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

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Gebregiorgis, Abebe S.Characterizing Satellite Rainfall Errors based <strong>on</strong>Land Use and Land Cover and Tracing Error Sourcein Hydrologic Model Simulati<strong>on</strong>Gebregiorgis, Abebe S. 1 ; Peters-Lidard, Christa D. 2 ; Tian,Yud<strong>on</strong>g 2, 3 ; Hossain, Faisal 11. Civil and Envir<strong>on</strong>mental Eng’g, Tennessee TechnologicalUniversity, Cookeville, TN, USA2. Hydrological Science Branch, NASA Goddard SpaceFlight Center, Greenbelt, MD, USA3. Goddard Earth Sciences and Technology Center,University <strong>of</strong> Maryland Baltimore County, Greenbelt,MD, USAHydrologic modeling has benefited from operati<strong>on</strong>alproducti<strong>on</strong> <strong>of</strong> high resoluti<strong>on</strong> satellite rainfall products. Theglobal coverage, near-real time availability, spatial andtemporal sampling resoluti<strong>on</strong>s have advanced <strong>the</strong>applicati<strong>on</strong> <strong>of</strong> physically based semi-distributed anddistributed hydrologic models for wide range <strong>of</strong>envir<strong>on</strong>mental decisi<strong>on</strong> making processes. Despite thissuccess, <strong>the</strong> existence <strong>of</strong> uncertainties inherent in <strong>the</strong>indirect way <strong>of</strong> satellite rainfall estimati<strong>on</strong> and hydrologicmodels pose a challenge in making meaningful and practicalpredicti<strong>on</strong>s. This study comprises breaking down <strong>of</strong> totalsatellite rainfall error into three independent comp<strong>on</strong>ents(hit bias, missed precipitati<strong>on</strong> and false alarm),characterizing <strong>the</strong>m as functi<strong>on</strong> <strong>of</strong> land use and land cover(LULC), and tracing back <strong>the</strong> source <strong>of</strong> simulated soilmoisture and run<strong>of</strong>f error in physically based distributedhydrologic model. Here, we asked “<strong>on</strong> what way <strong>the</strong> threeindependent total bias comp<strong>on</strong>ents, hit bias, missed, andfalse precipitati<strong>on</strong>, affect <strong>the</strong> estimati<strong>on</strong> <strong>of</strong> soil moisture andrun<strong>of</strong>f in a physically based hydrologic model?” Weimplemented a systematic approach by characterizing anddecomposing <strong>the</strong> total satellite rainfall error as a functi<strong>on</strong> <strong>of</strong>land use and land cover <strong>of</strong> <strong>the</strong> Mississippi basin. Thisfacilitated <strong>the</strong> understanding <strong>of</strong> <strong>the</strong> major source <strong>of</strong> soilmoisture and run<strong>of</strong>f errors in hydrologic model simulati<strong>on</strong>and tracing back <strong>of</strong> <strong>the</strong> informati<strong>on</strong> to algorithmdevelopment and sensor type. C<strong>on</strong>sequently, we believe sucha forensic approach stands to improve algorithmdevelopment, applicati<strong>on</strong> and data assimilati<strong>on</strong> scheme forGlobal Precipitati<strong>on</strong> Measurement (GPM) missi<strong>on</strong>. Keywords: total bias, hit bias, missed precipitati<strong>on</strong>, false alarm,soil moisture error, and run<strong>of</strong>f error, land use and land cover66Gebremichael, Mek<strong>on</strong>nenEstimati<strong>on</strong> <strong>of</strong> Daily Evapotranspirati<strong>on</strong> over Africausing MODIS/Terra and SEVIRI/MSG dataGebremichael, Mek<strong>on</strong>nen 1 ; Sun, Zhigang 21. Civil and Env. Engineering, University <strong>of</strong> C<strong>on</strong>necticut,Storrs, CT, USA2. Nati<strong>on</strong>al Institute <strong>of</strong> Envir<strong>on</strong>mental