@article{fdi:010078041,
  title = {{Q}uantifying the uncertainty of a coupled plume and tephra dispersal model : {PLUME}-{MOM}/{HYSPLIT} simulations applied to {A}ndean volcanoes},
  author = {{T}adini, {A}. and {R}oche, {O}livier and {S}amaniego, {P}ablo and {G}uillin, {A}. and {A}zzaoui, {N}. and {G}ouhier, {M}. and {V}itture, {M}. {D}. and {P}ardini, {F}. and {E}ychenne, {J}. and {B}ernard, {B}. and {H}idalgo, {S}. and {L}e {P}erinec, {J}. {L}.},
  editor = {},
  language = {{ENG}},
  abstract = {{N}umerical modeling of tephra dispersal and deposition is essential for evaluation of volcanic hazards. {M}any models consider reasonable physical approximations in order to reduce computational times, but this may introduce a certain degree of uncertainty in the simulation outputs. {T}he important step of uncertainty quantification is dealt in this paper with respect to a coupled version of a plume model ({PLUME}-{M}o{M}) and a tephra dispersal model ({HYSPLIT}). {T}he performances of this model are evaluated through simulations of four past eruptions of different magnitudes and styles from three {A}ndean volcanoes, and the uncertainty is quantified by evaluating the differences between modeled and observed data of plume height (at different time steps above the vent) as well as mass loading and grain size at given stratigraphic sections. {D}ifferent meteorological data sets were also tested and had a sensible influence on the model outputs. {O}ther results highlight that the model tends to underestimate plume heights while overestimating mass loading values, especially for higher-magnitude eruptions. {M}oreover, the advective part of {HYSPLIT} seems to work more efficiently than the diffusive part. {F}inally, though the coupled {PLUME}-{M}o{M}/{IIYSPLIT} model generally is less efficient in reproducing deposit grain sizes, we propose that it may he used for hazard map production for higher-magnitude eruptions (sub-{P}linian or {P}linian) for what concern mass loading.},
  keywords = {{EQUATEUR} ; {CHILI} ; {ANDES} ; {TUNGURAHUA} {VOLCAN} ; {COTOPAXI} {VOLCAN} ; {PUYEHUE} {VOLCAN} ; {CORDON} {CAULLE} {VOLCAN}},
  booktitle = {},
  journal = {{J}ournal of {G}eophysical {R}esearch : {S}olid {E}arth},
  volume = {125},
  numero = {2},
  pages = {e2019{JB}018390 [20 ]},
  ISSN = {2169-9313},
  year = {2020},
  DOI = {10.1029/2019jb018390},
  URL = {https://www.documentation.ird.fr/hor/fdi:010078041},
}