2018
DOI: 10.1002/dac.3779
|View full text |Cite
|
Sign up to set email alerts
|

Joint low‐complexity equalization and carrier frequency offset compensation for underwater acoustic OFDM communication systems with banded‐matrix approximation at different channel conditions

Abstract: Summary Underwater acoustic wireless communication is considered as one of the most challenging communication technologies due to low propagation speed, water salinity, water depth, PH degree, and water temperature. Equalization is one of the means to improve the system performance. Matched filter (MF), zero forcing (ZF), and minimum mean square error (MMSE) equalizers can be used for channel equalization. Unfortunately, the performance of the matched filter is destroyed in the Multiple‐Input Multiple‐Output (… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1

Citation Types

0
17
0

Year Published

2019
2019
2022
2022

Publication Types

Select...
5

Relationship

2
3

Authors

Journals

citations
Cited by 20 publications
(17 citation statements)
references
References 38 publications
0
17
0
Order By: Relevance
“…At the receiver side, the CP vector is removed and the N ‐point FFT matrix F N ϵ ℂ N × N converts the time‐domain vector to frequency‐domain as: Y=boldη0.25emboldHπX+Z, where Y ϵ ℂ 2 N × 1 is the received frequency‐domain vector, X ϵ ℂ 2 N × 1 represents the transmitted frequency‐domain samples after the mapping process, and Z denotes the noise vector. H , and η ϵ ℂ 2 N × 2 N are the frequency‐domain MIMO channel matrix, and the interference matrix, respectively, given as in References : H=boldH11boldH12boldH21boldH22, η=boldηm,p0N×N0N×Nboldηm,p, where H ji ϵ ℂ N × N represents the frequency‐domain channel matrix between the j th transmit antenna and the i th receive antenna. The MIMO channel induces inter‐antenna interference due to its coupling nature.…”
Section: Mimo‐ofdm System Modelmentioning
confidence: 99%
See 1 more Smart Citation
“…At the receiver side, the CP vector is removed and the N ‐point FFT matrix F N ϵ ℂ N × N converts the time‐domain vector to frequency‐domain as: Y=boldη0.25emboldHπX+Z, where Y ϵ ℂ 2 N × 1 is the received frequency‐domain vector, X ϵ ℂ 2 N × 1 represents the transmitted frequency‐domain samples after the mapping process, and Z denotes the noise vector. H , and η ϵ ℂ 2 N × 2 N are the frequency‐domain MIMO channel matrix, and the interference matrix, respectively, given as in References : H=boldH11boldH12boldH21boldH22, η=boldηm,p0N×N0N×Nboldηm,p, where H ji ϵ ℂ N × N represents the frequency‐domain channel matrix between the j th transmit antenna and the i th receive antenna. The MIMO channel induces inter‐antenna interference due to its coupling nature.…”
Section: Mimo‐ofdm System Modelmentioning
confidence: 99%
“…Different approaches have been used to improve the performance of wireless radio communication systems such as multiple‐input‐multiple output (MIMO) configuration, Frequency‐domain equalization (FDE), and time‐domain equalization . In References , the authors presented linear equalizers that jointly perform FDE and CFO compensation with lower complexity using banded‐matrix approximation . In fact, these equalizers do not implement the successive interference cancellation (SIC) over spatial streams.…”
Section: Introductionmentioning
confidence: 99%
“…2 In general, the ocean water can be divided into four horizontal layers: the surface layer (mixed layer), seasonal thermocline layer, permanent thermocline layer, and deep isothermal layer. The UWA channel has a lot of challenges such as attenuation, water salinity, temperature, frequency-dependent attenuation, and time-varying nature.…”
Section: Introductionmentioning
confidence: 99%
“…Thus, those challenges cause a limitation to communications in sea water. 2 In general, the ocean water can be divided into four horizontal layers: the surface layer (mixed layer), seasonal thermocline layer, permanent thermocline layer, and deep isothermal layer. The sound propagation speed differs in each layer because of the variation of the water properties (salinity, pressure, and temperature).…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation