The original paper is in English. Non-English content has been machine-translated and may contain typographical errors or mistranslations. ex. Some numerals are expressed as "XNUMX".
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The original paper is in English. Non-English content has been machine-translated and may contain typographical errors or mistranslations. Copyrights notice
A obstrução do gelo marinho foi medida usando um radar de banda X localizado na cidade de Mombetsu, em Hokkaido. A largura de pulso do radar era de 80 nseg. Para amostrar em 40 ns e gravar digitalmente, uma lógica acoplada ao emissor (ECL) foi usada como um IC de alta velocidade. Os dados amostrados foram primeiramente transferidos para uma placa de memória dinâmica de 64 Kbytes e posteriormente para um disquete de 5 polegadas através de um microcomputador de 8 bits. Esses dados foram processados por um microcomputador de 16 bits. Como resultado, mostra-se que a amplitude do gelo marinho obedece a uma distribuição de Weibull com parâmetros de forma de 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://global.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 -