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Record #166498:
- #166498
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MARC recordOn the shape of refecting surfaces investigated by a 60 MHz radar / C. Bianchi, U. Sciacca, E. Tabacco, A. Zirizzotti, E. Zuccherettit.
| Title: | On the shape of refecting surfaces investigated by a 60 MHz radar / C. Bianchi, U. Sciacca, E. Tabacco, A. Zirizzotti, E. Zuccherettit. |
| Author(s): | Bianchi, C. Sciacca, U. Tabacco, E. Zirizzotti, A. Zuccherettit, E. |
| Date: | 2003. |
| In: | International Journal of Remote Sensing. (2003.), Vol. 24(15) (2003) |
| Abstract: | Describes radio echo sounding (RES) system used to study Drygalski ice tongue, Antarctica. Presents analysis of amplitude of received signals and discusses results of actual measurements. Presents model of reflecting surface and compares forecasts from it with experimental results. Concludes that, under certain conditions, amplitude variations arise mainly from focusing or defocusing effects determined by reflector shape. |
| Notes: | International Journal of Remote Sensing. Vol. 24(15) :3049-3058 (2003). |
| Keywords: | 551.32 -- Glaciology. 551.321 -- Glaciological methods and instruments. 551.321.61 -- Ice sounding, geophysical methods. 551.324 -- Land ice. 551.324.28 -- Ice shelves: Drygalski ice tongue. 621.396.96 -- Radar. E3 -- Glaciology: instruments and methods. (*7) -- Antarctic regions. |
| SPRI record no.: | 166498 |
LDR 01687naa#a2200000#a#4500 001 SPRI-166498 005 20230402093855.0 007 ta 008 230402s2003####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-166498 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aOn the shape of refecting surfaces investigated by a 60 MHz radar /‡cC. Bianchi, U. Sciacca, E. Tabacco, A. Zirizzotti, E. Zuccherettit. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2003. 300 ## ‡ap. 3049-3058 :‡bdiags., tables. 500 ## ‡aInternational Journal of Remote Sensing. Vol. 24(15) :3049-3058 (2003). 520 3# ‡aDescribes radio echo sounding (RES) system used to study Drygalski ice tongue, Antarctica. Presents analysis of amplitude of received signals and discusses results of actual measurements. Presents model of reflecting surface and compares forecasts from it with experimental results. Concludes that, under certain conditions, amplitude variations arise mainly from focusing or defocusing effects determined by reflector shape. 530 ## ‡aAlso issued online ‡uurn:doi:10.1080/0143116031000070300‡uhttps://dx.doi.org/10.1080/0143116031000070300 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.321 -- Glaciological methods and instruments.‡2udc 650 07 ‡a551.321.61 -- Ice sounding, geophysical methods.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.28 -- Ice shelves: Drygalski ice tongue.‡2udc 650 07 ‡a621.396.96 -- Radar.‡2udc 650 07 ‡aE3 -- Glaciology: instruments and methods.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 700 1# ‡aBianchi, C. 700 1# ‡aSciacca, U. 700 1# ‡aTabacco, E. 700 1# ‡aZirizzotti, A. 700 1# ‡aZuccherettit, E. 773 0# ‡7nnas ‡tInternational Journal of Remote Sensing. ‡gVol. 24(15) (2003) ‡wSPRI-1038 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230402