MICC_2013_Hakim.pdf
Transcript of MICC_2013_Hakim.pdf
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Microwave Point-to-Point Transmission Impairment
over Malaysia Sea Tidal at 7 GHz
Ahmad Firdaus Hakim Muhammad, Mahamod Ismail, J.S.Mandeep and A.T. Adediji
Dept. of Electrical, Electronic & System EngineeringUniversiti Kebangsaan Malaysia, 43600 UKM Bangi Selangor, Malaysia
Email: [email protected], {mahamod, mandeep}@eng.ukm.my, [email protected]
Abstract Cellular radio deployment involved Point-to-Point
(P2P) microwave transmission and planning. Proper planning
and design must take into consideration various impairments
such as atmosphere, rain attenuation, terrain profile, signal
blockage, and others. In this paper, we analyze received signal
level performance for microwave link propagating over sea tidal.
Data was collected over one day for P2P link with path length of
14.26 km that constitute 73.63% sea tidal. The study showed that
the signal fade varied about 13 dB and at least over 20% of daytime below threshold level.
Keywords-component; propagation; line-of-sight; point-to-
point; sea tidal; multipath
I. INTRODUCTIONMicrowave line-of-sight (LOS) links, sometime referred as
microwave link, LOS microwave, Point-to-Point (P2P) or
radio links, are composed of point-to-point systems between
two terrestrial stations that transmit and receive signal. Thelinks are designed to preserve direct LOS propagation path as
the main propagation mechanism, but in practice other
component and anomalies coexists due to reflection,diffraction, refraction and multipath [1].
The availability of P2P connection between the stationsmust always be nearly perfect (99.99%) in order to ensure that
the transmitted voice/data maintain its integrity at the receiver.
The received signal level or received signal strength must be
above the link threshold to make sure the links have a strength
value to cater for the fade margin. Without adequate value of
fade margin, there will be signal loss within the link in thestations, hence the data/voice signal being transmitted will not
reach the target area and resulted in high bit error ratio (BER).
The challenge in ensuring good system performance is to
ensure that the P2P link can militate against any obstacle
between the medium of the microwave stations.
In this paper, the study of sea tidal as one of the factorsthat affect microwave P2P performance is undertaken.Although there are many other obstructions to microwave P2Ptransmission, such as; rain, dust, terrain obstacle, etc., sea tidalis an obstacle that is very complicated to analyze and itinvolves a solution to some rural area data/voice coverage.The effect of sea tidal or sea ground to microwave propagationis related to multipath fading phenomena.
Hence, in this work, we dealt more on multipath fadingpropagation effect using two prediction models; BarnettVigants, and ITU models. Received Signal Level (RSL)characteristics on a flat terrain are also discussed.
The paper is divided into five sections; the present sectionis the introduction, section II present microwave propagationmechanism due to reflection and multipath fading in particular
to sea tidal followed by site description and signal receptionover P2P links in section III. Section IV analyzes andcompares signal reception collected over one day period forsignal propagates over sea tidal and reflected from groundterrain. Finally in Section V, we conclude the impairment dueto signal propagation over sea tidal and some mitigationtechnique.
II. MICROWAVE PROPAGATION MECHANISMMicrowave P2P typically use LOS mechanisms but
subjected to either clear path (Fresnel Zone) or obstructed path
due to terrain, building, vegetation and others. Multipathpropagation phenomenon and fading occurs when radio signal
reaching the receiving antenna by two or more indirect pathdue to reflection. A rigorous study on the acceptable path
length subjected to the rain attenuation and other factors for
P2P at and above 7 GHz been presented in [2][3].
Tidal fading occurs as a result of the interference between
the direct line-of-sight path from the transmitter antenna to the
receiver antennas and the indirect path that reflect on the waterplane as in Fig.1.
Fig 1. The two ray model, showing (a) the direct path and (b) the indirect path
reflected off the water plane.
