443.4250 KA9RIX Tampa Coordination

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This has been running as an uncoordinated repeater for some time.  It’s a multi-mode digital repeater with a remote base on it.

https://plots.fasma.org/440/443.4250_KA9RIX_Tampa_1491.kmz

443.4250|448.425|16K0F3E|6K25F7W|NULL|NULL|NULL|NULL|NULL|NULL|1|NULL|NULL|NULL|NULL|1491|1|KA9RIX|Florida Simulcast Group, Inc|Tampa|2020-01-05|2020-01-05|27.95|-82.46|140.21|BANT|NULL|200|25.000|52|104|NULL|NULL|1|https://plots.fasma.org/440/443.4250_KA9RIX_Tampa_1491.kmz|NULL|NULL|NULL|NULL|NULL|1|https://flscg.org/repeater|1|NULL|NULL|NULL|NULL|NULL|1
443.4250 KA9RIX Tampa
443.4250 KA9RIX Tampa

Updates from KA9RIX

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145.3900|144.7900|16K0F3E|NULL|141.3|141.3|NULL||NULL||0||NULL|||56|1|KA9RIX|Matthew Bush|St Petersburg|2019-03-16|2020-01-06|27.77|-82.65|45.00|BANT|GP-9|100|20.000|39|98|NULL|NULL|1|https://plots.fasma.org/144/145.3900_KA9RIX_St-Petersburg_56.kmz|0|0|0|0||0|https://arsrepeaters.com|0|0|0|N|0||0
145.3900 KA9RIX St-Petersburg
145.3900 KA9RIX St-Petersburg
147.2850|147.885|16K0F3E|9K36F7W|NULL|NULL|NULL|NULL|NULL|NULL|1|1|NULL|NULL|NULL|1493|1|KA9RIX|Matthew Bush|Madeira Beach|2020-01-06|2020-01-06|27.80|-82.80|18.00|GTOWER|GP-9|100|15.000|23|73|17|NULL|1|https://plots.fasma.org/144/147.2850_KA9RIX_Madeira-Beach_1493.kmz|NULL|NULL|NULL|NULL|NULL|NULL|https://arsrepeaters.com|NULL|NULL|NULL|NULL|0|NULL|NULL
147.2850 KA9RIX Madeira-Beach
147.2850 KA9RIX Madeira-Beach

 

444.0750|449.075|16K0F3E|6K25F7W|NULL|NULL|NULL||NULL||0||NULL|||373|1|KA9RIX|Matthew Bush|St Petersburg|2019-11-21|2020-01-06|27.77|-82.65|45.00|BANT|DB420|214|25.000|46|99|NULL|NULL|1|https://plots.fasma.org/440/444.0750_KA9RIX_St-Petersburg_373.kmz|0|0|0|0||0|https://arsrepeaters.com|0|0|0|N|0||0
444.0750 KA9RIX St-Petersburg
444.0750 KA9RIX St-Petersburg
444.7250|449.7250|16K0F3E|NULL|103.5|103.5|NULL|NULL|NULL|NULL|0|NULL|NULL|NULL|NULL|424|1|KA9RIX|Matthew Bush|Madeira Beach|2020-04-25|2020-01-05|27.80|-82.80|18.00|GTOWER|X501HD|157|25.000|27|79|NULL|NULL|1|https://plots.fasma.org/440/444.7250_KA9RIX_Madeira-Beach_424.kmz|0|0|0|0|NULL|0|https:arsrepeaters.com|0|0|0|Y|0||0

444.7250 KA9RIX Madeira-Beach

444.5000|449.5|16K0F3E|9K36F7W|NULL|NULL|NULL||NULL||1|1|NULL|NULL|NULL|406|1|KA9RIX|Matthew Bush|Madeira Beach|2019-11-21|2020-01-05|27.80|-82.80|18.00|GTOWER|GP-15|89|25.000|24|75|NULL|NULL|1|https://plots.fasma.org/440/444.5000_KA9RIX_Madeira-Beach_406.kmz|0|0|0|0||0|https://arsrepeaters.com|0|0|0|N|0||0
444.5000 KA9RIX Madeira-Beach
444.5000 KA9RIX Madeira-Beach

 

Transfer from W4FAO to KM4TTS

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Acting at the request of W4FAO he’s requested to transfer his coordination’s to KM4TTS.

