http://www.cnr.it/ontology/cnr/individuo/prodotto/ID183274
Analysis of Envisat RA2 altimeter sigma-nought bloom events for S and Ku bands backscattering intercomparison (Contributo in atti di convegno)
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- Analysis of Envisat RA2 altimeter sigma-nought bloom events for S and Ku bands backscattering intercomparison (Contributo in atti di convegno) (literal)
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- 2005-01-01T00:00:00+01:00 (literal)
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De Biasio F.; Pierdicca N.; Zecchetto S.; Pulvirenti L. (2005)
Analysis of Envisat RA2 altimeter sigma-nought bloom events for S and Ku bands backscattering intercomparison
in Envisat & ERS Symposium, Salzburg, Austria, 6-10 September 2004
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- De Biasio F.; Pierdicca N.; Zecchetto S.; Pulvirenti L. (literal)
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- Proceedings of the 2004 Envisat & ERS Symposium, 6-10 September 2004, Salzburg, Austria (ESA SP-572, April 2005) (literal)
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- 1,3. : ISAC, CNR, Corso Stati Uniti 4, 35127 Padova, Italy /
2,4 : Pierdicca, N. ; Pulvirenti, L. : Dept. Electronic Engineering, Univ. La Sapienza of Rome, V. Eudossiana 18, 00184 Roma, Italy (literal)
- Titolo
- Analysis of Envisat RA2 altimeter sigma-nought bloom events for S and Ku bands backscattering intercomparison (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#isbn
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- H. Lacoste ; L. Ouwehand (literal)
- Abstract
- The RA2 radar altimeter onboard the European Satellite Envisat is a double band microwave instrument working at Ku- and S-band. The S-band measurements provide appropriate atmospheric corrections for the more precise Ku-band measurements, but are also used in conjunction with the Ku-band data in order to investigate the underlying surface. In this study we try to identify differences and similarities of the backscatter signal in the two bands. We focus our attention on the condition of specular alike radar returns, which mostly occur on sea-ice regions. An attempt to find situations in which highly correlated radar waveforms in the two bands can be ascribed to simple scattering mechanisms is made in order to find indications on the mutual calibration of the two channels. The paper reports a number of cases ancountered while analyzing RA-2 data. Both level 2 (1 Hz geophysical parameters) and level 1 (18 Hz waveforms) have been used. (literal)
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