Insights
Interference January 2025 9 min read

The Interference Event That Came From 100 Miles Away

Atmospheric conditions can carry CBRS 3.5 GHz signals far beyond their intended range. When that energy arrives at your network, it presents as sector degradation with no identifiable local source. This happens more than most operators realize. The diagnostic path that finds it is different from every other interference scenario.

The event that does not fit any local explanation

The call pattern looks like this: multiple subscribers on the same sector report degraded speeds. SINR is down across the board. RSSI is unchanged. You pull a spectrum scan and see elevated noise on your operating channel. You check for new local operators in your coverage area. Nothing shows up. The interference appears intermittently, worse in the evening, sometimes absent in the morning. No hardware faults. No new construction nearby. The degradation comes and goes on its own schedule over three to seven days and then largely disappears.

This is a tropospheric ducting event. The interference source is not in your market. It is not in the adjacent market. It may be operating 80 to 150 miles away, and under the right atmospheric conditions its signal is arriving at your sector with enough power to materially degrade your SINR floor.

The Core Pattern
Tropospheric ducting at 3.5 GHz can carry CBRS signals 100+ miles beyond their intended service area. The interference presents as sector-wide SINR degradation with no identifiable local source, appears intermittently, and resolves on its own. Most operators who experience it diagnose it as equipment failure or a SAS anomaly. It is neither.

What tropospheric ducting is

Under normal atmospheric conditions, radio signals at 3.5 GHz propagate along a relatively predictable path. The atmosphere bends and absorbs signals in ways that are well-modeled and well-understood. Normal propagation follows the standard free-space path loss curves that link budget calculations are built around.

Tropospheric ducting occurs when temperature inversions in the lower troposphere, typically 0 to 2 km altitude, creating a layer where the refractive index of the atmosphere changes sharply with altitude. This layer acts as a waveguide, trapping radio signals and allowing them to propagate far beyond their normal range with dramatically less attenuation than free-space path loss would predict.

At 3.5 GHz, ducting events are most common in coastal and near-coastal regions during late spring, summer, and early fall, particularly in the evening hours when temperature inversions are strongest. Inland regions experience ducting less frequently but are not immune, particularly during stable high-pressure periods.

The signals that duct are not weak. A CBRS CBSD operating at full Category B power (47 dBm EIRP) that normally produces -85 dBm at 10 km can arrive at 100 km during a strong ducting event at power levels that are competitive with your own signal at the subscriber's CPE. When that happens to a subscriber sitting on the edge of your sector's coverage footprint, the arriving interference may be only 6 to 10 dB below your signal, enough to collapse the SINR from acceptable to marginal or below.

Why it is difficult to diagnose

Every other interference scenario in CBRS has an identifiable local cause. A new co-channel operator. A CPE in an overlap zone. A SAS registration error producing unexpected frequency assignments. You can identify each of these by looking at what changed in your immediate operating environment.

Tropospheric ducting has no local cause. The interfering signal is coming from a CBSD that is operating legitimately in its own market, causing no problems there, and accidentally degrading your network as a byproduct of atmospheric physics. There is no regulatory mechanism that prevents this. The SAS does not manage inter-market interference at these propagation distances because under normal conditions no inter-market interference exists.

The interference is intermittent. Ducting events last hours to days and then dissipate. The interference appears, degrades your network, and disappears without any local action being taken. This pattern leads operators to suspect intermittent hardware faults or software anomalies.
The interference is sector-wide but uneven. CPEs at the edge of your sector's coverage footprint, where your signal is weakest relative to the arriving ducted signal, are most affected. CPEs closer to the RN with strong SINR margins may show no degradation at all. This geographic pattern looks like coverage shrinkage, which leads to incorrect antenna diagnostics.
The spectrum shows elevated noise on your operating channel from a direction that has no local CBSD. If you have directional spectrum monitoring capability, the noise source will be arriving from outside your normal coverage footprint. Most operators do not have directional spectrum scanning at the RN level, so this observation is not available.
The timing correlates with weather patterns, not with subscriber activity or operational changes. Strong high-pressure systems, coastal fog, and calm, clear evenings are the atmospheric conditions that produce ducting. If you track the timing of your interference events against weather records and find a consistent correlation, you have likely identified the mechanism.

Coastal operators and elevated exposure

Operators in coastal and near-coastal markets should treat tropospheric ducting as a baseline operational risk, not an edge case. The combination of marine layer temperature inversions, coastal geography that concentrates ducting channels along the coastline, and the high density of CBRS deployments in coastal metropolitan areas creates conditions where ducting events occur multiple times per year in some markets.

Operators within 50 miles of a major coastline operating on GAA spectrum channels with no PAL protection should consider this risk when evaluating their frequency planning strategy. A ducting event affecting a GAA-only operation has no regulatory remedy. The interfering signal is arriving legally, from a legal source, and neither the SAS nor any regulatory process provides rapid relief.

