Influence of the envelope curve on the estimate of probable maximum precipitation (PMP) in the coastal region of Algeria

被引:1
作者
Batout, Soumia [1 ,2 ]
Houichi, Larbi [3 ]
Marouf, Nadir [1 ,2 ]
机构
[1] Univ Larbi Ben Mhidi, Dept Hydraul, Fac Sci & Appl Sci, POB 358, Oum El Bouaghi 04000, Algeria
[2] Univ Larbi Ben Mhidi, Lab Ecol & Environm, Oum El Bouaghi, Algeria
[3] Batna Univ, Dept Hydraul, Fac Technol, Batna, Algeria
关键词
Probable maximum precipitation; Hershfield method; Frequency factor; Envelope curve; Algerian coastal basins; DURATION;
D O I
10.1007/s40808-021-01209-1
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Probable maximum precipitation (PMP) is considered as a principal factor for estimating probable maximum floods (PMF) when designing various hydraulic structures. The estimation of PMP by the Hershfield statistical method was adopted in this paper for 112 rainfall stations in the three Algerian coastal basins (coastal region). This method is based on the adequate estimation of the frequency factor (K-m) using some envelope curves. Several researchers have used different types of envelope curves in their works such as the linear, exponential, and polynomial type. In this work, a new linear envelope curve was introduced and adopted. This paper will perform a comparison between linear, exponential, second degree polynomial, composite and proposed linear envelope curves. On the basis of the coefficient of determination (R-2) the proposed linear envelope curve was chosen to obtain reliable PMP values, thus avoiding underestimation and overestimation. The obtained PMP values vary from a minimum of 152.21 mm (station 109, BV04) to a maximum of 436.15 mm (station 47, BV02) with a mean value of 253. 32 mm. To comprehend the PMP spatial distribution in Algerian coastal region, the Inverse Distance Weighting (IDW) method was used with ArcGIS 10.5 software from the Environmental Systems Research Institute (ESRI).
引用
收藏
页码:2083 / 2093
页数:11
相关论文
共 33 条
  • [1] Review of studies on hydrological modelling in Malaysia
    Abdulkareem J.H.
    Pradhan B.
    Sulaiman W.N.A.
    Jamil N.R.
    [J]. Modeling Earth Systems and Environment, 2018, 4 (4) : 1577 - 1605
  • [2] Probable maximum precipitation estimation in a humid climate
    Afzali-Gorouh, Zahra
    Bakhtiari, Bahram
    Qaderi, Kourosh
    [J]. NATURAL HAZARDS AND EARTH SYSTEM SCIENCES, 2018, 18 (11) : 3109 - 3119
  • [3] Al Mamun A, 2010, INT J ARTS SCI, V3, P383
  • [4] Alias N. E., 2013, ANN DISAS PREV RES I, V56B, P65
  • [5] Alias N. E., 2013, J JPN SOC CIV ENG B1, V69, pI_157, DOI 10.2208/jscejhe.69.I_157
  • [6] Estimating probable maximum precipitation for Bangladesh
    Bari, Sheikh Hefzul
    [J]. INTERNATIONAL JOURNAL OF HYDROLOGY SCIENCE AND TECHNOLOGY, 2021, 11 (04) : 415 - 421
  • [7] Stochastic Modeling of Extreme Precipitation: a Regional Approach
    Bolgov, M. V.
    Filippova, I. A.
    Trubetskova, M. D.
    Osipova, N. V.
    [J]. WATER RESOURCES, 2019, 46 (SUPPL 2) : S1 - S7
  • [8] Predetermination of flood flows by different methods: Case of the catchment area of the Biskra Oued (North-East Algeria)
    Boumessenegh, Amel
    Dridi, Hadda
    [J]. MODELING EARTH SYSTEMS AND ENVIRONMENT, 2022, 8 (01) : 1321 - 1333
  • [9] Estimation of the probable maximum precipitation in Barcelona (Spain)
    Casas, M. Carmen
    Rodriguez, Rauel
    Prohom, Marc
    Gazquez, Antonio
    Redano, Angel
    [J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2011, 31 (09) : 1322 - 1327
  • [10] Spatio-temporal precipitation variability over Western Ghats and Coastal region of Karnataka, envisaged using high resolution observed gridded data
    Doranalu Chandrashekar V.
    Shetty A.
    Singh B.B.
    Sharma S.
    [J]. Modeling Earth Systems and Environment, 2017, 3 (4) : 1611 - 1625