Skip to main content
Log in

Assessment of drought vulnerability based on the soil moisture PDF

  • Original Paper
  • Published:
Stochastic Environmental Research and Risk Assessment Aims and scope Submit manuscript

Abstract

This paper studies the statistics of the soil moisture condition and its monthly variation for the purpose of evaluating drought vulnerability. A zero-dimensional soil moisture dynamics model with the rainfall forcing by the rectangular pulses Poisson process model are used to simulate the soil moisture time series for three sites in Korea: Seoul, Daegu, and Jeonju. These sites are located in the central, south-eastern, and south-western parts of the Korean Peninsular, respectively. The model parameters are estimated on a monthly basis using hourly rainfall data and monthly potential evaporation rates obtained by the Penmann method. The resulting soil moisture simulations are summarized on a monthly basis. In brief, the conclusions of our study are as follows. (1) Strong seasonality is observed in the simulations of soil moisture. The soil moisture mean is less than 0.5 during the dry spring season (March, April, and June), but other months exceed the 0.5 value. (2) The spring season is characterized by a low mean value, a high standard deviation and a positive skewness of the soil moisture content. On the other hand, the wet season is characterized by a high mean value, low standard deviation, and negative skewness of the soil moisture content. Thus, in the spring season, much drier soil moisture conditions are apparent due to the higher variability and positive skewness of the soil moisture probability density function (PDF), which also indicates more vulnerability to severe drought occurrence. (3) Seoul, Daegue, and Jeonju show very similar overall trends of soil moisture variation; however, Daegue shows the least soil moisture contents all through the year, which implies that the south-eastern part of the Korean Peninsula is most vulnerable to drought. On the other hand, the central part and the south-western part of the Korean peninsula are found to be less vulnerable to the risk of drought. The conclusions of the study are in agreement with the climatology of the Korean Peninsula.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7

Similar content being viewed by others

References

  • Bell KR, Blanchard BJ, Schmugge TJ, Witczak MW (1980) Analysis of surface moisture variations within large field sites. Water Resour Res 16(4):796–810

    Google Scholar 

  • Byun HR (1996) On the atmospheric circulation caused drought in Korea. J Korea Meteorol Soc 32(3):455–469

    Google Scholar 

  • Castelli F, Rodriguez-Iturbe I (1996) On the dynamical coupling of large scale spatial patterns of rainfall and soil moisture. Tellus 48(A):290–311

    Google Scholar 

  • Cordova JR, Rodriguez-Iturbe I (1985) On the probabilistic structure of storm surface runoff. Water Resour Res 21(5):755–763

    Google Scholar 

  • Entekhabi D, Rodriguez-Iturbe I (1994) Analytical framework for the characterization of the space-time variability of soil moisture. Adv Water Resour 17:35–45

    Article  Google Scholar 

  • Entekhabi D, Rodriguez-Iturbe I, Castelli F (1996) Mutual iinteraction of soil moisture state and atmospheric processes. J Hydrol 184:3–17

    Article  CAS  Google Scholar 

  • Han YH, Byun HR (1994) On the existence of seasonal drought in the Korean Peninsula. J Korea Meteorol Soc 30(3):457–467

    Google Scholar 

  • Jackson TJ, Le Vine DE (1996) Mapping surface soil moisture using an aircraft-based passive microwave instrument: algorithm and example. J Hydrol 184:85–99

    Article  CAS  Google Scholar 

  • Korea Water Resources Coporation (KOWACO) (2002) Study on comprehensive drought management. Daejeon, pp 554

  • Kustas WP, Goodrich DD (1994) Preface. Water Resour Res 30(5):1211–1225

    Article  Google Scholar 

  • Njoku E, Entekhabi D (1996) Passive microwave remote sensing of soil moisture. J Hydrol 184:101–129

    Article  CAS  Google Scholar 

  • North GR, Nakamoto S (1989) Formalism for comparing rain estimation designs. J Atmos Ocean Tech 6:985–992

    Article  Google Scholar 

  • Rhee DY (1998) Relationship between El Nino/Southern oscillation and Korean drought. J Korean Assoc Civil Eng 18(2):67–70

    Google Scholar 

  • Rodriguez-Iturbe I (1986) Scale of fluctuation of rainfall models. Water Resour Res 22(9):15S–37S

    Google Scholar 

  • Rodriguez-Iturbe I, Gupta VK, Waymire E (1984) Scale considerations in the modeling of temporal rainfall. Water Resour Res 20(11):1611–1619

    Google Scholar 

  • Yoo C (2001) Sampling of soil moisture fields and related errors: implications to the optimal sampling design. Adv Water Resour 24(5):521–530

    Article  Google Scholar 

  • Yoo C, Valdes JB, North GR (1998) Evaluation of the impact of rainfall on soil moisture variability. Adv Water Resour 21(5):375–384

    Article  Google Scholar 

  • Yoo C, Kim Seong J, Lee J-S (2001) Land cover change and its impact on soil-moisture-field evolution. J Hydrol Eng ASCE 6(5):436–441

    Article  Google Scholar 

  • Yoo C, Kim S-J, Valdes JB(2005) Sensitivity of soil moisture field evolution on rainfall forcing. Hydrol Processes 19:1855–1869

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Chulsang Yoo.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Yoo, C., Kim, S. & Kim, TW. Assessment of drought vulnerability based on the soil moisture PDF. Stoch Environ Res Ris Assess 21, 131–141 (2006). https://doi.org/10.1007/s00477-006-0050-9

Download citation

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00477-006-0050-9

Keywords

Navigation