PAL Consideration
PAL licenses do not prevent ducted interference from arriving at your CPEs. They do, however, give you a regulatory basis for documenting the interference and potentially coordinating with the SAS on channel assignment adjustments during sustained events. A GAA-only operator has no such mechanism. If your business model depends on consistent coverage in a coastal market, this is one more reason PAL is not optional.

How to identify a ducting event in your network

The diagnostic process for a suspected ducting event is different from standard interference investigation. You are not looking for a local source. You are correlating your network behavior with atmospheric conditions.

01
Pull sector SINR history against a timeline. Identify the exact start and end of the degradation event. Note whether it began gradually or abruptly. Ducting events typically begin gradually as the inversion layer forms and end more abruptly as it dissipates.
02
Check subscriber impact geography. Map which subscribers were affected. If the affected subscribers are disproportionately at the edge of your sector's footprint, further from the RN, at your coverage boundary. The pattern is consistent with an external interference source arriving at lower power than your own signal. Edge subscribers have less SINR margin to absorb it.
03
Pull weather records for the event period. Check surface temperature inversions, barometric pressure trend, coastal fog reports if applicable, and overnight temperature differential. Strong surface inversions (warm air layer over cooler surface layer) are the primary ducting mechanism. A consistent correlation between weather patterns and your interference events over multiple occurrences is strong evidence of ducting.
04
Check CBRS SAS records for your channel during the event. If the SAS shows no new grants or changes in your operating area that coincide with the interference event, a local source is unlikely. The absence of a local explanation in the SAS data supports the ducting hypothesis.
05
Consider a channel change during sustained events. If ducting events are occurring regularly on your operating channel, and if you have channel flexibility through GAA or PAL on alternative frequencies, a temporary channel shift during identified events may reduce the impact. Ducting propagation is frequency-direct. The same conditions that duct on one channel may not produce equivalent results on an adjacent channel.

What you can and cannot control

The honest assessment of tropospheric ducting interference is that the atmospheric mechanism is not controllable. You cannot prevent a temperature inversion from forming over the ocean. You cannot prevent a distant CBSD from operating on your channel. You cannot file an interference complaint against a source that is operating legally and causing harm as a byproduct of atmospheric conditions that neither you nor they created.

What you can control is your network's resilience to it:

SINR margins at edge-of-sector subscribers. The deeper your SINR margin at your coverage boundary, the more external interference those subscribers can absorb before their link quality degrades below acceptable threshold. Tier 3 subscribers are the first to fail during a ducting event. Operators who maintain a high serviceability standard and minimize Tier 3 approvals have more resilient networks during atmospheric events.
PAL spectrum where ducting risk is elevated. A PAL-licensed operator has a regulatory basis for interference documentation and coordination. This does not prevent the event but provides a mechanism for escalation if events become sustained or frequent.
Subscriber communication during identified events. If you have identified tropospheric ducting as a recurring pattern in your market, having a prepared communication for affected subscribers during events is the difference between a documented atmospheric anomaly and an unexplained service failure. Subscribers who understand what is happening, and why, churn at lower rates than subscribers who experience repeated degradation with no explanation.
Conditional approval documentation for coastal edge subscribers. Subscribers at the edge of coverage in ducting-prone markets should have their Tier 3 conditional approval documentation explicitly note the elevated atmospheric interference risk and set expectations accordingly. An operator who documented the risk at install has a defensible position when a ducting event produces a service complaint. An operator who approved the install without documentation does not.

The pattern recognition that matters

Most operators who experience a ducting event do not identify it as such. They experience a period of degraded performance, dispatch field resources that find nothing wrong at the CPE level, watch the interference resolve on its own, and file it as an unexplained anomaly. If it happens again, they repeat the process.

The operators who identify ducting as a pattern are the ones who track their interference events against atmospheric conditions over multiple occurrences. This takes no additional technology. It requires correlating your NMS data against publicly available weather records after the fact. Three correlated events is enough to establish the pattern with confidence.

Once the pattern is identified, the network management response changes. Unnecessary truck rolls during identified events are avoided. Subscriber communication is prepared and deployed. Channel strategy during events is pre-planned. The interference still arrives. The operational response to it costs less and produces better subscriber outcomes.

STANDARD CONTEXT
This pattern is formalized inside the NGWA Standards framework and used as a reference for real-world deployment decisions.

See how it connects to deployment rules and design decisions.
View Standard Section

The full interference framework is in the Standards

CBRS spectrum strategy, GAA vs PAL analysis, interference identification, and the failure pattern documentation for co-channel and adjacent-operator scenarios are in the NGWA Standards.

Ducting Risk Indicators
When to suspect a ducting event
Sector-wide SINR drop, RSSI unchanged
Edge subscribers affected, inner zone unaffected
No local source identifiable in SAS data
Worse in evenings, correlates with stable high pressure
Resolves in 1-7 days without local intervention