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About PlaneWX

Multi-Model Icing Analysis

PlaneWX goes far beyond traditional AIRMETs and PIREPs. We analyze icing conditions using three independent weather models, the FAA/NWS Current Icing Product (CIP) observation-fused nowcast, and the next-generation DAFS Icing Forecast Integration (IFI) for flights up to 18 hours out — giving you aviation-specific icing forecasts, confidence levels, cloud layer boundaries, SLD risk, and total exposure estimates, all tailored to your route and altitude.

Why Multi-Model Icing Matters

Traditional icing information comes from two sources: G-AIRMETs (broad geographic areas with blanket severity ratings) and PIREPs (sporadic pilot reports that may be hours old). Both have significant limitations:

G-AIRMETs: Too Broad

  • • Cover hundreds of thousands of square miles
  • • Single severity for the entire area
  • • No information about specific altitudes within the range
  • • Don't tell you where the clouds actually are
  • • Updated every 3 hours — conditions change faster

PIREPs: Too Sparse

  • • Depend on other pilots filing reports
  • • Subjective severity assessments
  • • Represent a single point in space and time
  • • Often hours old by the time you see them
  • • Huge gaps in coverage, especially at night and in rural areas

PlaneWX's approach: Instead of relying solely on these broad products, we query three independent numerical weather models at multiple points along your specific route — and for CONUS flights within 18 hours of departure, we layer in the FAA's own aviation icing products (CIP nowcast and DAFS IFI forecast) for purpose-built, observation-informed icing guidance. Each source covers the time window where it performs best.

The Icing Models

PlaneWX queries multiple weather models independently and compares their output for confidence scoring — something no single model can provide alone. The exact model mix depends on where you're flying: US domestic routes use three models; European routes add two high-resolution regional models for significantly sharper analysis.

HRRR

High-Resolution Rapid Refresh

NOAA's highest-resolution hourly model — the gold standard for short-range icing forecasts.

Resolution

3 km

Updates

Every hour

Range

0–18 hours

Best for

Cloud layers, convection, terrain effects

HRRR's 3-km grid captures terrain-induced effects that coarser models miss — critical for mountain flying where icing conditions can vary dramatically over short distances.

GFS

Global Forecast System

NOAA's primary global model — the backbone of most weather predictions.

Resolution

~13 km

Updates

4 times daily

Range

0–16 days

Best for

Big-picture trends, extended-range icing outlook

GFS provides the longest forecast range. When HRRR data expires (beyond 18h), GFS and ECMWF continue to provide icing guidance — critical for PlaneWX's mission of long-range trip planning.

ECMWF

European Centre for Medium-Range Weather Forecasts

Widely regarded as the world's most accurate global forecast model.

Resolution

~9 km

Updates

4 times daily

Range

0–10 days

Best for

Overall accuracy, moisture fields, jet stream patterns

ECMWF's IFS model consistently outperforms other global models in verification studies. Its independent European perspective on atmospheric conditions strengthens consensus scoring alongside the two NOAA models.

Why Multiple Models?

No single model is always right. By comparing independent models, PlaneWX determines how much to trust the forecast. When all models agree, confidence is HIGH. When they disagree, confidence drops — and that disagreement itself is valuable information. It tells you the atmosphere is uncertain and conditions could go either way.

European Routes: ICON EU + ICON D2

For routes involving European airports, PlaneWX adds two high-resolution regional models operated by Germany's national weather service (DWD). These run alongside GFS and ECMWF to give European pilots significantly sharper icing analysis — especially over the Alps, coastal UK, Scandinavia, and complex terrain.

ICON EU

DWD ICON EU

DWD's regional European model — sharp terrain resolution.

Resolution

~7 km

Updates

4× daily

Range

0–5 days

Coverage

Europe + N. Africa

ICON D2

DWD ICON D2

Ultra-high-resolution nest covering central Europe.

Resolution

~2 km

Updates

8× daily

Range

0–48 hours

Coverage

Germany + neighbors

ICON D2's 2-km grid captures orographic effects — Alpine lenticulars, Föhn, valley fog — that 7–13 km models often miss. When available, ICON D2 is the highest-resolution source in the PlaneWX icing model suite.

CIP/IFI Hybrid — Aviation Icing Data from Now Through 18 Hours

NWP forecast models are excellent for planning flights days in advance, but for the critical 0–18 hour window PlaneWX uses two aviation-specific icing data sources that run parallel to the NWP consensus: the Current Icing Product (CIP) — an observation-fused nowcast for imminent departures — and the DAFS Icing Forecast Integration (IFI) — the FAA's next-generation icing forecast covering flights departing 4–18 hours from now. Together they replace generic model icing estimates with purpose-built aviation data across the entire day-of-flight window.

