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
Pavelsky, Tamlin M.C<strong>on</strong>tinuous River Width-Drainage AreaRelati<strong>on</strong>ships in <strong>the</strong> Yuk<strong>on</strong> River BasinPavelsky, Tamlin M. 1 ; Allen, George H. 11. Dept <strong>of</strong> Geological Sciences, University <strong>of</strong> NorthCarolina, Chapel Hill, NC, USAThrough <strong>the</strong>ir role in transporting water and sedimentfrom upland catchments to coastal oceans, rivers play a keyrole in organizing landscapes and represent a major link in<strong>the</strong> global hydrologic cycle. River form varies widely, anddifferent characteristics reflect variati<strong>on</strong>s in discharge,substrate, climate, and human impacts. Studies <strong>of</strong> <strong>the</strong>relati<strong>on</strong>ship between fluvial form and discharge (orcatchment area, which is <strong>of</strong>ten substituted) have beenc<strong>on</strong>ducted since at least <strong>the</strong> early 1950s, with statisticalrelati<strong>on</strong>ships between discharge and river depth, width, andvelocity encapsulated in <strong>the</strong> hydraulic geometry framework.However, large-scale examinati<strong>on</strong>s <strong>of</strong> river form have beenlimited by a lack <strong>of</strong> data, and most prior studies havefocused <strong>on</strong> discrete cross-secti<strong>on</strong>s surveyed <strong>on</strong> <strong>the</strong> ground or<strong>on</strong> descripti<strong>on</strong>s <strong>of</strong> network form (i.e. stream order) ra<strong>the</strong>rthan c<strong>on</strong>tinuous river morphology. More recently, satelliteremote sensing has been used to study river form over largerscales, without <strong>the</strong> need for ground-based surveying. To thispoint, however, studies <strong>of</strong> river form from space have largelyfocused <strong>on</strong> individual river reaches or sets <strong>of</strong> discrete crosssecti<strong>on</strong>sra<strong>the</strong>r than measuring fluvial form c<strong>on</strong>tinuouslyover entire large river basins. In this study, we use <strong>the</strong>RivWidth s<strong>of</strong>tware tool(http://www.unc.edu/~pavelsky/Pavelsky/RivWidth.html) toc<strong>on</strong>tinuously map river widths from 30 m Landsat imageryfor all rivers wider than ~50m in <strong>the</strong> Yuk<strong>on</strong> River Basin <strong>of</strong>Canada and Alaska. The Yuk<strong>on</strong> basin was selected because itis almost entirely free <strong>of</strong> direct human influence <strong>on</strong> riverform, while also c<strong>on</strong>taining a wide range <strong>of</strong> different channelplanforms. The resulting map <strong>of</strong> river widths is <strong>the</strong>n linkedto a map <strong>of</strong> catchment area derived from <strong>the</strong> Hydro1Kdigital elevati<strong>on</strong> dataset, allowing width and catchment areato be c<strong>on</strong>tinuously compared across an entire large riverbasin for <strong>the</strong> first time. From <strong>the</strong>se linked datasets, weevaluate <strong>the</strong> c<strong>on</strong>sistency <strong>of</strong> width-catchment arearelati<strong>on</strong>ships over <strong>the</strong> entire basin and compare individualsub-basins with different characteristics including sedimentload, permafrost extent, and annual precipitati<strong>on</strong>. Inadditi<strong>on</strong>, <strong>the</strong> width dataset developed here provides a firstmeasure <strong>of</strong> which rivers within <strong>the</strong> Yuk<strong>on</strong> Basin will besampled by <strong>the</strong> NASA/CNES Surface Water and OceanTopography (SWOT) satellite missi<strong>on</strong>. One <strong>of</strong> SWOT’s majorgoals is <strong>the</strong> provisi<strong>on</strong> <strong>of</strong> discharge estimates for all riverswider than 100 m, globally, yet <strong>the</strong> extent and locati<strong>on</strong>s <strong>of</strong><strong>the</strong>se rivers remains poorly c<strong>on</strong>strained. We dem<strong>on</strong>strate <strong>the</strong>ability <strong>of</strong> RivWidth measurements to estimate SWOTsampling extent over larger river basins such as <strong>the</strong> Yuk<strong>on</strong>.Peters-Lidard, Christa D.The Impact <strong>of</strong> AMSR-E Soil Moisture Assimilati<strong>on</strong><strong>on</strong> Evapotranspirati<strong>on</strong> Estimati<strong>on</strong>Peters-Lidard, Christa D. 1 ; Kumar, Sujay 2, 1 ; Mocko, David 2, 1 ;Tian, Yud<strong>on</strong>g 3, 11. Hydrological Sciences Laboratory, NASA/GSFC Code 617,Greenbelt, MD, USA2. SAIC, Beltsville, MD, USA3. ESSIC, University <strong>of</strong> Maryland, College Park, MD, USAAn assessment <strong>of</strong> ET estimates for current LDASsystems is provided al<strong>on</strong>g with current research thatdem<strong>on</strong>strates improvement in LSM ET estimates due toassimilating satellite-based soil moisture products. Using <strong>the</strong>Ensemble Kalman Filter in <strong>the</strong> Land Informati<strong>on</strong> System, weassimilate both NASA and Land Parameter Retrieval Model(LPRM) soil moisture products into <strong>the</strong> Noah LSM Versi<strong>on</strong>3.2 with <strong>the</strong> North American LDAS phase 2 (NLDAS-2)forcing to mimic <strong>the</strong> NLDAS-2 c<strong>on</strong>figurati<strong>on</strong>. Throughcomparis<strong>on</strong>s with two global reference ET products, <strong>on</strong>ebased <strong>on</strong> interpolated flux tower data and <strong>on</strong>e from a newsatellite ET algorithm, over <strong>the</strong> NLDAS2 domain, wedem<strong>on</strong>strate improvement in ET estimates <strong>on</strong>ly whenassimilating <strong>the</strong> LPRM soil moisture product.http://lis.gsfc.nasa.govPipunic, RobertImpacts <strong>of</strong> satellite surface soil moistureassimilati<strong>on</strong> <strong>on</strong> modelled root z<strong>on</strong>e soil moistureand ET over a six year period: Assessment across anin-situ soil moisture m<strong>on</strong>itoring network, Murray-Darling Basin, AustraliaPipunic, Robert 1 ; Ryu, D<strong>on</strong>gryeol 1 ; Walker, Jeffrey 21. Department <strong>of</strong> Infrastructure Engineering, TheUniversity <strong>of</strong> Melbourne, Parkville, VIC, Australia2. Department <strong>of</strong> Civil Engineering, M<strong>on</strong>ash University,Clayt<strong>on</strong>, VIC, AustraliaThe importance <strong>of</strong> root z<strong>on</strong>e soil moisture is recognisedfor its role in partiti<strong>on</strong>ing rainfall between infiltrati<strong>on</strong> andrun-<strong>of</strong>f, drainage to groundwater, and as a water storeaccessible to plant roots c<strong>on</strong>tributing to evapotranspirati<strong>on</strong>.Thus accurate predicti<strong>on</strong>s <strong>of</strong> moisture c<strong>on</strong>tent in <strong>the</strong> rootz<strong>on</strong>e will have enormous benefit for land and watermanagement practices including agriculture, flood andwea<strong>the</strong>r forecasting. While this has been l<strong>on</strong>g known, it isstill very difficult to predict <strong>the</strong> soil moisture c<strong>on</strong>tent <strong>of</strong>desired accuracies with spatially distributed Land SurfaceModels (LSMs), which becomes more challenging whenLSMs are run at
- Page 5 and 6:
SCIENTIFIC PROGRAMSUNDAY, 19 FEBRUA
- Page 7 and 8:
1600h - 1900hMM-1MM-2MM-3MM-4MM-5MM
- Page 9 and 10:
GM-7GM-8GM-9GM-10GM-11GM-12GM-13160
- Page 11 and 12:
EM-25EM-26EM-27EM-28EM-29EM-301600h
- Page 13 and 14:
SMM-8SMM-9SMM-10SMM-11SMM-12SMM-13S
- Page 15 and 16:
SCM-24SCM-251600h - 1900hPM-1PM-2PM
- Page 17 and 18:
1030h - 1200h1030h - 1200h1030h - 1
- Page 19 and 20:
ET-13ET-14ET-15ET-16ET-17ET-18ET-19
- Page 21 and 22:
SWT-19SWT-201600h - 1900hSMT-1SMT-2
- Page 23 and 24:
SCT-14SCT-15SCT-16SCT-17SCT-18SCT-1
- Page 25 and 26:
MT-2MT-3MT-4MT-5MT-6MT-7MT-8MT-9MT-
- Page 27 and 28:
1330h - 1530h1530h - 1600h1600h - 1
- Page 29 and 30:
esilience to hydrological hazards a
- Page 31 and 32:
Alfieri, Joseph G.The Factors Influ
- Page 33 and 34:
Montana and Oregon. Other applicati
- Page 35 and 36:
accuracy of snow derivation from si
- Page 37 and 38:
seasonal trends, and integrate clou
- Page 40 and 41:
a single mission, the phrase “nea
- Page 42 and 43:
climate and land surface unaccounte
- Page 44 and 45:
esolution lidar-derived DEM was com
- Page 46 and 47:
further verified that even for conv
- Page 48 and 49:
underway and its utility can be ass
- Page 50 and 51:
Courault, DominiqueAssessment of mo
- Page 52 and 53:
used three Landsat-5 TM images (05/
- Page 55:
storage change solutions in the for
- Page 59 and 60:
Famiglietti, James S.Getting Real A
- Page 61 and 62:
can be thought of as operating in t
- Page 63 and 64:
mission and will address the follow
- Page 65 and 66: Gan, Thian Y.Soil Moisture Retrieva
- Page 67 and 68: match the two sets of estimates. Th
- Page 69 and 70: producing CGF snow cover products.
- Page 71 and 72: performance of the AWRA-L model for
- Page 73 and 74: oth local and regional hydrology. T
- Page 75 and 76: Euphorbia heterandena, and Echinops
- Page 77 and 78: the effectiveness of this calibrati
- Page 79 and 80: presents challenges to the validati
- Page 81 and 82: long period time (1976-2010) was co
- Page 83 and 84: has more improved resolution ( ) to
- Page 85 and 86: in the flow over the floodplain ari
- Page 87 and 88: fraction of the fresh water resourc
- Page 89 and 90: to determine the source of the wate
- Page 91 and 92: hydrologists, was initially assigne
- Page 93 and 94: Sturm et al. (1995) introduced a se
- Page 95 and 96: calendar day are then truncated and
- Page 97 and 98: climate associated with hydrologica
- Page 99 and 100: California Institute of Technology
- Page 101 and 102: egion in Northern California that i
- Page 103 and 104: Moller, DelwynTopographic Mapping o
- Page 105 and 106: obtained from the Fifth Microwave W
- Page 107 and 108: a constraint that is observed spati
- Page 109 and 110: groundwater degradation, seawater i
- Page 111 and 112: approach to estimate soil water con
- Page 113 and 114: Norouzi, HamidrezaLand Surface Char
- Page 115: Painter, Thomas H.The JPL Airborne
- Page 119 and 120: interferometric synthetic aperture
- Page 121 and 122: elevant satellite missions, such as
- Page 123 and 124: support decision-making related to
- Page 125 and 126: oth the quantification of human wat
- Page 127 and 128: parameter inversion of the time inv
- Page 129 and 130: ground-based observational forcing
- Page 131 and 132: Selkowitz, DavidExploring Landsat-d
- Page 133 and 134: Shahroudi, NargesMicrowave Emissivi
- Page 135 and 136: well as subsurface hydrological con
- Page 137 and 138: Sturm, MatthewRemote Sensing and Gr
- Page 139 and 140: Sutanudjaja, Edwin H.Using space-bo
- Page 141 and 142: which can be monitored as an indica
- Page 143 and 144: tools and methods to address one of
- Page 145 and 146: Vanderjagt, Benjamin J.How sub-pixe
- Page 147 and 148: Vila, Daniel A.Satellite Rainfall R
- Page 149 and 150: and landuse sustainability. In this
- Page 151 and 152: e very significant as seepage occur
- Page 153 and 154: Wood, Eric F.Challenges in Developi
- Page 155 and 156: Xie, PingpingGauge - Satellite Merg
- Page 157 and 158: Yebra, MartaRemote sensing canopy c
- Page 159 and 160: used. PIHM has ability to simulate