761 to 770 of 926 Results
Tabular Data - 1.6 KB - 13 Variables, 19 Observations - UNF:6:pUYwyUIpsRWmCnpBju2KxQ==
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Feb 29, 2024 - UMR GET
Girard, Félix; Grippa, Manuela; Kergoat, Laurent; Nikiema, Hedwige; Wubda, Maxime; Yonaba, Roland; Fowé, Tazen; Abdourhamane Touré, Amadou; Mainassara, Ibrahim; De Fleury, Mathilde, 2024, "Shallow lakes in West Africa: height-area relationships derived from remote sensing (2018-2023)", https://doi.org/10.23708/CRZE9K, DataSuds, V1, UNF:6:FKg53StFN6/u24Mc/S3XFw== [fileUNF]
In West Africa, lakes and reservoirs play a vital role as they are critical resources for drinking water, livestock, irrigation and fisheries. Given the scarcity of in situ data, satellite remote sensing is an important tool for monitoring lake volume changes in this region. Seve... |
Feb 29, 2024 -
Shallow lakes in West Africa: height-area relationships derived from remote sensing (2018-2023)
Plain Text - 1.9 KB -
MD5: 2f918b3451c1af6032895fb3f43cd520
Dataset description |
Feb 29, 2024 -
Shallow lakes in West Africa: height-area relationships derived from remote sensing (2018-2023)
Tabular Data - 382.5 KB - 7 Variables, 3759 Observations - UNF:6:FKg53StFN6/u24Mc/S3XFw==
Remote sensing-derived height-area-volume relationships (CSV format) |
Feb 16, 2024 - DiDEM project
Hervé, Dominique; Randrianatoandro, Ravakiniaina; Delaitre, Eric; Robison, Laurent; Razanaka, Samuel; Ratiarson, Venot, 2024, "Identification, localization and numbering of islets and geomorphological units of the Betsiboka delta (northwestern Madagascar) on Sentinel 2 satellite images (2020, 2021)", https://doi.org/10.23708/COLVLV, DataSuds, V1
Long time series (more than a century) are difficult to construct but they are useful for understanding hydro-geomorphological phenomena that take place over the long term and anticipating future risks. The Betsiboka River into which the Ikopa flows from Antananarivo, capital of... |
Plain Text - 3.4 KB -
MD5: 9a7d68f27f682bf455db7d40d882d817
Dataset description |
Adobe PDF - 113.2 KB -
MD5: 02aff060eb26f7f5d00b10a2ab403395
Co-author contribution details. |
Adobe PDF - 334.6 KB -
MD5: d3fbb51a793a835071ea7029f837706e
Detail of the downstream limit of the Betsiboka delta, between Boanamary in the right bank and a river in the left bank. |
Adobe PDF - 518.1 KB -
MD5: da1207c2d5b47c908f6df6b64467b70e
Large limits of the delta are defined by the extension of mangrove soils in green (ORSTOM, 1952) and the maximum extension of flooded area in red (flooded area in 2015-2016 by Catry et al., 2017). |
JPEG Image - 1.9 MB -
MD5: db9dca815b111a010f1be6b12641f547
The definitive limits of the delta are defined by the downstream long limit (Boanamary), the upstream first right channel, and the large limits defined according to mangrove and flooded area. |
