1% 96.9%
    2006年10月[16] 77 91.8% 97.0%
    2007年10月[17] 96 94.0% 97.7%
    2008年10月[18] 114 95.1% 98.3%
    2009年10月[19] 114 95.1% 98.3%
    2010年10月[20] 114 95.1% 98.3%
     注:数据来自USCRN 2003—2010年财年报告[13-20]
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    Table  2  Explained variances of precipitation and temperature in different equilateral triangular grids

    格距 站点数目 降水量解释方差/% 气温解释方差/%
    三角网格点数 有数据的三角格点数 年平均 1月 7月 年平均 1月 7月
    5.0° 41 41 72.4 72.7 73.9 98.8 99.6 94.3
    4.5° 47 46 79.6 80.3 83.8 98.9 99.4 97.8
    4.0° 59 55 77.5 87.7 82.3 98.9 99.3 98.4
    3.5° 73 70 85.3 86.3 91.1 98.5 99.4 98.6
    3.0° 103 95 95.2 86.6 94.4 99.2 99.7 99.1
    2.5° 146 134 96.1 89.4 95.6 99.5 99.9 99.3
    2.0° 229 199 96.4 95.0 96.0 99.8 99.8 99.8
    1.5° 404 326 99.7 99.4 98.8 99.9 99.9 99.9
    1.0° 921 634 99.8 99.2 99.2 99.9 99.9 99.9
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    • Received : 2011-06-03
    • Accepted : 2011-11-08
    • Published : 2012-02-29

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