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

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global scale, having a better spatial coverage and increasednumber <strong>of</strong> observati<strong>on</strong>s. The developed merging strategy isbased <strong>on</strong> <strong>the</strong> use <strong>of</strong> AMSR-E night-time and ASCATobservati<strong>on</strong>s, <strong>of</strong> which <strong>the</strong> qualities were determined using<strong>the</strong> Triple Collocati<strong>on</strong> verificati<strong>on</strong> technique. To improve <strong>the</strong>spatial coverage and <strong>the</strong> number <strong>of</strong> observati<strong>on</strong>s, AMSR-Eday-time and WindSat observati<strong>on</strong>s could be included in <strong>the</strong>merging procedure. Here, we present a quality assessment <strong>of</strong>soil moisture anomalies from active and passive microwaveobservati<strong>on</strong>s which could be used for extending <strong>the</strong> recentlydeveloped merging strategy. We base our analysis <strong>on</strong> <strong>the</strong> use<strong>of</strong> two different evaluati<strong>on</strong> techniques, <strong>the</strong> TripleCollocati<strong>on</strong> and <strong>the</strong> Rvalue verificati<strong>on</strong> technique, and weinclude modeling to support <strong>the</strong> use <strong>of</strong> soil moistureretrievals from day-time passive microwave observati<strong>on</strong>s. Theresults from this study may be used for more comprehensivemerging strategy as <strong>the</strong>y suggest that surface soil moistureestimates from day-time passive microwave observati<strong>on</strong>sincrease in quality with increasing vegetati<strong>on</strong> cover. Inregi<strong>on</strong>s where passive and active products perform similarlywell, weighting functi<strong>on</strong>s may be derived using <strong>the</strong> resultspresented in this study.Parinussa, RobertA Multi-decadal soil moisture dataset from passiveand active microwave soil moisture retrievalsParinussa, Robert 1 ; De Jeu, Richard 1 ; Dorigo, Wouter 2 ; Liu,Yi 3, 1 ; Wagner, Wolfgang 2 ; Fernandez, Diego 41. Hydrology and Geo-envir<strong>on</strong>mental sciences, VUUniversity Amsterdam, Amsterdam, Ne<strong>the</strong>rlands2. Institute for Photogrammetry and <strong>Remote</strong> <strong>Sensing</strong>,Vienna University <strong>of</strong> Technology, Vienna, Austria3. Climate Change Research Centre, University <strong>of</strong> NewSouth Wales, Sydney, NSW, Australia4. ESA, ESRIN, Frascati, ItalyRecently, as part <strong>of</strong> <strong>the</strong> Water Cycle Multimissi<strong>on</strong>Observati<strong>on</strong> Strategy (WACMOS) project a methodology hasbeen developed to build a harm<strong>on</strong>ized multi-decadal satellitesoil moisture dataset. The VU University Amsterdam –Nati<strong>on</strong>al Aer<strong>on</strong>autics and Space Administrati<strong>on</strong> (VUA-NASA) passive microwave products derived from foursatellites and <strong>the</strong> Vienna University <strong>of</strong> Technology (TU-Wien) active microwave products derived from two satelliteswere used in this study. The products were merged, rescaled,ranked and blended into <strong>on</strong>e final product. The harm<strong>on</strong>izedsoil moisture values were compared to in situ data from <strong>the</strong>Internati<strong>on</strong>al Soil Moisture Network (ISMN) and generallyshowed a better agreement than <strong>the</strong> individual products.Interannual variability and l<strong>on</strong>g term trends within this soilmoisture dataset were analyzed and evaluated usingadditi<strong>on</strong>al datasets, including tree ring data and oceanoscillati<strong>on</strong> indices. These results gave us c<strong>on</strong>fidence in <strong>the</strong>quality <strong>of</strong> this new product. This product will now befur<strong>the</strong>r improved and implemented within <strong>the</strong> ClimateChange Initiative (CCI) programme <strong>of</strong> ESA.Paris, AdrienIMPROVING DISCHARGE ESTIMATES IN ALARGE, POORLY GAUGE BASIN BY TUNING AHYDROLOGICAL MODEL WITH SATELLITEALTIMETRY INFORMATIONCalmant, Stephane 1 ; Paris, Adrien 2, 1 ; Santos da Silva,Joecila 3 ; Collisch<strong>on</strong>n, Walter 2 ; Paiva, Rodrigo 2, 4 ; B<strong>on</strong>net,Marie-Paule 4 ; Seyler, Frederique 51. OMP-LEGOS-IRD, Toulouse Cedex 09, France2. IPH - UFRGS, Porto Alegre, Brazil3. CESTU - UEA, Manaus, Brazil4. UMR-GET-IRD, Toulouse, France5. UMR-Espace DEV-IRD, M<strong>on</strong>tpellier, FranceAccurate modeling <strong>of</strong> discharge in a basin requires alarge amount <strong>of</strong> informati<strong>on</strong>. This informati<strong>on</strong> is threefold:First, knowledge <strong>of</strong> <strong>the</strong> river geometry such as <strong>the</strong> slope <strong>of</strong>river surface and bottom, <strong>the</strong> width <strong>of</strong> <strong>the</strong> cross secti<strong>on</strong>throughout <strong>the</strong> river course, <strong>the</strong> height at whichoverbanking occurs; sec<strong>on</strong>d knowledge <strong>of</strong> <strong>the</strong> watershed,DTM soil characteristics and vegetati<strong>on</strong> type; and last,physical parameters such as a fricti<strong>on</strong> coefficient, includingits space and time variati<strong>on</strong>s (i.e. seas<strong>on</strong>al variati<strong>on</strong>s withwater level). In most large tropical basins, knowledge <strong>of</strong> <strong>the</strong>river geometry is dramatically lacking, in particular in <strong>the</strong>most upstream, remote, parts. Satellite altimetry providestime series <strong>of</strong> altitude <strong>of</strong> <strong>the</strong> river surface. Because <strong>the</strong>seseries are naturally leveled, slope <strong>of</strong> <strong>the</strong> river surface can alsobe derived easily. Also, in some favorable cases, <strong>the</strong> geometry<strong>of</strong> <strong>the</strong> secti<strong>on</strong> crossed by <strong>the</strong> satellite track is imaged by <strong>the</strong>successive height pr<strong>of</strong>iles, between <strong>the</strong> lowest and higheststages. The time sampling <strong>of</strong> <strong>the</strong>se series is quite poor,ranging from every decade in <strong>the</strong> best cases to a fewmeasurements a year in <strong>the</strong> worse cases. In turn, <strong>the</strong> spacingis ra<strong>the</strong>r good, from a few km to a few hundreds <strong>of</strong> km. TheMGB model was developed at IPH to compute river flow inlarge basins. Originally, for reaches where actual data arelacking, <strong>the</strong> riverbed geometry was derived from empiricalgeomorphological relati<strong>on</strong>ships. Besides, <strong>the</strong> flow dynamicshad to be left unc<strong>on</strong>strained and unchecked down until <strong>the</strong>first gauging stati<strong>on</strong>. In <strong>the</strong> present study, we present recentimprovements obtained in <strong>the</strong> flow modeling by tuning <strong>the</strong>MGB model in order that <strong>the</strong> river geometry and modeloutputs better fit altimetry series. We present and discuss<strong>the</strong> benefits gained in <strong>the</strong> case <strong>of</strong> <strong>the</strong> Japura-Caqueta river, in<strong>the</strong> Amaz<strong>on</strong> basin. The Japura-Caqueta river is atransboundary river, called Caqueta in its upstreamColombian part and Japura in its downstream, Brazilianpart. No gauge measurements are available in <strong>the</strong> Colombianpart, and <strong>on</strong>ly 3 gauging stati<strong>on</strong>s exist in <strong>the</strong> Brazilian part,when 29 ENVISAT tracks cross <strong>the</strong> river, making as muchopportunities to put c<strong>on</strong>strains <strong>on</strong> model parameters suchas reach width, river slope, or model outputs such as stagevariati<strong>on</strong>s.116

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