Quick estimates of discharg
Transcrição
Quick estimates of discharg
Quick estimates of discharges along the Negro River constrained by satel... 2010 Meeting of the Americas Search Results http://www.agu.org/cgi-bin/SFgate/SFgate?language=English&verbos... Cite abstracts as Author(s) (2010), Title, Eos Trans. AGU, 91(26), Meet. Am. Suppl., Abstract xxxxx-xx Your query was: bonnet HR: 0800h AN: U31A-07 Poster TI: Quick estimates of discharges along the Negro River constrained by satellite altimetry AU: *Moreira, D M EM: [email protected] AF: COPPE/UFRJ, Rio de Janeiro, Brazil AU: SANTOS DA SILVA, J EM: [email protected] AF: COPPE/UFRJ, Rio de Janeiro, Brazil AU: Souza, A E EM: [email protected] AF: COPPE/UFRJ, Rio de Janeiro, Brazil AU: Calmant, S EM: [email protected] AF: IRD, Brasília, Brazil AU: Seyler, F S EM: [email protected] AF: IRD, Brasília, Brazil AU: Monteiro, A EM: [email protected] AF: CPRM, Rio de Janeiro, Brazil AU: Rotunno Filho, O C EM: [email protected] AF: COPPE/UFRJ, Rio de Janeiro, Brazil AU: Bonnet, M EM: [email protected] AF: IRD, Brasília, Brazil AB: In this study, we present a methodology to obtain discharge values along the Negro River with short delays taking advantage of the rapid delivery of water stages by satellite altimetry. The methodology has the following steps: We modeled the discharges in the Rio Negro using the HEC-RAS model. Model inputs were discharges from rating curves at gauge stations and time-varying Manning coefficients. Indeed, following Chow (1959), temporal variations of the Manning coefficient in a river reach can be determined as the loss of energy due to stage and flow velocity variations at both ends of the reach. This computation of temporal variations of the Manning coefficient requires that the stage variations are leveled. We used various techniques to level the gauge series, including: direct leveling of the gauge with GPS, indirect leveling from the height of the water level at the time when a ship embarking a GPS passed in the vicinity of the gauge and last, leveling using the regression coefficients in the comparison between the gauge readings and water level series by radar altimetry. The water stages in output of the HEC-RAS runs were compared with the height series by satellite altimetry at the location of the crossing of the river with satellite tracks to validate the runs. The discharges in output of the HEC-RAS model at these locations were used to derive rating curves. Finally, these rating curves are used to predict near real time discharge using the radar altimetry heights computed from the fast delivery products provided by the space agencies in the Interim Geophysical Data Records. Reference: Chow, V. T., 1959, Open-channel Hydraulics, McGraw-Hill, NY, USA. DE: [1240] GEODESY AND GRAVITY / Satellite geodesy: results 1 sur 2 06/11/2010 14:55 Quick estimates of discharges along the Negro River constrained by satel... http://www.agu.org/cgi-bin/SFgate/SFgate?language=English&verbos... DE: [1860] HYDROLOGY / Streamflow SC: Union (U) MN: 2010 Meeting of the Americas New Search AGU Home 2 sur 2 06/11/2010 14:55