Studies, Tsukuba,JapanMost existing remote sensing-based evapotranspirati<strong>on</strong>(ET) algorithms rely exclusively <strong>on</strong> polar-orbiting satelliteswith <strong>the</strong>rmal infrared sensors, and <strong>the</strong>refore <strong>the</strong> resulting ETvalues represent <strong>on</strong>ly “instantaneous or snapshot” values.However, daily ET is more meaningful and useful inapplicati<strong>on</strong>s. In this study, daily ET estimates are obtainedby combining data from <strong>the</strong> MODIS sensor aboard <strong>the</strong>polar-orbiting Terra satellite and <strong>the</strong> SEVIRI sensor aboard<strong>the</strong> geostati<strong>on</strong>ary-orbiting MSG satellite. The procedurec<strong>on</strong>sists <strong>of</strong> estimating <strong>the</strong> instantaneous evaporative fracti<strong>on</strong>(EF) based <strong>on</strong> <strong>the</strong> MODIS/Terra land data products, andestimating <strong>the</strong> daily net radiati<strong>on</strong> and daily available energybased <strong>on</strong> <strong>the</strong> 30-min SEVIRI/MSG data products. Assumingc<strong>on</strong>stant EF during <strong>the</strong> daytime, daily ET is estimated as <strong>the</strong>product <strong>of</strong> <strong>the</strong> SEVIRI/MSG-based daily available energy andMODIS/Terra-based instantaneous EF. The daily ETestimates are evaluated against flux tower measurements atfour validati<strong>on</strong> sites in Africa. Results indicate that <strong>the</strong>synergistic use <strong>of</strong> SEVIRI/MSG and MODIS/Terra has <strong>the</strong>potential to provide reliable estimates <strong>of</strong> daily ET during wetperiods when daily ET exceeds 1 mm/day. The satellite-baseddaily ET estimates however tend to underestimate ET by 13%to 35%. The daily ET estimati<strong>on</strong> algorithm can fur<strong>the</strong>r beimproved by incorporating a temporal data-fillinginterpolati<strong>on</strong> technique to estimate <strong>the</strong> unavailable netradiati<strong>on</strong> informati<strong>on</strong> during cloudy sky c<strong>on</strong>diti<strong>on</strong>s, and byimproving <strong>the</strong> accuracy <strong>of</strong> <strong>the</strong> instantaneous EF. Theassumpti<strong>on</strong> <strong>of</strong> c<strong>on</strong>stant evaporative fracti<strong>on</strong> during <strong>the</strong> dayis reas<strong>on</strong>able, and does not result in substantial errors in <strong>the</strong>daily ET estimates.Gebremichael, Mek<strong>on</strong>nenError Model and Tuning Extremes for SatelliteRainfall EstimatesGebremichael, Mek<strong>on</strong>nen 11. Civil and Env. Engineering, University <strong>of</strong> C<strong>on</strong>necticut,Storrs, CT, USAA new model is developed that generates <strong>the</strong>distributi<strong>on</strong> <strong>of</strong> actual rainfall values for any given satelliterainfall estimate. The model handles <strong>the</strong> c<strong>on</strong>diti<strong>on</strong>aldistributi<strong>on</strong> as <strong>the</strong> mixture <strong>of</strong> a positive c<strong>on</strong>tinuousdistributi<strong>on</strong> and a point mass at zero. A method is alsopresented to probabilistically transform a set <strong>of</strong> satelliterainfall estimates into <strong>the</strong> more accurate rainfall estimates.As our c<strong>on</strong>cern lies with extreme precipitati<strong>on</strong>, a peaks overthreshold extreme value approach is adopted that fits aPareto distributi<strong>on</strong> to <strong>the</strong> large precipitati<strong>on</strong> estimates. Asimple distributi<strong>on</strong>al transformati<strong>on</strong> result is <strong>the</strong>n used to

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