2. Related Work
For aircraft near tropopause altitudes over oceans and wide deserts, the only current practical and feasible wireless communication can be achieved using low-Earth orbit (LEO) satellites which provide limited broadband Internet speeds of few Mbps or even lower per user [
7]. For example, Inmarsat satellites [
8] provide global mobile connectivity for aviation where passengers onboard an aircraft are kept connected through broadband Internet services and the maintenance data can be sent also to ground for analysis and improved aircraft safety. Although LEO satellites provide wide coverage and global connectivity, they suffer from short orbital periods and visibility duration and requires also very frequent handover processes which complicates the system operation and reduces the availability of the network connections. For example, the recent deployed Starlink satellites [
9] at 550 km orbit altitude or OneWeb satellites [
10] orbiting at 1200 km altitude are only visible for a few minutes per satellite. In addition, the very high speed of LEO satellites results in large Doppler frequency shifts during flight which complicates the system operation and its related communication circuits. In addition, the other medium and geostationary satellite orbits suffer from even more operational difficulties including larger signal attenuation and longer delay time [
11]. Recently in [
11], “GeoSurf” polar satellites constellation have been designed at altitudes ranging from 1500 up to 35,876 km which provide communication over zenith paths with most of the advantages of satellites at different altitudes. However, the continuous movement of satellites requires complex communication infrastructure and inter-satellite link design. On the other hand, aircraft can also communicate with ground-based transmitters through air-to-ground connectivity (ATG) [
12,
13,
14,
15,
16,
17,
18] using L-band digital aeronautical communication system (LDACS). However, the ATG communication channel suffers severely from multipath fading [
16] and the L-band suffers from congestion [
13] and did not become a suitable candidate for providing high-speed Internet connectivity for aircraft to support the three data domains required by ICAO [
2]. Also, ATG suffers from atmospheric losses and ground terrains which impacts the communication link performance and the high speed of the aircraft along with the required very large number of terrestrial transmitters indicates that frequent handovers during flight must be performed. In addition, there is a lack of connectivity in isolated regions such as wide deserts and oceans where there are no ground transmitters are available. Another solution for aircraft Internet provision uses air-to-air (A2A) connectivity through aeronautical ad hoc network (AANET) which has been proposed to provide aircraft with Internet above clouds [
19,
20,
21,
22,
23]. In AANET, the in-flight aircrafts are interconnected to spread the connectivity among them in an ad-hoc manner with enhanced capacity relative to ATG. Also, AANET may provide limited continuous connection over isolated regions where no ground transmitters are available. However, AANET suffers from many operational challenges [
21] such as continuous mobility issues, congestion, threats, and propagation and interference impairments. Therefore, there should be an efficient and feasible communication network to achieve the goal of providing aviation with high-speed broadband Internet services to improve the aircraft safety, monitoring, control and provide passengers with efficient high-speed connectivity during flight.
4. System Geometrical Modelling
In this section, the network geometry is described and analyzed. The SBs are located at height
from the ground surface (usually measured from sea level) as shown in
Figure 2. If the aircraft flies at altitude
, and the Earth’s radius is
, then the maximum range from the SB to the aircraft can be deduced as follows:
From triangle
,
or,
then,
Logically,
has a solution which includes the negative sign of the square root. Then
is finally simplified and given by:
where
is the pointing angle from the SB to the aircraft measured from the SB height
and is therefore given by:
The communication range
lies between minimum and maximum values where the minimum value is given by:
While the maximum value of
can be deduced from
Figure 2 as follows:
where
is the ground elevation angle at the airport.
and
can be deduced as follows:
or
then,
or
Similarly,
becomes:
As the aircraft is temporarily stayed at the airport during flight with onboard passengers and starts shortly for takeoff, so the minimum elevation angle can be considered less than the conventional 5° for satellite communications systems. This minimum elevation angle determines the coverage radius of the SB and the number of SBs in the network. At very low elevation angles, the slant distance between an aircraft and SB can be approximated by the sum of and which is important in discussing the atmospheric losses affecting the communication link between aircraft and SB.
5. Cellular SB-Aircraft Network
As shown in the previous section, to provide all-time flight connection, there should be a network of SBs. The size of each SB coverage area depends on the maximum communication range shown in Equation (7). For an aircraft, and before crossing this distance, there should be a standby link with another nearby SB that is ready for the handover process. One of the most important features of civil air traffic is the scheduled flights and regular aircraft paths which helps in achieving a scheduled resource management. This property gives good expectations about when and where the handover should occur between aircraft and SBs. The information about changes in scheduled flights should be provided to the system to reschedule the handover process. As shown in
Figure 3, a cellular aircraft–SB network is designed over the main traffic paths. The distance between neighbored SBs is determined according to the expected aircrafts altitudes and the maximum communication range without any loss of the line-of-sight between SB and aircraft. If two neighbouring SBs are at altitudes
and
with maximum geometrical communication ranges of
and
respectively, then, the inter-SB central distance can be given by:
Figure 4 displays the variation of the inter-SB distance with the aircraft height at different values of ground elevation angles. The value of
can be chosen as zero for regions where the aircraft is unlikely to land or takeoff such as over regions where oceans, wide deserts or forests exist, and in this case, the inter-SB distance can be extended to 1500 km for aircraft flying at 11 km cruise altitude. However, for aircraft security, control, and continued connection, it is recommended that the minimum elevation angle is greater than zero even over rural areas to achieve an acceptable quality of communication between aircraft and SB.
On the other hand, the practical value of the inter-SB distance is smaller than that given in Equation (13) to reduce the atmospheric losses resulting from the Earth’s atmospheric gases over the path between SB and aircraft. This problem arises near the end-of-coverage regions where the signal propagates through longer distances in the atmosphere. Also, the impact of weather conditions is severe during heavy rain or in the presence of taller clouds and high-humidity atmosphere which provide higher attenuation than other clear-sky regions. A detailed discussion of atmospheric losses will be presented and modelled in the next section.
For a cellular hexagonal SB-aeronautical system, a single SB has an area of coverage that can be determined by a hexagon of side length that is equal to
and the area of the aerial cell is, therefore, given by:
Figure 5 displays the variation of the SB cell coverage area in square kilometers with the aircraft height for SB located 20 km high. The area of a single SB may cover an area up to 1.5 million square kilometers for an aeronautical communication network which may extend over many countries.
6. Atmospheric Gaseous Losses Profile for Aircraft–Stratospheric Basestation (SB) Link
The communication channel between SB and aircraft is affected by three main regions according to the aircraft altitude and the elevation angle to SB.
Figure 6 demonstrates these three flight regions or stages where the atmospheric absorption in the troposphere has a considerable impact at the coverage boundary between neighbored SBs and during the climbing and descending periods, while the most efficient communication channel performance is expected when the aircraft is at full height in the cruise stage and not near the SB coverage boundary.
The atmospheric absorption increases when the signal passes in longer paths in the troposphere where atmospheric gases, clouds, rain, fog, and other factors impact the signal propagation by absorbing its energy [
25,
26,
27,
28,
29]. Fortunately, the aircraft is temporarily flying at low altitudes such as during takeoff or landing and also during overlapping regions of neighbouring SBs, therefore, it is expected that most of the time it receives high performance communication with the SB as it will be above clouds during cruise stage.
The clear sky between aircraft and SB and the much lower communication range compared to the lowest-altitude of 340 km satellite systems [
9] make a SB cellular network as an ideal solution for the provision of broadband services during flight and improves the efficiency of aircraft monitoring. Therefore, the signal loss due to atmospheric attenuation is analyzed during the complete flight duration in this section. A simple model for the flight stages is shown in
Figure 7 where the slant distance between SB and aircraft passes mainly in the troposphere and stratosphere layers. Most of the atmospheric gases and water vapor exist in the troposphere and their densities are decreased largely in the stratosphere. As a proof of concept and for investigation purposes, we may apply the simple formulas of the International Telecommunication Union (ITU) recommendations, so according to the ITU radio recommendation No.676-10 [
27], the atmospheric attenuation is due to the absorption of signal energy by atmospheric gases, mainly Oxygen and water vapor. Most of the designated frequencies for 5G services and networks are ranging from 3.5 GHz up to 66 GHz [
30]. The carrier frequencies are organized in two sets namely FR1 and FR2 where FR1 frequencies are sub 6 GHz while FR2 are above 6 GHz [
17]. In this paper, we will modify these two sets to include 3.5, 6, and 10 GHz in FR’1 while FR’2 includes 26, 28, 40, 50 and 66 GHz. At these mm-wave frequencies, the atmospheric attenuation changes drastically especially at the higher frequencies [
4]. For the aircraft–SB cellular network, the flight profile will be expected to have different attenuation levels as the signal passes through different tropospheric layers’ thicknesses. One related methodology for atmospheric attenuation calculations in the ITU recommendations in [
27] considers only the atmospheric path loss for elevated stations below 10 km altitude which is not suitable for the aircraft–SB network. Therefore, in this section, we will extend this model to calculate the atmospheric attenuation that fits the proposed system based on the numerical methodology in [
27] for slant paths. Assuming that the atmospheric slant range between an aircraft and SB can be divided into very small thickness layers where in the
nth layer, the signal has a path segment
along the aircraft–SB line of sight as shown in
Figure 7 with an incident angle
with the (
n + 1)th layer, the refraction angle of the
nth layer is
, and the new elevation angle of the (
n + 1)th layer is
. According to the layer altitude, the atmospheric parameters such as pressure and temperature change correspondingly, and hence each layer has its own refractive index which will determine the values of
,
, and
.