145.1100|144.51|16K0F3E|NULL|123.0|123.0|NULL||NULL||0|||||1134|1|KM4TTS|Andy Rudd, KM4TTS|Madison|2020-07-06|2020-01-04|30.47|-83.42|41.45|NULL|NULL|97|20.000|35|88|NULL|NULL|1|https://plots.fasma.org/144/145.1100_KM4TTS_Madison_1134.kmz|0|0|0|0||0||0|0|0|N|0||0
145.1900|144.59|16K0F3E|NULL|123.0|123.0|NULL||NULL||0|||||1031|1|KM4TTS|Andy Rudd, KM4TTS|Lee|2020-10-02|2020-01-04|30.42|-83.30|41.45|NULL|NULL|65|20.000|26|75|NULL|NULL|1|https://plots.fasma.org/144/145.1900_KM4TTS_Lee_1031.kmz|0|0|0|0||0||0|0|0|N|0||0
442.0000|447|16K0F3E|NULL|123.0|123.0|NULL||NULL||0|||||1101|1|KM4TTS|Andy Rudd, KM4TTS|Lee|2020-12-07|2020-01-04|30.42|-83.30|41.45|NULL|NULL|62|25.000|28|70|NULL|NULL|1|https://plots.fasma.org/440/442.0000_KM4TTS_Lee_1101.kmz|0|0|0|0||0||0|0|0|Y|0||0
444.3000|449.3|16K0F3E|8K10F1E|94.8|94.8|NULL||NULL||0|||293|293|1035|1|KM4TTS|Andy Rudd, KM4TTS|Madison|2020-10-04|2020-01-04|30.48|-83.45|60.96|NULL|NULL|90|25.000|34|83|NULL|NULL|1|https://plots.fasma.org/440/444.3000_KM4TTS_Madison_1035.kmz|0|0|0|0||0||0|0|0|N|0||0

444.3000 KM4TTS Madison

442.0000 KM4TTS Lee

145.1900 KM4TTS Lee

145.1100 KM4TTS Madison

147.2100 SERA Opp, AL

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Adjacent coordination granted by SERA.

https://plots.fasma.org/144/147.2100_SERA_Opp-AL_1489.kmz

147.2100|147.8100|16K0F3E|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|1489|1|SERA|NULL|Opp-AL|NULL|2020-01-03|31.25|-86.21|30.48|NULL|NULL|89|15.000|32|97|28|NULL|1|https://plots.fasma.org/144/147.2100_SERA_Opp-AL_1489.kmz|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL
147.2100 SERA Opp, AL
147.2100 SERA Opp, AL

443.8125 W4VCO Bartow DMR Coordination Granted

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443.8125 W4VCO Bartow

This DMR repeater coordination is granted.

443.8125|448.8125|7K60FXE|NULL|NULL|NULL|1|1|1|2|0|NULL|NULL|NULL|NULL|1485|1|W4VCO|Julian A. Homan, W4VCO|Bartow|2020-01-03|2020-01-03|27.75|-81.89|126.00|LTOWER|455-5N|212|12.500|50|97|NULL|NULL|1|https://plots.fasma.org/440/443.8125_W4VCO_Bartow_1485.kmz|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|NULL|0|NULL|1
443.8125 W4VCO Bartow
443.8125 W4VCO Bartow

Modeling Repeaters in North Florida

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With the recent success of modeling all coordinated repeaters in the state, we’ve found some issues with the existing data. Issues including, coordinates being way off, powers wrong, ERP wrong and so forht. Then a major problem in northern Florida was discovered, models were ignoring the digital elevation model (DEM) when coverage was being plotted.

FASMA uses an implementation of Longely-Rice or the Irregular Terrain Model which takes into account the elevations of terrain and loss due to signals scattering and absorbed by terrain. Essentially when this data is missing it’s assumed as sea-level and the model generated is very smooth, and concentric about the transmitter. Such a model is quite far off from reality, and can over or under state the coverage (understanding is possible as we assume the antenna height above ground is now at sea level, not the actual height).

The DEM data used was provided by the Shuttle Radar Topography Mission (SRTM) which mapped the surface of the earth at resolutions not available before. The earth was scanned and elevation was averaged over 1 and 3 arc-seconds (30m and 90m). FASMA uses the 90m data as there is little gained, other than a much longer processing time, using the 30m average for non-microwave work. The USGS has several different versions of this data released, but by the most common is 2.1, which has the ability to be directly downloaded from a web-server at the USGS.

This brings us to the issue with north Florida. An example for this is the below repeater model:

NF4CQ Lake City with bad DEM data

The solid color area here indicates the model has no variation in elevation for most of it. This appears to be a rhombus shaped void centered just south of Lake City and obscuring most of North Florida. The underlying SRTM data was checked and found to possess the same void.

