@article{fdi:010091166,
  title = {{R}ecovery of time series of water volume in {L}ake {R}anco ({S}outh {C}hile) through satellite altimetry and its relationship with climatic phenomena},
  author = {{F}uentes-{A}guilera, {P}. and {R}odríguez-{L}ópez, {L}. and {B}ourrel, {L}uc and {F}rappart, {F}.},
  editor = {},
  language = {{ENG}},
  abstract = {{I}n the context of escalating climate change-induced impacts on water resources, robust monitoring tools are imperative. {S}atellite altimetry, benefiting from technical improvement such as the use of {SAR} and {I}n{SAR} techniques and tracking modes considering topography, is emerging as a crucial means of estimating lake levels, data that are fundamental to understanding climate dynamics. {T}his study delves into the use of satellite-altimetry-determined water levels to analyze changes in water storage and superficial area in {L}ake {R}anco, in south-central {C}hile, from 1995 to 2023. {T}he main objective is to provide valuable information for water-resource management and policy formulation. {L}everaging {A}l{T}i{S} software (v2.2.9-0-gf5938ab), radar-altimetry data from the missions {ERS}-2, {ENVISAT}, {SARAL}, and {S}entinel-3{A} were processed, generating a complete time series of water levels. {T}he lake-level data were complemented by the bathymetric data for the lake to obtain the variation in the area and volume in the period 1995-2023. {T}hese results were analyzed with respect to hydrometeorological data from the study area, such as precipitation, temperature, relative humidity, and potential evapotranspiration. {A}dditionally, the effects of {ENSO} ({ENSO} 3.4 index) and the {P}acific {D}ecadal {O}scillation index ({PDO}) were considered. {R}esults reveal a strong correlation between altimetry-derived lake levels and observed in situ data, with a mean square error of 0.04 m, a coefficient of determination of 0.99, an index of agreement of 0.99, and a {K}ling-{G}upta efficiency of 0.90. {T}he analysis of climatic variables showed that variations in lake level coincide with changes in precipitation within the study area and also showed the influence of variations in temperature and potential evapotranspiration. {A}dditionally, the effects of the {ENSO} phenomenon can be seen within the study area for its cold phase (i.e., {L}a {N}i & ntilde;a) in the 2010-2012 period and for its warm phase (i.e., {E}l {N}ino) in the 2015-2016 period, with a decrease and increase in precipitation, respectively. {T}hese effects were enhanced when the cold and warm phases of the {ENSO} and {PDO} phenomena occured. {T}he successful application of satellite altimetry demonstrated in this study underscores its critical role in advancing our understanding and management of water resources amidst changing climate scenarios.},
  keywords = {water level ; altimetry ; water volume ; hydroclimatology ; {ENSO} ; {PDO} ; lake ; {C}hile ; {CHILI}},
  booktitle = {},
  journal = {{W}ater},
  volume = {16},
  numero = {14},
  pages = {1997 [20 p.]},
  year = {2024},
  DOI = {10.3390/w16141997},
  URL = {https://www.documentation.ird.fr/hor/fdi:010091166},
}