Therefore, for aircraft–SB communications link, the overall atmospheric attenuation,
, can be written by:
where
and
are the Oxygen and water vapor specific gaseous attenuation in dB/km respectively. The
nth layer thickness,
, can be calculated according to the following equation [
27]:
Figure 8 displays the layer thickness variation with
n along with the altitude of the segment. This figure is useful for determining the range of values for
n between the aircraft and SB as will be explained below.
If we start with
given by:
then, we can calculate the incidence and refraction angles using Snell’s Law in polar form as follows:
and,
The corresponding
nth layer path segment can be calculated using the following formula [
27]:
where
is the radial distance from the Earth’s center to the bottom boundary of the
nth layer and
is the refractive index of the
nth layer.
The layer thicknesses in Equation (16) are used to calculate the atmospheric path loss of the whole atmosphere as suggested in [
14], however, for the aircraft–SB communication link, the signal passes through specific slant range that will not span all the atmosphere and the therefore not all the steps provided in Equation (16) will be used. For example, to reach an altitude of 100 km, the value of
N should be 992, while the link stops at the SB height at approximately 20 km. Also, the starting step at which
n = 1 is used only when the aircraft is on the ground level. Denoting the starting value of
n by
at an aircraft altitude
should achieve the following equation:
For SB, it will be
, which is found by achieving the following equation:
Then, the slant path atmospheric attenuation between aircraft and SB can be calculated from the following equation:
Therefore, each segment has its corresponding specific atmospheric attenuation and length, and the overall atmospheric attenuation can be calculated using Equation (23). According to the link path between an aircraft and SB, there are two main scenarios that could be followed as discussed in the following sections.
6.1. Complete Flight Profile Scenario
In this communication scenario, an aircraft has the complete flight stages as shown in
Figure 6. From takeoff to landing in a complete flight, the aircraft passes three main stages including climbing, cruise and descending. A typical civil flight has cruise altitudes ranging from 33,000 to 40,000 ft (10–12 km) high. The climbing and descending ground distance ranges from 100 to 250 km according to the cruise height.
Figure 9 demonstrates the flight geometry model during the three phases where the ground elevation angle is
at the airport. The flight starts/ends at a distance
and the aircraft reaches the cruise height
at an elevation angle
. In the climbing/descending stage, the aircraft has an altitude
and elevation angle
. Assuming also that the climbing/descending inclination angle is
, then the ground distances measured from an airport during takeoff and climbing/descending stages are obtained as follows respectively:
and,
Also, the starting cruise elevation angle is given by:
where during cruise stage, the cruise elevation angle is given by:
The atmospheric losses will vary with the aircraft height where it is expected to have lower losses in the cruise stage while severe losses impact the communication performance during the climbing/descending periods. Fortunately, for passengers during climbing/descending periods, it is not allowed to engage in activities and they must stay fastened. The most active period of broadband services will, therefore, during cruise stage.
The flowchart shown in
Figure 10 can be followed when we calculate the atmospheric gaseous attenuation. The main factors affecting this attenuation is the aircraft altitude and the elevation angles which define the atmospheric thickness in the troposphere which affects the communication link. The impact of frequency on the atmospheric attenuation is described for each set of frequencies (i.e., FR’1 and FR’2) where there is an expected big difference in performance between the two sets. As a case study to investigate the atmospheric losses for this scenario, assume that the
which results in ground distance of approximately 508 km between the aircraft and SB. If the climbing/descending ground distance is assumed to be 200 km and the cruise height is 11 km, then the resulting flight atmospheric attenuation profile is displayed for the set of FR’1 frequencies (i.e., @ 3.5, 6, and 10 GHz) in
Figure 11a. The effect of atmospheric attenuation especially during the cruise stage is less than 0.1 dB at f = 10 GHz which is negligible compared to a maximum of 2 dB loss during the takeoff stage at the same frequency. This is because at cruise heights, the aircraft is almost above the troposphere where the air density and temperature provide very low atmospheric attenuation and the three frequency attenuation curves converge to the same values indicating almost frequency-independent atmospheric attenuation in this frequency range. At the minimum distance between aircraft and SB, where the SB is at the zenith position of the aircraft, the atmospheric attenuation is very small and can be neglected.