This discovery prompted much research into the SRTM data, and the 30m data was found to have the same issue. In the image below it can be seen of a massive gap across north Florida. Further research found this to be a product of “voids” or gaps in the SRTM radar. Typically this effects areas of deep canyons and high variation where the radar cannot see due to the angle of the shuttle to the surface of the earth. These areas of uncertainty are removed and set to negative elevation.

Black is Sea-Level, note the gap from Ocala to the State Line

USGS has newer versions of data available, known as Version 3 and includes what’s know as void fill, however it is not available for direct download. An account is required and one must point-and-click through the USGS map server interface for it. This precludes downloading automatically, as the number of 3 x 3 tiles required for US coverage is impractical to download by hand. The download is also in a different format than the HGT SRTM standard, and would need to be converted. As luck would have it, there is a web download of the SRTMv3 data as the HGT files, but it requires a user/password once registered with USGS. Using this password and some shell scripting, the entire world was able to be downloaded as SRTMv3 HGT zip files. All 14280 of them.

As the FASMA modeling program is based on SPLAT!, a conversion is required to SDF from HGT of the data. The SDF files are much larger with the entire wold of SDF files taking ~77 GiBytes of space. SPLAT! does support bzip2 compressed SDF, and a multi-threaded version of bzip2, pbzip2 was uses to compress the files in short order on a 24 core server. This compressed down to a more reasonable 10 GB.

After remodeling a number of repeaters in North Florida, it was found some tiles of DEM data looked to be corrupted, with some areas below sea-level and others with “noise” data in them. Comparisons were made with the source SRTM files and found to be perfect. Data looked good and gdal_translate was used to make PNG’s of the terrain, confirming the SRTMv3 was not the source of the issue.

  • Tile issue with some corruption in this tile at N30W82
  • W9CR St Pete repeater with bunk data

 

After much trial and error to locate the bug, it was discovered uncompressed SDF files worked fine. Further when compressed again with bzip2, the resulting sdf.bz2 file rendered as expected. This was quickly confirmed as the library in SPLAT! not being able to decompress files compressed with pbzip2 perfectly. A script was made to unbzip and then bzip2 all sdf files in place. The results below show it was a simple fix. The ultimate issue will be submitted as a bug report.

  • JAX repeater with proper DEM
  • St Pete Repeater fixed

The Lake City 444.9000 NF4CQ revised plots using the SRTMv3 models are below. Note due to the void “fill” it’s not a perfect and we have some discrepancies in the elevation corrections and the valid SRTM data. This is not perfect but it’s much better than assuming sea-level, especially for elevations in North Florida where 30-40m ASL is normal.

  • Combined
  • Interference Plot
  • Service Plot

References:

 

http://srtm.fasma.org/ – FASMA has made it’s collection of SRTMv3 HGT and SDF data for the wold available for direct download.

https://e4ftl01.cr.usgs.gov/MEASURES/SRTMGL3S.003/2000.02.11/ – USGS SRTMv3 source, password required.

Coordinated Repeater Models

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Recently we’ve completed the modeling of all coordinated repeaters in Florida. This was scripted and database driven modeling. Right now the individual KMZ files are available at https://plots.fasma.org under the various bands. Each KMZ file has the service, interference and point of repeater, along with channel size and modulation type.

Most repeater owners/operators/trustees will look at the service contour which is in blue. This shows an area where at 1.83m (6′) above the ground, there is a 50% chance that location will have a signal, 50% of the time greater or equal to the service contour. This is typically the mobile service area of a repeater and designated (50, 50).

The green interference contour is modeled to show 50% of locations 10% of the time (50,10) where a signal will be 18 dB below the service contour. This de-rating to 10% makes the chances of receiving a signal much smaller and thus the interference contour is larger. No other co-channel users interference contour should overlap the service contour of any other repeater. This ensures a repeater in it’s protected service contour has a signal at least 18 dB greater than any co-channel repeaters.

In some cases there are adjacent contours, and these are used much like the interference contour. No adjacent contour should overlap another service contour. These are used on 144-146 and 146-148 MHz and for narrowband in 222-225 MHz.

The eventual goal is to have this database driven in real time. This is being worked on and we hope to have a much better interface shortly.

Comparison of Radio Propagation Modeling Software

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Recently discussions regarding the use of various software in the study of coordination modeling have happened.  All claim to implement the same models along with their own variations or empirical derived models.  The model we are most interested in is known as Longley–Rice, or the irregular terrain model (ITM).  This model is optimized to cover 20 to 20,000 MHz for predicting signal strength over real terrain when used with a digital elevation model (DEM).

