Sea ice clutter was measured using an X-band radar which is located at the city of Mombetsu in Hokkaido. The pulsewidth of the radar was 80 nsec. To sample by 40 nsec and record digitally, an emitter coupled logic (ECL) was used as a high-speed IC. The sampled data were first transferred to 64 Kbyte dynamic memory board and next to a 5 inch floppy disk through an 8 bit micro-computer. These data were processed by a 16 bit micro-computer. As a result, it is shown that the amplitude of sea ice obeys a Weibull disturibution with shape parameters of c
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Hiroshi OGAWA, Matsuo SEKINE, Toshimitsu MUSHA, Masaaki AOTA, Masayuki OHI, Hiroki FUKUSHI, "Weibull-Distributed Radar Clutter Reflected From Sea Ice" in IEICE TRANSACTIONS on transactions,
vol. E70-E, no. 2, pp. 116-120, February 1987, doi: .
Abstract: Sea ice clutter was measured using an X-band radar which is located at the city of Mombetsu in Hokkaido. The pulsewidth of the radar was 80 nsec. To sample by 40 nsec and record digitally, an emitter coupled logic (ECL) was used as a high-speed IC. The sampled data were first transferred to 64 Kbyte dynamic memory board and next to a 5 inch floppy disk through an 8 bit micro-computer. These data were processed by a 16 bit micro-computer. As a result, it is shown that the amplitude of sea ice obeys a Weibull disturibution with shape parameters of c
URL: https://globals.ieice.org/en_transactions/transactions/10.1587/e70-e_2_116/_p
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@ARTICLE{e70-e_2_116,
author={Hiroshi OGAWA, Matsuo SEKINE, Toshimitsu MUSHA, Masaaki AOTA, Masayuki OHI, Hiroki FUKUSHI, },
journal={IEICE TRANSACTIONS on transactions},
title={Weibull-Distributed Radar Clutter Reflected From Sea Ice},
year={1987},
volume={E70-E},
number={2},
pages={116-120},
abstract={Sea ice clutter was measured using an X-band radar which is located at the city of Mombetsu in Hokkaido. The pulsewidth of the radar was 80 nsec. To sample by 40 nsec and record digitally, an emitter coupled logic (ECL) was used as a high-speed IC. The sampled data were first transferred to 64 Kbyte dynamic memory board and next to a 5 inch floppy disk through an 8 bit micro-computer. These data were processed by a 16 bit micro-computer. As a result, it is shown that the amplitude of sea ice obeys a Weibull disturibution with shape parameters of c
keywords={},
doi={},
ISSN={},
month={February},}
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TY - JOUR
TI - Weibull-Distributed Radar Clutter Reflected From Sea Ice
T2 - IEICE TRANSACTIONS on transactions
SP - 116
EP - 120
AU - Hiroshi OGAWA
AU - Matsuo SEKINE
AU - Toshimitsu MUSHA
AU - Masaaki AOTA
AU - Masayuki OHI
AU - Hiroki FUKUSHI
PY - 1987
DO -
JO - IEICE TRANSACTIONS on transactions
SN -
VL - E70-E
IS - 2
JA - IEICE TRANSACTIONS on transactions
Y1 - February 1987
AB - Sea ice clutter was measured using an X-band radar which is located at the city of Mombetsu in Hokkaido. The pulsewidth of the radar was 80 nsec. To sample by 40 nsec and record digitally, an emitter coupled logic (ECL) was used as a high-speed IC. The sampled data were first transferred to 64 Kbyte dynamic memory board and next to a 5 inch floppy disk through an 8 bit micro-computer. These data were processed by a 16 bit micro-computer. As a result, it is shown that the amplitude of sea ice obeys a Weibull disturibution with shape parameters of c
ER -