The atmospheric attenuation is added to the free space path loss which is given by:
where
f is the signal frequency and
c is the speed of light.
L can be expressed in dB as follows:
where
is the communication range in km and
is the carrier frequency in GHz. The path loss is displayed in
Figure 11b and the total signal loss (atmospheric plus free space path losses) is shown in
Figure 11c where the impact of path loss on the transmitted signal is dominant. Therefore, for FR’1 frequencies, the broadband aircraft–SB aeronautical network is mainly affected by the free-space path loss rather than atmospheric absorption losses.
The same demonstrations for the FR’2 higher set of mmWave frequencies are shown in
Figure 12a–c and
Figure 13 including atmospheric gaseous attenuation only, FSL, and the combined attenuation of both, respectively. As shown in
Figure 12a, the atmospheric attenuation at 26 and 28 GHz are almost of the same profile with aircraft altitude and ground distance. However, higher atmospheric losses affect greatly the other higher frequencies (i.e., above 40 GHz), especially during the climbing/descending stage, while the losses drop to very low levels at the cruise heights with converging performance indicating low dependency of atmospheric losses at this height. In
Figure 12b, the FSL variations are shown for FR’2 frequencies while the combined atmospheric attenuation and FSL is shown in
Figure 12c where the higher impact of atmospheric attenuation appears clearly during climbing/descending stages. On the other hand, at cruise levels, the FSL is the dominant attenuation factor.
As shown in
Figure 13, at the 66 GHz mmWave frequency, the atmospheric attenuation is very high and it is not feasible at all to use during the climbing/descending stage, while it does not exceed 20 dB at the cruise height.
6.2. Long Flight Handover Scenarios
As shown in the previous section, the impact of atmospheric losses is very high near ground especially at higher frequencies, while it becomes insignificant at the cruise altitudes. For long flight distances, handover should be performed between aircraft and neighbouring SBs. The inter-SB distance is determined according to the level of received signals at the aircraft. Long flights stay at the cruise level most of the time, however the spherical surface of the Earth means that, over the horizon, the line-of-sight between an aircraft and SB will be inserted into the troposphere again and is subjected to higher atmospheric attenuation. The situation becomes more complicated if the troposphere contains clouds/fog along this path which means a huge signal attenuation may occur especially at high mm-wave frequencies. This scenario is shown in
Figure 14, where the line-of-sight between an aircraft and SB at which a handover may be performed lies between two limits
and
.
A compromise between the inter-SB distance and the acceptable minimum signal level at the aircraft should be performed to reduce the number of SBs in the network while providing acceptable communication performance. The best communication performance can be achieved when the handover is performed at a cruise distance where the aircraft is at the tangential point to the circular path of altitude
, a point under which the minimum elevation angle exits on the ground. This scenario leads to denser SB network where the number of required SBs is the largest. On the other hand, the worst communication performance is obtained at a handover distance
at which the line-of-sight is almost tangential to the Earth’s surface which corresponds to paths at minimum elevation angles as shown in
Figure 14. If the line-of-sight becomes closer to the Earth surface than
, severe blocking will occur, and the link will be eventually lost. The atmospheric attenuation at distances close to
can be calculated by splitting the path between an aircraft and SB into two main segments; one from ground point “g” to the aircraft and the other from this point to the SB or:
The overall path atmospheric attenuation will be the sum of the two atmospheric attenuations exhibited in the two segments or:
This equation is expected to give a little bit overestimation for the atmospheric attenuation due to the approximation of as the sum of the two segments between ground and both aircraft and SB. However, it gives a good estimation at an elevation angle that is equal to zero where is exactly equal to the sum of and .
If the flight is spanning very long distance over areas with no airports such as wide desert or oceans, the communication slant range may be extended to its maximum allowable value in order to reduce the required number of SBs in the network provided that it does not affect seriously the communication performance especially the atmospheric losses. As shown in
Figure 15, the aircraft at the maximum line-of-sight distance, the signal will be exposed to denser atmosphere and hence more atmospheric attenuation. The atmospheric attenuation at
is approximately double the value at
due to the re-insertion of the line-of-sight into the troposphere.