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As the tide rises and falls, the length of the reflected path
changes. This in turn causes a change in the phase difference
between the two paths. As the phase difference approaches180 degrees, the interference between the paths will be
increasingly destructive, resulting in a deeper fade. The
reflected path is longer and so may interfere destructively with
the direct path. Refraction is neglected in this diagram. The
ray paths are curved due to the flat-earth representation used
to clarify the reflection. The two phenomenons that getinvolved in the both fluctuated link are reflection and
multipath fading.
A.ReflectionReflection occurs when an electromagnetic wave strikes a
nearly smooth, large surface, such as a water surface, and a
portion of the energy is reflected from the surface and
continues propagating along a path that defines an angle with
the surface equal to that of the incident wave. Obstruction
dimensions are very large compared to the signal wavelength.
The strength of the reflected wave is determined by the
reflection coefficient; a value that depends on the frequencyand polarization of radiation, the angle of incidence, and the
roughness of the reflecting surface.
For shallow incidence angles and smooth seas, typical
values of the reflection coefficient are near unity, i.e., the
reflected wave is almost as strong as the incidence wavecausing the so-calledspecular reflection. The law of reflection
states that for specular reflection, the angle at which the wave
is incident on the surface equals the angle at which it is
reflected. Reflection rays from different surfaces may interfere
constructively or destructively at a receiver causing multipath
propagation or multipath fading.
B.Multipath FadingMultipath fading is the dominant fading mechanism for
frequencies lower than approximately 10 GHz. A reflected
wave causes a phenomenon known as multipath, meaning that
the radio signal can travel many paths to reach the receiver.
Typically, multipath occurs when a reflected wave reaches the
receiver at the same time as the direct wave that travels in a
straight line from the transmitter. Multipath propagation gives
rise to two kinds of signal fading effects, i.e., flat fading and
frequency selective fading. The flat fading effect is due tothermal noise and interference. Certainly, both flat and
selective fading typically occur in combination. Two scenariosof multipath are possible:
i. If the two signals reach the receiver in phase, then thesignal is amplified. This is known as an upfade.
Upfades can also occur when the radio wave is
trapped within an atmospheric duct. As can be seen
from equation (1), higher upfades are possible for
longer paths:
Upfademax = 10 log d 0.03d(dB) (1)
where dis the path length in km.
For example, ford= 14.26 km, the maximum upfade
can be up to 11.11 dB.
ii. If the two waves reach the receiver out of phase, theyweaken the overall received signal. If the two waves
are 180 apart when they reach the receiver, they can
completely cancel each other out which may result intotal loss of signal. A location where a signal is to
cancel out by multipath is called a null ordownfade.
In [4], measurement results show that most multipath
fading occurs at night during the inter-moon seasons when
there is low wind activity and high humidity. Under such
conditions, the sea surface is smooth and the reflected signal isstrong and produces deep and fast multipath fading. The sea
breeze observed over a LOS link situated in Visakhapatnam
operating at 6 GHz [5] brought about some distinct
characteristic changes in the LOS link signal strength.
III. MEASUREMENT SETUP AND DATA COLLECTIONThese comprise site selection, path profile, measurement
setup, and data collection.
A. Site SelectionFour study sites as shown in Figure 2 are selected for P2P
measurement between Station A and Station B with link
distances as summarized in Table 1, however only data for
Kuala Linggi Tanjung Bidara (KLTB/TB-KL) will be
analyzed in this paper.
Fig. 2: P2P Study site
Table 1: Characteristics of the Stations considered for the P2P
measurements.STATION A STATION B LATITUDE A LONGITUDE A LATITUDE B LONGITUDE B LINK DISTANCE(KM) SEA WATER DISTANCE(KM)
Kuala Linggi Tanjung Bidara 02 22 38.40 N 1 01 59 04.90 E 02 18 02.00 N 102 05 15.70 E 14.26 10.5
Pulau Perhentian Bukit Bintang 05 54 04.80 N 1 02 44 29.30 E 05 37 41.99 N 102 38 54.95 E 31.89 20
Pulau Pemanggil Sekakap 02 34 58.20 N 104 18 55.20 E 02 21 43.30 N 103 53 56.10 E 52.4 52
Taman Puteri Wangsa Desa Tebrau 01 35 29.10 N 1 03 47 55.00 E 01 33 30.15 N 103 47 20.84 E 3.8 0
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B. Path ProfileThe path profile is generated using P2P link planning tool,
namely Pathloss 4.0. Figure 3 show path profile for KL-TBthat propagates over sea tidal.
