Hou Wei, Yang Jie, Zhao Junhu. Staged meteorological drought index based on boltzmann function. J Appl Meteor Sci, 2013, 24(6): 695-703.
Citation: Hou Wei, Yang Jie, Zhao Junhu. Staged meteorological drought index based on boltzmann function. J Appl Meteor Sci, 2013, 24(6): 695-703.

Staged Meteorological Drought Index Based on Boltzmann Function

  • Received Date: 2012-12-11
  • Rev Recd Date: 2013-08-22
  • Publish Date: 2013-12-31
  • In the practical research and business, it's often needed to evaluate the overall meteorological drought degree of a site within a certain period of time. Based on the daily meteorological drought index, the accumulative probability distribution of the number of days for different drought and flood degrees at a time scale can be obtained, and through solving the accumulative probability distribution by Boltzmann function, the standardized staged meteorological drought intensity index (ISD) and staged meteorological drought discrepancy index (ISDD) is designed.ISD and ISDD of Kunming Station at the monthly scale are constructed as an example. Through comparing and analyzing the precipitation anomaly percentage, ISD, standardized precipitation index (ISP) and ISDD in the different periods, and combined with the day by day evolution of the rainfall and multi-scale standardized precipitation index (IMSP), the effectiveness of ISD and ISDD index are verified. A basic principle is that the rainfall at a certain moment could affect the drought and flood states after that moment, but has no impact on the drought and flood states before.ISD makes full use of daily meteorological drought index which contains prophase precipitation information to synthesize drought and flood characteristics of a certain period of time. The bigger ISD is, the more serious the drought is, and vice versa. The larger (smaller) ISDD means the drought or the flood is more concentrated (scattered). Moreover, these two indices can be calculated in different time scales for any site, and in the practical application, the other meteorological drought index also can be used by a forementioned method to build ISD and ISDD. A theoretical algorithm to get ISD and ISDD on any time scale is proposed, but the most applicable time scale should be 10 days, month and season, and on the inter-annual and inter-decadal scale, the proposed approach and other methods such as precipitation anomaly percentage and ISP can also be used.In view of the complexity of drought, no single index can fully express its intensity, harm and the potential impact, so the drought index is still being continuously explored and improved.
  • Fig. 1  The average probability distribution of the number of days for different drought and flood degrees in July 2009 and July 2008 at Kunming Station

    Fig. 2  The average accumulative probability distribution of the number of days for different drought and flood degrees in July 2009 and July 2008 at Kunming Station

    Fig. 3  The average accumulative probability distribution of the number of days for different drought and flood degrees in July from 1981 to 2010 at Kunming Station

    Fig. 4  The daily variation of precipitation in four periods at Kunming Station

    (a) from July to August in 2006, (b) from August to September in 2006, (c) from February to March in 2010, (d) from March to April in 2010

    Fig. 5  The daily variation of IMSP in four months at Kunming Station (a) August 2006, (b) September 2006, (c) March 2010, (d) April 2010

    Fig. 6  The probability distribution of the number of days for different drought and flood degrees at Kunming Station

    (a) August 2006, (b) September 2006, (c) March 2010, (d) April 2010

    Table  1  The contrast of precipitation anomaly percentage, ISD, ISDD and ISP in four periods at Kunming Station

    时间降水距平百分率/%ISDISDDISP
    2006-08-42.2-0.15-0.87-1.14
    2006-09-49.70.32-0.40-1.25
    2010-0338.40.67-0.480.78
    2010-0422.6-0.02-0.870.67
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    • Received : 2012-12-11
    • Accepted : 2013-08-22
    • Published : 2013-12-31

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