The minimum atmospheric attenuation exists when the aircraft is directly underneath the SB where the atmospheric layer thickness is minimum between them. The performance of this case is shown in
Figure 15 as the minimum line-of-sight (LOS) distance performance.
Figure 15 shows a huge dynamic range of signal attenuation between an aircraft and SB especially at high frequencies for the case of maximum LOS distance between SBs. The dynamic range is very important as it defines the requirements of the receiver and transmitter circuits for proper signal reception and affects the power control and consumption of the aircraft.
Table 1 displays the signal dynamic range due to atmospheric attenuation only at the operating 5G frequencies. The performance of tangential LOS handover is acceptable even at high frequencies where the dynamic range in this case is only 2.634 dB at 50 GHz and increases to 19.454 dB at 66 GHz. However, the dynamic range of atmospheric attenuation is very small at lower frequencies where it is only 0.522 dB at 40 GHz and is negligible at 28 GHz and lower frequencies. On the other hand, a special care for applying handover at maximum LOS link distance should be performed especially at high frequencies greater than 40 GHz. The handover process is impossible at maximum LOS case for the 50 and 66 GHz where the dynamic range is very large due to the huge atmospheric attenuation which is more than 110 dB. The other lower frequencies could be used for SB networks performing handover at the maximum LOS distance.
7. Other Temporary Atmospheric Attenuation Factors
Although gaseous absorption is the most dominant impacting factor for signal transmission, other atmospheric factors provide severe signal attenuation such as rains, clouds, and fog. The occurrence of these tropospheric phenomena depends on the regional and seasonal climatic characteristics where rainy and humid regions suffer from these factors most of the year [
26]. The rain rate, signal frequency, along with the path length of the signal passing through rain all determine the rain attenuation as recommended by ITU-R P.838-3 [
28] which will be used for simple calculations in this paper, while other rain attenuation models can be also applied [
26]. For a stratospheric 5G aircraft network, frequencies below 10 GHz suffer slightly at light and moderate rain conditions as shown in
Figure 16 for an aircraft located at the airport and communicating with SB. The curves in this figure assume a worst case of 300 km length of the rainy region that the signal passes through. At 6 GHz, the very heavy rain conditions result in 4.4 dB loss while at 10 GHz it becomes as high as 21.7 dB. For frequencies above 10 GHz, the rain attenuation becomes very impacting which almost results in signal loss especially at very high frequencies. Only light rain conditions can be tolerable while other rain rates almost shadow the signal with more than 100 dB loss at frequencies above 30 GHz during very heavy rain conditions. For a network of SB with handover operation, an aircraft–SB maximum LOS passes through the troposphere and the rain path may be 500 km long. The rain attenuation performance for this case is shown in
Figure 17 where a higher attenuation occurs, especially at higher frequencies.
The other main affecting temporary factor is the fog/cloud attenuation. This attenuation is insignificant for frequencies below 10 GHz. However, as a worst case, the clouds and fog may be extended over the whole horizon from the aircraft towards SB during airport-climbing/descending phases and maximum LOS distance such as in tropical regions or over oceans near equator circle. The air temperature and the cloud water density along with the communication distance will determine the fog/cloud attenuation according to the ITU recommendations ITU-R P.840-8 [
29]. As the LOS from an aircraft to SB passes through different tropospheric layers, then the temperature profile should be inserted in the fog/cloud attenuation equation for accurate calculation.
As most cloud peaks do not increase more than 12 km, then the total fog/cloud attenuation,
, in dB can be given by:
where
is the fog/cloud specific attenuation in dB/km [
29] and
is the nth air layer length generated by Equation (20) with layer thickness
calculated from Equation (16) and the upper limit of
n is 710 calculated to achieve the total height of 12 km as follows:
The atmospheric temperature of the
nth layer used in the calculation of
can be given by:
where
is the height of the
nth layer in km and can be calculated as from the following summation:
The fog/cloud attenuation performance with frequency is shown in
Figure 18 where approximately 13 dB of minimum attenuation level occur at 10 GHz for an aircraft located at the airport and increases to approximately 32 dB for the maximum LOS case. Severe fog/cloud attenuation occurs at higher frequencies which indicate a total loss of the communication link at these frequencies. For example, at 28 GHz, the loss will be approximately 80 dB for airport communication while it increases to 200 dB for maximum LOS communication.