% IMPORTANT: The following is UTF-8 encoded.  This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.

@ARTICLE{KhoshBinGhomash:910791,
      author       = {Khosh Bin Ghomash, Shahin and Bachmann, Daniel and
                      Caviedes-Voullième, Daniel and Hinz, Christoph},
      title        = {{I}mpact of {R}ainfall {M}ovement on {F}lash {F}lood
                      {R}esponse: {A} {S}ynthetic {S}tudy of a {S}emi-{A}rid
                      {M}ountainous {C}atchment},
      journal      = {Water},
      volume       = {14},
      number       = {12},
      issn         = {2073-4441},
      address      = {Basel},
      publisher    = {MDPI},
      reportid     = {FZJ-2022-04143},
      pages        = {1844 -},
      year         = {2022},
      abstract     = {Rainfall is a spatiotemporally varied process and key to
                      accurately capturing catchment runoff and determining flood
                      response. Flash flood response of a catchment can be
                      strongly governed by a rainfall’s spatiotemporal
                      variability and is influenced by storm movement which drives
                      a continuous spatiotemporal change throughout a rainfall
                      event. In this work, the sensitivity of runoff and flooded
                      areas to rainfall movement are assessed in the Kan catchment
                      (Iran). The allochthonous nature of floods in the catchment
                      and how they interact with the effects of rainfall movement
                      are investigated. Fifty synthetic rain hyetographs are
                      generated and traversed over the catchment under different
                      velocities and directions and used to force a 1D/2D
                      hydrodynamic model. The results suggest rainfall movement
                      affects the runoff response in different degrees. Peak
                      discharge, hydrograph shapes and flooded areas are affected.
                      Storms with higher velocities result in higher peaks and
                      faster onsets of runoff and consequently higher flooded
                      areas in comparison to slower storms. The direction of the
                      movement also plays a role. Storms moving along the average
                      direction of the stream result in higher peaks and flooded
                      areas. The relevance of storm direction is greater for slow
                      moving storms. Additionally, the influence of rainfall
                      movement is modulated by hyetograph structure, and the
                      allochthonous behavior is greatly dependent on the location
                      within the drainage network at which it is assessed.},
      cin          = {IBG-3 / JSC},
      ddc          = {690},
      cid          = {I:(DE-Juel1)IBG-3-20101118 / I:(DE-Juel1)JSC-20090406},
      pnm          = {2173 - Agro-biogeosystems: controls, feedbacks and impact
                      (POF4-217)},
      pid          = {G:(DE-HGF)POF4-2173},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000815938500001},
      doi          = {10.3390/w14121844},
      url          = {https://juser.fz-juelich.de/record/910791},
}