Fig 3. Terrain Profile Kuala Linggi - Tanjung Bidara
C.Measurement SetupThe experimentation set-up for TB-KL reported in this
paper is as shown in Table 2.
Table 2: Base station parameters
Parameter KL Station TB Station
Antenna Size, (m) 1.8 1.8
Frequency (GHz) 7.575
k-factor 1.33
RSL (dBm) -29
D.Data CollectionThe data was collected at three microwave PTP links.
Received signal level (dBm) for main Out Door Unit (ODU)reading was collected. The data was captured and recorded in
IDU monitoring software for one day. Pathloss 4.0 software
was used to generate link budget for all the links and estimated
RSL at receiving station for KL-TB link is -29 dBm as shown
in Table 2.
IV. RESULT AND DISCUSSIONWireless links over estuaries experience time-varying
dependent on height of the tide. This is a problem becauselinks experiencing such fading can degrade in quality or result
in total failure when the fade margin is insufficient. Figure 3and 4 shows the measured signal strength for the KL-TB link
distance of 14.26 km with water spanning 10.5 km of the
entire link between the stations.
Fig. 3: Received Signal Level at Kuala Linggi Station
Fig. 4: Received Signal Level at Tanjung Bidara Station
From the figures, it is observed that RSL fluctuated andfaded most of the time and did not achieve the estimated RSL.
This is because of unstable reflection effect from the sea that
needs further analysis.
A.
Sea Tidal Height AnalysisAs we know sea tidal height can change any time depends
on countrys climate. In this study, the changes of the tidal
height may have effect on the RSL reading. This is because as
the tidal height changes, more multipath fading results due to
effects from the water reflection.
Figures 5 and 6 show the multipath for TB-KL and KL-TBrespectively. There are many reflected and indirect waves
from sea are transmitted back to the receiver area, thus cause
interference to the direct wave and reduced RSL reading. The
interference effects from reflection wave and multipath fading
is called inter-system interference (ISI).
The multipath view only represents certain k-factor values.The ground-earth terrain may not be much affected by the k-
factor; however for sea surface the k-factor varies as sea tidal
height change although not significant.
Path length (14.26 km)
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
Elevation(m)
-10
0
10
20
30
40
50
60
70
80
90
100
110
120
-80
-60
-40
-20
0
8:30:00AM
9:30:00AM
10:30:00AM
11:30:00AM
12:30:00PM
1:30:00PM
2:30:00PM
3:30:00PM
4:30:00PM
5:30:00PM
6:30:00PM
7:30:00PM
8:30:00PM
ReceivedS
ignalLevel(dBm)
Main ODU RSL Vs Time
Current RSL
Maximum RSL
Minimum RSL
-80
-60
-40
-20
0
8:30:00AM
9:30:00AM
10:30:00AM
11:30:00AM
12:30:00PM
1:30:00PM
2:30:00PM
3:30:00PM
4:30:00PM
5:30:00PM
6:30:00PM
7:30:00PM
8:30:00PM
ReceiveSign
alLevel(dBm)
Main ODU RSL Vs Time
Maximum RSL
Minimum RSL
Current RSL
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Fig. 5: Multipath from Tanjung Bidara-Kuala Linggi
Fig. 6: Multipath from Kuala Linggi-Tanjung Bidara
Figure 7 shows the reflection analysis for TB-KL link using
Pathloss 4.0 where RSL fluctuated when there is change in the
k-factors.
Fig. 7: Reflection Analysis.