The product family: CIP, FIP, and IFI

The FAA and NOAA have run two parallel icing products for over 20 years. Understanding the lineage explains why PlaneWX uses what it uses — and why it matters for your flight planning:

CIP

Current Icing Product — the nowcast. Answers "what does icing look like right now?" by fusing PIREPs, radar, satellite, and surface observations. It is not a forecast and has no predictive validity beyond 1–2 hours. Using CIP for a flight 8 hours away is like checking today's radar for tomorrow's weather.

FIP

Forecast Icing Product — the legacy forecast. CIP's companion product, using the same algorithm framework but applied to NWP model output to predict future icing conditions. FIP is what products like ForeFlight and EZWxBrief have historically used for future flights. It runs on a 13-km grid.

IFI

DAFS Icing Forecast Integration — the next-generation FIP. Launched operationally by NOAA in March 2026, IFI replaces FIP with a major upgrade: 3-km resolution (vs. 13-km), 60 altitude levels (vs. 30), HRRR as the model background (vs. the older RAP), and radar data ingested every 15 minutes. Same concept as FIP — purpose-built aviation icing forecast — but substantially sharper.

PlaneWX uses CIP for the 0–2 hour window (where observation fusion beats any forecast) and DAFS IFI for the 4–18 hour window (where you need a forecast, not a snapshot). This mirrors how the FAA's own systems are designed to be used together.

CIP

Current Icing Product (CIP) — FAA / NWS Aviation Weather Center

Observation-fused icing nowcast. Updated hourly. CONUS coverage.

What it fuses
  • • PIREPs (icing pilot reports)
  • • METARs (surface observations)
  • • Satellite multi-spectral imagery
  • • Radar reflectivity
  • • NWP model background fields
Output fields
  • • Icing severity (none → severe)
  • • Icing probability (0–100%)
  • • SLD potential (0–100%)
  • • 30 altitude levels, 1,000–30,000 ft
  • • 13.5 km horizontal resolution
Coverage
  • • CONUS (contiguous U.S.) only
  • • Updated every hour at :10–:15
  • • Data typically 10–45 min old when used
  • • Non-CONUS routes: NWP model drives icing
IFI

DAFS Icing Forecast Integration (IFI) — FAA / NCEP Aviation Weather Center

Aviation-specific icing forecast. Updated hourly. 18-hour forecast horizon. CONUS coverage.

What it provides
  • • Icing probability (0–1 scale)
  • • SLD potential (0–1 scale)
  • • Icing severity index
  • • 60 altitude levels, 1,000–30,000 ft
  • • 3 km horizontal resolution
Forecast hours
  • • f001, f002, f003, f006, f009, f012, f018
  • • Published every hour at :30
  • • From the NCEP DAFS system (successor to CIP/FIP)
  • • Data typically 30–60 min old when used
Coverage
  • • CONUS (contiguous U.S.) only
  • • Covers 4–18 hours ahead of departure
  • • Same grid as CIP — direct comparison possible
  • • Non-CONUS routes: NWP consensus drives icing

DAFS IFI is the next-generation replacement for the legacy FIP (Forecast Icing Product). At 3-km resolution, it captures orographic and mesoscale icing structures that NWP models at 9–13 km resolution commonly miss — the same structures that have historically caused serious incidents when pilots relied solely on NWP icing guidance. NOAA announcement ↗

How PlaneWX Blends CIP, IFI, and NWP

CIP is a nowcast — it captures the current state of icing, not a forecast. IFI provides aviation-specific icing forecasts up to 18 hours ahead. PlaneWX uses a time-based selection model that puts the best available data source in charge for each waypoint:

0–2 hours

CIP drives the icing assessment. Observation-fused data is more reliable than any forecast for imminent conditions.

CIP Zone
2–4 hours

Conservative blend: PlaneWX reports the worse of CIP and IFI for each waypoint. When sources disagree, we err on the side of caution.

CIP/IFI Blend Zone
4–18 hours

DAFS IFI drives the assessment. Purpose-built aviation icing forecast at 3-km resolution. Replaces generic NWP icing estimates for the most important planning window.

IFI Forecast Zone
Beyond 18 hours

NWP consensus models drive the assessment. IFI's forecast horizon ends at 18 hours; global models (GFS, ECMWF, HRRR) continue providing guidance beyond that.