The ITM model in area propagation mode essentially breaks up the underlying map into tiles of a given resolution, and taking account the DEM heights, computes the signal level in a tile and then onto the adjacent tiles and so on using the now attenuated signals from the source area.  The original code was written in FORTRAN, converted to C++ and has been re-implemented a number of times to speed it up, improve it and add a given vendors “secret sauce”.  The original docs and code may be found on the ITS website.  Keeping in mind the ITM model was used to layout FM and most importantly the VHF/UHF Television spectrum in the 1960’s it’s proven to be a reliable model.  Land Mobile radio has adopted the same basic concepts in needing to predict interference between co and adjacent channel users, albeit with different criteria than TV broadcasters.

As amateurs push to coordinate frequency use in their spectrum, it’s imperative we understand our tools and what software we may use to predict coverage.  This is more important we have repeatable standards which anyone can model and check to keep our coordination bodies honest as well.  FASMA has standardized on SignalServer which is a multithreaded version of SPLAT!, both implement the C++ version of the ITM model.  Also common in amateur circles is the use of RadioMobile, a non-free application for windows operating systems.

Commercially there are many packages used for radio modeling, and two of the most popular are ComStudy and Pathloss.  ComStudy is the de-facto standard used by the LMR coordinators approved by the FCC and implements it’s own proprietary version of the ITM model and ships with an additional land cover database.  Pathloss 5 is mostly known in the Part 101 and microwave Point to Point (PtP) modeling space, but has an ITM mode, and unlike most software, describes the algorithm implemented in great detail.  As Pathloss doesn’t provide source code, we cannot be sure how faithfully they have implemented the ITM model.

The DEM model data used is the 3 arc second resolution data from the Shuttle Radar Topography Mission (SRTM).  This is a digital model of the earth’s elevation in 90×90 meter tiles as a height.  This works well for most areas, but there is higher resolution data 1 arc second and even 1/3rd arc-second available for certain areas of the earth.  Ultra-high resolution DEM data has national defense implications, and is generally not available.  The SRTM data typically includes the tops of trees in forests, which can present a problem if a tower is in a forest.  We can say the height above ground is 100 meters, but if the adjacent trees are 20 meters average height, the model AGL should adjusted to 80m (100-20 tree height), or we will be modeling the system 20m too high.  This same phenomena can present in dense cities as an urban forest area.

 

Modeling Criteria

In comparison we have modeled a test repeater with an omni directional antenna as follows:
<font=monospace>

Latitude:        42.33
Longitude:      -87.91
Frequency:      446 MHz
Antenna Height Above Ground: 97.5 meters
ERP:            707 watts
Signal Criteria: 39 dBuV/m (dBu)
Reliability and confidence criteria - (50, 50)

Signal Server

SignalServer was invoked with the following command:

./signal-server-base.sh -lat 42.328889 -lon -87.912500 -txh 97.54 -f 445 -erp 707 -rt 39 -conf 50 -o blueblue | ./genkmz.sh

This produced the plot below with a radius (based over the water) of 62km.

The reason for basing the plot over the water for radius is it should be the same height and signal strength in all models, as there is nothing there.

This plot took about 150 seconds on a quad core computer.

The Keyhole Markup Language file is here, and a version of the same plot, but red is here.  The red color version is useful for comparing and contrasting with the other results in the various shades of blue.

RadioMobile

RadioMobile is interesting as its non-Free Software, but doesn’t appear to have a commercial use keeping it from being Free Software.  Due to the GUI, it’s popular with a number of amateurs.  The configuration for generating plots is quit complex and poorly documented to get a 1:1 ITM model from it.  RadioMobile is not multi-threaded, in fact the entire GUI locks up while rendering, however a render is completed on a Dell D830 (a laptop circa 2006) in about 60 seconds.  From this we must assume some “speedups” or shortcuts in the code are taken when compared to the ITM reference code.

We followed the FASMA reference guide on modeling in RadioMobile for this plot.

This modeled with an 82km radius over water, and seemed to have greatly overstated coverage compared to the other models.

 

Pathloss 5.1

Pathloss has no easy way to export the configuration for a model.  We had this modeled by a trained professional user of the software.  Pathloss in area mode is exceptional slow, there below took about 12 hours to render.  We found no multi-threading taking place, and like RadioMobile the GUI locked up during this. Based on this, we can assume the code very close to the ITM reference.

The radius here was 65km and compared very closely with the SignalServer model.