We observed at Tanjung Bidara site, the RSL change
very badly during 1 PM to 2.45 PM due increase in the seatidal. Table 3 shows and the sea tidal reading Tanjung
Bidara during 9/03/2010 taken from Malaysia Metrological
Department. During that time the interference of reflected
signal strength was too high.
Table 3 Tide Level at Tanjung Bidara
Time Height
0221 1.54 (HIGH)
1200 1.02 (HIGH)
1330 1.03 (HIGH)
2021 0.62 (LOW)
B.Multipath Fading Probability Model
Microwave links as for other links is a must to have
accurate prediction method in order to reduce the different
between simulation results and real system performance.
Nevertheless many microwave links have been deployedaround the world; unfortunately many of these links are in
the short range which path length is less than 20 km.
Therefore to address these constraints, these links need to as
accurate as possible.
There are two famous models in microwave link
propagation prediction model. These are Vigants-Barnett
model and ITU-R Multipath Probability model. The two
outages models are expressed as follows:
Vigants-Barnett [6]:
= 2.5 106310/10 (2)
and ITU-R [7]:
0 = 3.2(1 + )0.97 100.0320.00085/10 (3)
where, f is the frequency, d is the distance K is the
geoclimatic, Cis the terrain factor, FM is the effective fade
margin is the link inclination and hL is the lowestantenna altitude above sea level.
The each link probability is evaluated for both models using
simulated fade margin with link over sea tidal (softwaresimulation) and the measured real fade margin (average per
day). The measured and estimated fade margins are shown
in Tables 4 and 5 respectively.
Table 4: Simulated and measured fade margin over TB-KL link
Table 5: Estimated Fade Margin for Vigants-Barnett and ITU-R Multipath
Probability model
Link Estimated FM (%) Measured FM (%)
Vigants-Barnett 99.99991526 99.99822947
ITU-R 99.99991526 99.99822947
From the tables, the simulated and measured fade margin be
difference at least by 13 dB due to link passing through the
flat sea water.
14.30 1 2 3 4 5 6 7 8 9 10 11 12 13-10
0
10
20
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110
120
14.30 1 2 3 4 5 6 7 8 9 10 11 12 13-10
0
10
20
30
40
50
60
70
80
90
100
110
120
RelativeReceiveSignal(dB)
EarthRadius Factor - arctan(K) ()
53.133.8 36 38 40 42 44 46 48 50 52-1.6
-1.4
-1.2
-1.0
-0.8
-0.6
-0.4
-0.2
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.00
H1=55.0m, H2=45.0m, F=7575.0MHz, V
Link Simulated Measured
TB-KL fade (dB) 37.20 24.0314
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V. CONCLUSIONThe propagation mechanism of a microwave P2P link over
sea tidal has been analyzed using data collected over one day.
The tidal height affects the RSL and deep fades have a
significant impact on link quality. Furthermore, unlike LOS
and ground reflection propagation, tidal effects may be the
primary cause of performance degradation. However, bettermodel should include weather information such as rain and
humidity. In the near future, mitigation methods such as slow
frequency hopping and space diversity strategies will be
investigated.
ACKNOWLEDGMENT
The authors are very grateful and express dear thanks to theUniversiti Kebangsaan Malaysia for funding this work underGPP-2013-006 research university grant.
REFERENCES
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[4] Jin-Teong Ong and Chu-Feng Hu, Propagation measurement on anOver-Water, Line-of-Sight Link in Singapore, Proc. InternationalConference on Information, Communications and Signal Processing(ICICS'97), 9-12 Sept. 1997, pp.1714-1718.
[5] G.S.V. Radha Krishna Rao and M. Purnachandra Rao, A Study on thelnfluence of Sea breeze on Line-Of-Sight links located inVisakhapatnam, Proc. of INMIC 2004, pp. 293-300.
[6] Barnett, W. T., Multipath propagation at 4, 6 and 11 GHz,Bell SystemTechnical Journal,Vol. 51, No. 2, 311-361, Feb. 1972.
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