- 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: MT-2MT-3MT-4MT-5MT-6MT-7MT-8MT-9MT-
- 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
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presents challenges to the validati
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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
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hydrologists, was initially assigne
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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
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California Institute of Technology
- Page 101 and 102:
egion in Northern California that i
- Page 103 and 104:
Moller, DelwynTopographic Mapping o
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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 and 116:
Painter, Thomas H.The JPL Airborne
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Pavelsky, Tamlin M.Continuous River
- 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
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Shahroudi, NargesMicrowave Emissivi
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well as subsurface hydrological con
- Page 137 and 138:
Sturm, MatthewRemote Sensing and Gr
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Sutanudjaja, Edwin H.Using space-bo
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which can be monitored as an indica
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tools and methods to address one of
- Page 145 and 146:
Vanderjagt, Benjamin J.How sub-pixe
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Vila, Daniel A.Satellite Rainfall R
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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
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Xie, PingpingGauge - Satellite Merg
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Yebra, MartaRemote sensing canopy c
- Page 159 and 160:
used. PIHM has ability to simulate