@article{fdi:010062713, title = {{W}ater level fluctuations in the {C}ongo basin derived from {ENVISAT} satellite altimetry}, author = {{B}ecker, {M}. and da {S}ilva, {J}. {S}. and {C}almant, {S}t{\'e}phane and {R}obinet, {V}. and {L}inguet, {L}. and {S}eyler, {F}r{\'e}d{\'e}rique}, editor = {}, language = {{ENG}}, abstract = {{I}n the {C}ongo {B}asin, the elevated vulnerability of food security and the water supply implies that sustainable development strategies must incorporate the effects of climate change on hydrological regimes. {H}owever, the lack of observational hydro-climatic data over the past decades strongly limits the number of studies investigating the effects of climate change in the {C}ongo {B}asin. {W}e present the largest altimetry-based dataset of water levels ever constituted over the entire {C}ongo {B}asin. {T}his dataset of water levels illuminates the hydrological regimes of various tributaries of the {C}ongo {R}iver. {A} total of 140 water level time series are extracted using {ENVISAT} altimetry over the period of 2003 to 2009. {T}o improve the understanding of the physical phenomena dominating the region, we perform a {K}-means cluster analysis of the altimeter-derived river level height variations to identify groups of hydrologically similar catchments. {T}his analysis reveals nine distinct hydrological regions. {T}he proposed regionalization scheme is validated and therefore considered reliable for estimating monthly water level variations in the {C}ongo {B}asin. {T}his result confirms the potential of satellite altimetry in monitoring spatio-temporal water level variations as a promising and unprecedented means for improved representation of the hydrologic characteristics in large ungauged river basins.}, keywords = {satellite altimetry ; {C}ongo {B}asin ; regional hydrology ; {K}-means ; {CONGO} {BASSIN}}, booktitle = {}, journal = {{R}emote {S}ensing}, volume = {6}, numero = {10}, pages = {9340--9358}, ISSN = {2072-4292}, year = {2014}, DOI = {10.3390/rs6109340}, URL = {https://www.documentation.ird.fr/hor/fdi:010062713}, }