@article{fdi:010086865,
  title = {{T}he distinct impacts of the two types of {ENSO} on rainfall variability over {S}outheast {A}sia},
  author = {{N}guyen-{T}hanh, {H}. and {N}go-{D}uc, {T}. and {H}errmann, {M}arine},
  editor = {},
  language = {{ENG}},
  abstract = {{T}his study investigates the impact of {E}l {N}ino {S}outhern {O}scillation ({ENSO}) and {ENSO} {M}odoki on rainfall variability over {S}outheast {A}sia ({SEA}) with a focus on its twenty sub-regions. {F}or the period 1979-2019, seven {E}l {N}ino ({EN}), six {L}a {N}ina ({LN}), five {E}l {N}ino {M}odoki ({EM}), and five {L}a {N}ina {M}odoki ({LM}) events were identified. {I}n the boreal summer ({JJA}) and winter ({DJF}) of {EN} events, rainfall reduction occurred over the {M}aritime {C}ontinent and the {P}hilippines except for {W}est {P}hilippines in {JJA} and {W}est {K}alimantan in {DJF}. {S}imilar patterns but with enhanced drier/wetter conditions were detected during {EM}. {D}uring {LN}, rainfall increased in most sub-regions except for {W}est {P}hilippines and parts of mainland {I}ndochina in {JJA}, and in {DJF} in some southern areas such as {S}outh {S}umatra, {W}est {K}alimantan, and {P}apua. {C}ompared to {LN}, {LM} generally exhibited less wet/drier conditions in {JJA} over most sub-regions and wetter conditions in {DJF} over a major part of the {M}aritime {C}ontinent. {T}he decrease (increase) in rainfall over {SEA} during {M}odoki events compared to the canonical {ENSO} events was explained by a reduced (enhanced) moisture transport into the region and a weakening (strengthening) of the ascending branch of the {W}alker circulation.},
  keywords = {{ENSO} ; {ENSO} {M}odoki ; {R}ainfall variability ; {S}outheast {A}sia ; {ASIE} {DU} {SUD} {EST}},
  booktitle = {},
  journal = {{C}limate {D}ynamics},
  volume = {[{E}arly access]},
  numero = {},
  pages = {[18 p.]},
  ISSN = {0930-7575},
  year = {2023},
  DOI = {10.1007/s00382-023-06673-2},
  URL = {https://www.documentation.ird.fr/hor/fdi:010086865},
}