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2012 AGU Chapman Conference on Remote Sensing of the ...

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importance to global hydrology. The SWOT missi<strong>on</strong> willprovide data products <strong>of</strong> river discharge globally at anunprecedent spatial resoluti<strong>on</strong> (at least 100m), using twotypes <strong>of</strong> algorithms. One <strong>of</strong> <strong>the</strong>se algorithms is based <strong>on</strong> adata assimilati<strong>on</strong> framework, that ingests SWOTobservati<strong>on</strong>s into a hydrodynamic model and producesoptimal estimates <strong>of</strong> river discharge and o<strong>the</strong>r hydrualicvariables. In this study, results from a fraternal twinsyn<strong>the</strong>tic experiment are presented where “true” WSEs aresimulated over <strong>the</strong> Ohio River basin, and are <strong>the</strong>n fed into<strong>the</strong> SWOT Instrument Simulator to produce syn<strong>the</strong>ticsatellite observati<strong>on</strong>s over <strong>the</strong> same study area with <strong>the</strong>correct orbital and error characteristics. A “first-guess”simulati<strong>on</strong> that emulates <strong>the</strong> measurement availability andmodeling capabilities globally, is produced by using asimpler model at a coarser spatial resoluti<strong>on</strong> with artificialerrors added to boundary inflows and river channelcharacteristics (geometry, roughness etc.). An EnsembleKalman Filter and Smoo<strong>the</strong>r are used to assimilate <strong>the</strong>SWOT observati<strong>on</strong>s into <strong>the</strong> “first-guess” (open-loop)model, and different c<strong>on</strong>figurati<strong>on</strong>s <strong>of</strong> <strong>the</strong> state vectors aretested. Assimilated estimates <strong>of</strong> river discharge and WSE areevaluated against <strong>the</strong> “true” values, and <strong>the</strong> impact <strong>of</strong> <strong>the</strong>partial spatial coverage <strong>of</strong> SWOT at different times isassessed. In additi<strong>on</strong>, <strong>the</strong> temporal persistence <strong>of</strong> <strong>the</strong> SWOT“correcti<strong>on</strong>s” to <strong>the</strong> “first-guess” discharge estimates isquantified and related to <strong>the</strong> river topology. AlthoughSWOT observati<strong>on</strong>s will be provided at 100m resoluti<strong>on</strong>, it ishypo<strong>the</strong>sized that <strong>the</strong> assimilati<strong>on</strong> will be able to downscalethat informati<strong>on</strong> to rivers smaller than that providingdischarge estimates upstream. Finally, <strong>the</strong> informati<strong>on</strong>c<strong>on</strong>tent <strong>of</strong> SWOT observati<strong>on</strong>s is evaluated for <strong>the</strong>estimati<strong>on</strong> <strong>of</strong> o<strong>the</strong>r hydraulic variable such as river bedtopography and channel roughness.Anker, YaakovSmall stream m<strong>on</strong>itoring by spectral classificati<strong>on</strong><strong>of</strong> high spatial resoluti<strong>on</strong>, digital RGB aerial imagesAnker, Yaakov 1, 3 ; Hershkovic, Yar<strong>on</strong> 2 ; Gasith, Avital 2 ; BenDor, Eyal 3 ; Livne, Ido 31. Samaria-Jordan Rift R&D, Ariel University Center, Ariel,Israel2. Zoology, Tel-Aviv University, Tel-Aviv, Israel3. <strong>Remote</strong> <strong>Sensing</strong> Laboratory, Tel-Aviv University, Tel-Aviv,IsraelAquatic plants proliferati<strong>on</strong> in small streams is <strong>of</strong>tenmanaged by seas<strong>on</strong>al variables. Occasi<strong>on</strong>ally biomassesaccumulati<strong>on</strong> might result in damming effect and over-bankflow. Under <strong>the</strong>se circumstances habitat scale m<strong>on</strong>itoring <strong>of</strong>an entire stream secti<strong>on</strong> is essential for crops andinfrastructure destructi<strong>on</strong> preventi<strong>on</strong>. The present workevaluated <strong>the</strong> applicati<strong>on</strong> <strong>of</strong> High Resoluti<strong>on</strong> RGB airbornedigital images spectral analysis (ADP-SA) for small streams(

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