The Keyhole Markup file of this is here.

ComStudy 2.2

ComStudy was run by an experienced engineer who has worked LMR across the VHF and UHF business spectrum.  Again there is no easy open way to export the study inputs for ComStudy, but the below files were modeled.  We didn’t have exact measurements of time for the generation of the below plots.

This is a 42km radius and has the smallest area of any model we studied.  The Keyhole Markup file is here.

In ComStudy it also has proprietary land-cover databases which ship with it.  Much like a DEM file, this identifies the type of cover in a given area, which changes the radio propagation characteristics of that area.  We have a model with the LCF enabled and it’s much smaller as well.

Comparisons

SignalServer with PL5

This was the closest comparison, and based on the PathLoss docs, we believe PathLoss has implemented a truthful version ITM algorithm.  This would confirm the SignalServer/SPLAT! model as being correct as well, and we belive this confirms it is the case.

In the below, SignalServer is in red and the PathLoss model is in blue.

The slight variation over water (3km) and the open arc in the PathLoss model would indicate it has two ray turned on by default.  This only comes into effect over large flat reflective areas such as water.  Over land the models align 99%.

Looking at the fringe coverage we see the same tiles, just slightly offset.  This may be due to the datum used internally in PathLoss not being corrected to the WGS84 datum of our coordinates.  This would further confirm the agreement both SignalServer and PathLoss have a true ITM model implementation.

SignalServer with ComStudy

ComStudy claims to implement the same ITM model, however it doesn’t appear to be the same.  We’re not certain why this is, perhaps it’s due to some of the speedup code or just a general desire to mix the ITM with an empirical model as they can call it the ComStudy model.  ComStudy also may take into account the LCF data for land cover and we have presented that below as well.

ComStudy with a 42km vs 62km radius in SignalServer.  ComStudy is the lighter blue color.

We’re not certain why it’s different, but at least in the areas that are covered ComStudy and SignalServer seem to align; looking to the north west above McHenry on the map we can see gaps between the airports and they align in both models.  This may be due to the ComStudy using a different height, correcting for antenna gain, or another issue.  What we do see is that the models do appear to use the same DEM data to determining a valley or non-coverage area.

Zoomed area showing the alignment between areas in ComStudy and SignalServer.

This is the overlay of the ComStudy on Signal Server with the land cover data.  We can see this LCF data has impacted coverage to the north and south over land.  This does give some value to the theory ComStudy may be adjusting the DEM data for forested regions as suspect in the other non-LCF model, and explain some of the descripency between it and SingalServer/Pathloss.

RadioMobile vs. SignalServer

Perhaps in the most interesting study, we found RadioMobile to vastly overstate coverage compared to the other three programs.  This may be due to the primary user base of amateurs who are wowed by the enhanced coverage predictions, thus it encourages many users.  It may also be the “speed ups” done to allow RadioMobile to so fast.  Indeed RadioMobile was the fastest to produce a model of any of the programs tested.

In the above we can see the overstated RadioMobile plot in blue and the SignalServer plot in red.

Here we can see the light blue of the ComStudy in the center, red of SignalServer and then the blue of RadioMobile.

We’re not certian why this is with RadioMobile, but have found ~15 dB of reduction of ERP will bring the model to align more with SignalServer and Pathloss.  This was not tested in other areas and we caution anyone using RadioMobile (or any non-Free Software) to not trust the results.  We cannot recommend using RadioMobile for any real modeling of amateur repeaters due to these issues.

 

Conclusions

The intent of this research was to compare and validate SignalServer’s ITM model with other popular radio propagation software models.  We found a great agreement between SignalServer and Pathloss, confirming a faithful implementation of the ITM model.  ComStudy was shown to be slightly less generous with coverage, but where the models did overlap, we found they agreed.

RadioMobile was the outlier, and was found to be greatly overstating a coverage area, and no alignment with even common areas of coverage in SignalServer.  Based on this the author cannot suggest the use of RadioMobile.

 

References

SignalServer 39 dBu model Keyhole Markup File
Signal Server 39dBu red KMZ 
ComStudy 2.2 with no landcover
Pathloss 5.0 Study
RadioMobile
ComStudy 2.2 with landcover

SRTM mission overview on wikipedia
Shuttle Radar Topography Mission on the JPL homepage

ITM Model homepage on the Institute for Telecommunications Sciences

FASMA Library

SignalServer – Github fork by N9OZB
SPLAT! – Homepage
RadioMobile – Homepage
ComStudy – Homepage
Pathloss – Homepage