Essential Limitations to Signal Detection and Estimation: An Application to the Arctic Under Ice Environmental Noise Problem
It has been observed that Arctic under ice noise is at times composed of narrowband components. The narrowband noise is primarily due to rubbing ice flows but possibly acoustic dispersion contributes to this phenomenon. This type of interference can significantly degrade the performance of systems w...
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ftdtic:ADA143828 2023-05-15T14:43:17+02:00 Essential Limitations to Signal Detection and Estimation: An Application to the Arctic Under Ice Environmental Noise Problem Dwyer,R F NAVAL UNDERWATER SYSTEMS CENTER NEW LONDON CT NEW LONDON LAB 1984-01 text/html http://www.dtic.mil/docs/citations/ADA143828 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA143828 en eng http://www.dtic.mil/docs/citations/ADA143828 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Acoustic Detection and Detectors *ENVIRONMENTS *ACOUSTIC DETECTION *NOISE *NARROWBAND *UNDERICE FREQUENCY TIME INTERVALS AUTOCORRELATION ICE SIGNALS SOUND INTERFERENCE NAVAL RESEARCH FAST FOURIER TRANSFORMS STATISTICAL ANALYSIS FUNCTIONS(MATHEMATICS) ARCTIC REGIONS LPN-NUSC-A75030 Text 1984 ftdtic 2016-02-20T23:01:55Z It has been observed that Arctic under ice noise is at times composed of narrowband components. The narrowband noise is primarily due to rubbing ice flows but possibly acoustic dispersion contributes to this phenomenon. This type of interference can significantly degrade the performance of systems which estimate autocorrelation functions to obtain bearing and range information. The data were collected as part of the 1980 Arctic Ocean experiments. Many segments of Arctic under ice data contained these highly dynamic narrowband components as shown in Figure 1. The statistical behavior of the dynamic narrowband frequency components were measured by first transforming the data into the frequency domain using a fast Fourier transform (FFT). Then the Kurtosis was estimated for each real and imaginary part of each frequency component over the band for a group of consecutive FFT segments. This procedure is called frequency domain Kurtosis (FDK) estimation. Thus, the FDK estimates the distribution over a time interval consisting of many FFT segments for each real and imaginary frequency component. Many of the Arctic data segments showed non-Gaussian components in the frequency domain based on the FDK estimate. This was due mainly to the highly dynamic nature of the narrowband ice components. Therefore, the FDK is a method whereby the desired signal can be distinguished from the unwanted ice sound. Presented at the International Conference on Acoustics, Speech, and Signal Processing, 19-21 Mar 84, San Diego, CA. Text Arctic Arctic Ocean Ice permafrost Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean |
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Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Snow Ice and Permafrost Acoustic Detection and Detectors *ENVIRONMENTS *ACOUSTIC DETECTION *NOISE *NARROWBAND *UNDERICE FREQUENCY TIME INTERVALS AUTOCORRELATION ICE SIGNALS SOUND INTERFERENCE NAVAL RESEARCH FAST FOURIER TRANSFORMS STATISTICAL ANALYSIS FUNCTIONS(MATHEMATICS) ARCTIC REGIONS LPN-NUSC-A75030 |
spellingShingle |
Snow Ice and Permafrost Acoustic Detection and Detectors *ENVIRONMENTS *ACOUSTIC DETECTION *NOISE *NARROWBAND *UNDERICE FREQUENCY TIME INTERVALS AUTOCORRELATION ICE SIGNALS SOUND INTERFERENCE NAVAL RESEARCH FAST FOURIER TRANSFORMS STATISTICAL ANALYSIS FUNCTIONS(MATHEMATICS) ARCTIC REGIONS LPN-NUSC-A75030 Dwyer,R F Essential Limitations to Signal Detection and Estimation: An Application to the Arctic Under Ice Environmental Noise Problem |
topic_facet |
Snow Ice and Permafrost Acoustic Detection and Detectors *ENVIRONMENTS *ACOUSTIC DETECTION *NOISE *NARROWBAND *UNDERICE FREQUENCY TIME INTERVALS AUTOCORRELATION ICE SIGNALS SOUND INTERFERENCE NAVAL RESEARCH FAST FOURIER TRANSFORMS STATISTICAL ANALYSIS FUNCTIONS(MATHEMATICS) ARCTIC REGIONS LPN-NUSC-A75030 |
description |
It has been observed that Arctic under ice noise is at times composed of narrowband components. The narrowband noise is primarily due to rubbing ice flows but possibly acoustic dispersion contributes to this phenomenon. This type of interference can significantly degrade the performance of systems which estimate autocorrelation functions to obtain bearing and range information. The data were collected as part of the 1980 Arctic Ocean experiments. Many segments of Arctic under ice data contained these highly dynamic narrowband components as shown in Figure 1. The statistical behavior of the dynamic narrowband frequency components were measured by first transforming the data into the frequency domain using a fast Fourier transform (FFT). Then the Kurtosis was estimated for each real and imaginary part of each frequency component over the band for a group of consecutive FFT segments. This procedure is called frequency domain Kurtosis (FDK) estimation. Thus, the FDK estimates the distribution over a time interval consisting of many FFT segments for each real and imaginary frequency component. Many of the Arctic data segments showed non-Gaussian components in the frequency domain based on the FDK estimate. This was due mainly to the highly dynamic nature of the narrowband ice components. Therefore, the FDK is a method whereby the desired signal can be distinguished from the unwanted ice sound. Presented at the International Conference on Acoustics, Speech, and Signal Processing, 19-21 Mar 84, San Diego, CA. |
author2 |
NAVAL UNDERWATER SYSTEMS CENTER NEW LONDON CT NEW LONDON LAB |
format |
Text |
author |
Dwyer,R F |
author_facet |
Dwyer,R F |
author_sort |
Dwyer,R F |
title |
Essential Limitations to Signal Detection and Estimation: An Application to the Arctic Under Ice Environmental Noise Problem |
title_short |
Essential Limitations to Signal Detection and Estimation: An Application to the Arctic Under Ice Environmental Noise Problem |
title_full |
Essential Limitations to Signal Detection and Estimation: An Application to the Arctic Under Ice Environmental Noise Problem |
title_fullStr |
Essential Limitations to Signal Detection and Estimation: An Application to the Arctic Under Ice Environmental Noise Problem |
title_full_unstemmed |
Essential Limitations to Signal Detection and Estimation: An Application to the Arctic Under Ice Environmental Noise Problem |
title_sort |
essential limitations to signal detection and estimation: an application to the arctic under ice environmental noise problem |
publishDate |
1984 |
url |
http://www.dtic.mil/docs/citations/ADA143828 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA143828 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Ice permafrost |
genre_facet |
Arctic Arctic Ocean Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA143828 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766314965786951680 |