NWP Zone

Why DAFS IFI? NOAA began operational deployment of DAFS in late March 2026, describing it as the culmination of over 25 years of FAA/NOAA partnership on aviation icing research. The system is built on the HRRR model's 3-km grid and ingests radar data every 15 minutes — giving PlaneWX access to the same icing intelligence used by Air Route Traffic Control Centers nationwide. Read the NOAA announcement ↗

Supercooled Large Droplets (SLD)

CIP includes a dedicated SLD potential field — a probability estimate for Supercooled Large Droplets. DAFS IFI also provides an SLD potential field with the same structure. SLD is particularly dangerous because it can cause rapid ice accretion on unprotected surfaces and even penetrate behind protected leading edges. PlaneWX detects SLD risk using phase-specific thresholds: ≥10% probability during climb or descent, and ≥20% at cruise.

When SLD is detected, it directly impacts your WX Score — not just as a display warning. No GA aircraft is certified for SLD conditions (14 CFR Part 25, Appendix O). FIKI covers Appendix C icing only; SLD accretes aft of all protected surfaces regardless of equipment. The scoring reflects this:

  • 10–19% SLD: −10 pt caution
  • 20–29% SLD: −20 pt caution
  • 30–39% SLD: −30 pt caution (pushes score to marginal)
  • ≥40% SLD: NO-GO — CIP has high confidence SLD is present

FIKI does not mitigate SLD. Unlike general icing, FIKI provides zero protection against supercooled large droplets — de-ice boots, heated leading edges, and TKS panels all protect surfaces that SLD bypasses. SLD scoring is identical for FIKI and non-FIKI aircraft. (FAA AC 91-74B)

Reading the Icing Route Bar

When CIP or IFI is active, a per-waypoint Route Icing — CIP/IFI Hybrid bar appears below the phase grid. Each segment shows the hybrid in-cloud icing severity for that waypoint, colored by the data source that drove it:

  • Bright cyan segments — driven by CIP nowcast (0–2 hours)
  • Amber segments — driven by CIP/IFI blend (2–4 hours)
  • Indigo/blue segments — driven by DAFS IFI forecast (4–18 hours)
  • Dimmed segments — driven by NWP consensus (beyond 18 hours)
  • Color intensity — green = none/trace, blue = light, amber = moderate, red = severe
  • SLD badge — appears when CIP or IFI detects SLD probability ≥10% in climb/descent or ≥20% at cruise; at ≥40% this triggers a NO-GO
  • Hover tooltips — card-style popups showing exact severity, data source (CIP / IFI forecast / CIP/IFI blend / NWP), temporal zone, icing probability, and SLD probability for each segment

FZRA Risk Strip: When a warm nose inversion is detected during descent, a thin amber strip labeled "FZRA risk" appears below the descent portion of the bar. This indicates freezing rain risk — a phenomenon that occurs below the cloud base and is not captured by CIP (which only detects in-cloud structural icing). Hover the strip for a full explanation. The descent phase tile will separately show the severity for this freezing rain risk.

Probability filter: When CIP or IFI reports icing probability below 10% at a waypoint, PlaneWX suppresses that CIP/IFI severity and falls back to NWP — preventing rare false-alarm severe readings from driving the bar when observational confidence is very low.

How We Detect Icing

Icing requires two ingredients simultaneously: subfreezing temperatures and visible moisture (clouds). PlaneWX checks both at each altitude level along your route.

Temperature Check

PlaneWX detects icing across two zones: a primary zone (0°C to -20°C) where ~90% of structural icing occurs, and an extended zone (-20°C to -40°C) where supercooled water can persist in convective updrafts and orographic lift. Below -40°C, homogeneous nucleation ensures all water is frozen — liquid water cannot exist.

0°C to -10°C: Maximum icing risk — supercooled water droplets most common (clear ice zone)

-10°C to -20°C: Decreasing risk — mixed phase, smaller droplets (rime ice zone)

-20°C to -40°C: Extended range — supercooled water rare but possible in vigorous convection. Probability attenuates linearly toward -40°C

Below -40°C: No icing — homogeneous nucleation, liquid water cannot exist

Moisture Check

Relative humidity ≥ 70% at a pressure level indicates proximity to cloud or visible moisture. Higher RH means denser moisture and higher icing probability.

RH ≥ 90%: Almost certainly in cloud — highest icing probability

RH 80–89%: Likely in cloud — moderate-to-light icing probability

RH 70–79%: Near cloud threshold — trace icing probability (primary zone only)

RH < 70%: Dry air — no icing at this level

Icing Probability Formula

At each altitude level, PlaneWX calculates an icing probability from 0–100% based on:

  1. Is the temperature between 0°C and -40°C? If not, probability is 0% regardless of moisture.
  2. Is relative humidity ≥ 70%? If not, probability is 0% — insufficient moisture for icing.
  3. Primary zone (0°C to -20°C): RH ≥ 90% with temp above -10°C yields moderate severity (80–90% prob). Lower RH and colder temps scale down through light and trace.
  4. Extended zone (-20°C to -40°C): Only RH ≥ 80% triggers icing detection. Probability attenuates linearly with temperature — approaching zero at -40°C. Max severity is trace.

