مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Verion

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

video

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

sound

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Version

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

View:

3,152
Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Download:

0
Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Cites:

4

Information Journal Paper

Title

FLOOD HAZARD ZONATION USING AND HYDRAULIC MODELS

Author(s)

VAHABI J. | Issue Writer Certificate 

Pages

  33-40

Abstract

 Flood studies to plan for optimal utilization and to control this natural phenomenon is main concern in the world and our country. Great damages caused by floods in different parts of the country during past few years demand comprehensive plans; knowing that it is impossible to Plan and apply flood control methods without a good knowledge about the behavior of this phenomenon. The extend of flood damages in various conditions depends on the amount of inflow and the geometrical characteristics of flow bed and adjacent areas. Thus FLOOD HAZARD ZONATION for different return Periods 'is necessary to predict the extend of damages caused by floods in different conditions and to justify socio-economical aspects of flood control programs. To Plan optimal land use in river margins and flood plains, the prohibitive, restrictive and it is impossible to zone flood hazard plain without a good knowledge of flood intensity and torrential flow behavior along the river route and flood plain. As a result, regarding more adaptation between estimated hydrographs by SCS method and observed hydrographs, this method was selected to estimate flood hydrographs, in related sub basins for given return periods. After this stage by estimating the outlet flood hydrograph in the headwaters and existing sub basins along given route for determining flood hazard plain by SCS method of HEC-1 Model, maximum water levels in 28 distinct cross sections were determined by MIKE11 model along about 14 kilometers of the river route. In the end, by using digital elevation model (DEM) produced from river bed and boundaries and the maximum water level in given cross sections for return periods of 5, 10, 25 and 100 years the flood hazard plain was determined by ILWIS Software Capability.

Cites

References

  • No record.
  • Cite

    APA: Copy

    VAHABI, J.. (2006). FLOOD HAZARD ZONATION USING AND HYDRAULIC MODELS. PAJOUHESH-VA-SAZANDEGI, 19(2 (71 IN NATURAL RESOURCES)), 33-40. SID. https://sid.ir/paper/20048/en

    Vancouver: Copy

    VAHABI J.. FLOOD HAZARD ZONATION USING AND HYDRAULIC MODELS. PAJOUHESH-VA-SAZANDEGI[Internet]. 2006;19(2 (71 IN NATURAL RESOURCES)):33-40. Available from: https://sid.ir/paper/20048/en

    IEEE: Copy

    J. VAHABI, “FLOOD HAZARD ZONATION USING AND HYDRAULIC MODELS,” PAJOUHESH-VA-SAZANDEGI, vol. 19, no. 2 (71 IN NATURAL RESOURCES), pp. 33–40, 2006, [Online]. Available: https://sid.ir/paper/20048/en

    Related Journal Papers

    Related Seminar Papers

  • No record.
  • Related Plans

  • No record.
  • Recommended Workshops






    Move to top