Severity Levels

PlaneWX converts the calculated icing probability into FAA-standard severity levels. These are the same severity terms used in AIRMETs, PIREPs, and aviation forecasts.

0–19%

NONE

No icing expected. Temperature and/or moisture conditions don't support ice accumulation.

20–39%

TRACE

Ice becomes perceptible. Rate of accumulation slightly greater than the rate of sublimation. Not hazardous unless encountered for more than an hour.

40–69%

LIGHT

Rate of accumulation may create a problem if flight continues for more than an hour. Occasional use of de-icing/anti-icing equipment removes or prevents accumulation. Non-FIKI aircraft should exit these conditions.

70–89%

MODERATE

Rate of accumulation requires frequent cycling of de-icing equipment or diversion. Even FIKI-equipped aircraft should have an exit strategy. Significant impact on aircraft performance — increased drag, reduced lift, higher stall speed.

90–100%

SEVERE

Rate of accumulation exceeds the capability of de-icing/anti-icing equipment. Immediate action required. Even FIKI-certified aircraft are not approved for severe icing. PlaneWX always marks severe icing as unfavorable regardless of aircraft equipment.

Multi-Model Confidence

One of PlaneWX's most powerful capabilities is multi-model consensus scoring. Instead of trusting a single model, we compare all three and rate how much they agree.

HIGH

Unanimous

All models agree on icing severity at this altitude and location. You can have high confidence in this forecast. If all three say moderate icing at 8,000 ft, expect moderate icing at 8,000 ft.

MODERATE

Majority

Most models agree, with one or two differing. The majority view is likely correct, but there's some uncertainty. PlaneWX uses the majority consensus as the primary forecast and notes the dissent.

LOW

Split

Models disagree significantly. This happens at atmospheric boundaries where conditions are changing rapidly. Low confidence doesn't mean no icing — it means the atmosphere is uncertain. Plan for the worse-case model and have an exit strategy.

Model agreement labels appear in your briefing's icing section and in the Weather Sources panel. "Unanimous" means all models agree. "Split" means they disagree. This is valuable intelligence that traditional aviation weather products simply don't provide.

Route Sampling

PlaneWX doesn't just check icing at your departure and arrival. We sample 3 to 7 points along your route, depending on route length, to build a complete picture of icing conditions from takeoff to landing.

At Each Sample Point, We Query:

  • Temperature at 20 pressure levels (1000–300 hPa)
  • Relative humidity at 20 pressure levels
  • Geopotential height (actual altitude of each pressure level)
  • Dewpoint depression at each level
  • Cloud cover at low, mid, and high layers
  • Freezing level height from each model
  • Surface temperature and visibility
  • Precipitation type and probability

This means for a typical 300 NM flight, PlaneWX analyzes approximately 300 data points (5 sample points × 20 altitude levels × 3 models) to build your icing profile. All of this data is available in the Weather Sources panel for full transparency.

Ice Types: Clear, Rime, and Mixed

Not all ice is created equal. PlaneWX identifies the type of ice you're likely to encounter based on the temperature at your cruise altitude. This matters because different ice types affect your aircraft differently and require different responses.

Clear IceMost Dangerous

Temperature

0°C to -10°C

Appearance

Smooth, transparent, glass-like

Formation

Large supercooled water droplets

Clear ice is heavy, hard to see, and difficult to remove. It forms when large supercooled droplets hit the aircraft and spread before freezing, creating a smooth layer that conforms to the airfoil shape. It accumulates rapidly, adds significant weight, and can change the wing's aerodynamic profile. De-icing boots may be less effective because the ice conforms tightly to the surface.

Rime IceMore Common

Temperature

-10°C to -20°C

Appearance

Rough, opaque, milky white

Formation

Small supercooled water droplets

Rime ice forms when small droplets freeze instantly on contact, trapping air bubbles and creating a rough, white, opaque coating. It accumulates on leading edges and is generally easier to remove with de-icing equipment. While rime ice is easier to manage than clear ice, it still degrades performance and should not be taken lightly.

Mixed Ice

Temperature

-10°C to -15°C

Appearance

Combination of clear and rime

Formation

Both large and small droplets present

Mixed ice combines characteristics of both clear and rime ice and can be unpredictable. It often forms in clouds with varying droplet sizes or at temperatures in the transition zone.

SLD Risk & Warm Nose Detection

Supercooled Large Droplets (SLD)

SLD conditions are among the most dangerous icing scenarios in aviation. Supercooled large droplets are raindrops or large cloud droplets that remain liquid below 0°C. When they strike an aircraft, they run back along the surface before freezing — accumulating ice behind the protected areas of boots, heated surfaces, and TKS panels.

Even FIKI-certified aircraft can be overwhelmed by SLD conditions. The American Eagle ATR-72 crash in Roselawn, Indiana (1994) was caused by SLD ice accumulating behind the de-ice boots. This accident led to significant FAA regulation changes.

What Is a "Warm Nose"?

A warm nose is a layer of above-freezing air sandwiched between subfreezing layers in the atmosphere. It's a key indicator of SLD risk and freezing rain.

Altitude profile (example):

15,000 ft -18°C ❄️  Subfreezing (ice crystals)

10,000 ft  -8°C ❄️  Subfreezing (supercooled water)

6,000 ft  +2°C 🌡️  WARM NOSE — ice melts into rain

3,000 ft  -3°C ❄️  Subfreezing — rain refreezes as SLD/freezing rain

Surface    -1°C ❄️  Subfreezing

When ice crystals or snow fall through the warm layer, they melt into rain. As that rain continues falling into the subfreezing layer below, it becomes supercooled — liquid water below 0°C. These large, supercooled drops are the defining characteristic of SLD conditions.

How PlaneWX Detects SLD Risk

PlaneWX uses two independent SLD detection pathways:

  • CIP nowcast (0–2 hours): The Current Icing Product includes a direct SLD probability field derived from radar, satellite, and observations. When SLD probability exceeds phase-specific thresholds (10% climb/descent, 20% cruise), PlaneWX scores it deterministically — the WX Score reflects the risk regardless of what the AI analysis says.
  • DAFS IFI (4–18 hours): The Icing Forecast Integration product also includes a dedicated SLD potential field. For flights departing 4–18 hours out, IFI SLD potential is evaluated at the same thresholds as CIP, giving you SLD guidance beyond the CIP nowcast window.
  • NWP warm nose (any range): PlaneWX scans the temperature profile from each model at each sample point along your route. If we detect a warm layer (above 0°C) sandwiched between subfreezing layers, we flag it as a warm nose and assess SLD/FZRA risk. A warm nose + cloud moisture = hard NO-GO, regardless of FIKI status or icing severity.

Visual indicator: A thin amber "FZRA risk" strip appears below the descent portion of the Icing Route Bar when a warm nose is detected during descent. Because CIP only detects in-cloud structural icing and freezing rain falls below the cloud base, the bar itself shows NONE for in-cloud icing while the tile separately shows the FZRA severity. Hover the amber strip for a full explanation of the distinction.

Total Icing Exposure

PlaneWX calculates your total time in icing conditions broken down by flight phase. This is calculated server-side from your route, altitude, aircraft climb/descent performance, and the icing layer boundaries — not estimated by AI.

Climb

Time spent climbing through the icing layer from departure airport elevation to cruise altitude. Based on a standard 500 ft/min climb rate.

Cruise

Time at cruise altitude inside the icing layer. If your cruise altitude is within the icing band, this is the duration of your entire cruise segment.

Descent

Time spent descending through the icing layer from cruise altitude to destination elevation. Based on a standard 500 ft/min descent rate.

TKS Fluid Planning

If your aircraft uses a TKS (weeping wing) anti-ice system, total icing exposure is critical for planning fluid usage. Most TKS systems have limited fluid capacity — typically 1.5 to 4 gallons depending on the system. Knowing exactly how many minutes you'll be in icing helps you determine if you have enough fluid for the flight, or if you need to adjust your route or altitude.

Example: A TKS system consuming 0.6 gal/hr in "normal" mode with a 2.5 gallon tank provides approximately 4 hours of protection. If your total icing exposure is 45 minutes, you have plenty of margin. If it's 3 hours, you're cutting it close.

Icing Trap Analysis: Can You Actually Avoid It?

Icing severity alone doesn't tell the full story. A light icing layer at 8,000 ft is a very different problem depending on whether you can fly at 5,000 ft below it, climb above it at 12,000 ft — or whether frozen cloud fills your entire flyable altitude band from terrain to your service ceiling with no escape.

PlaneWX's icing trap analysis answers the question traditional icing products ignore: can this pilot, in this aircraft, on this route, actually avoid the icing by choosing a different altitude? If yes, the penalty is modest. If the entire usable altitude band is frozen and there's no way around it, the score reflects a genuine structural trap.

How It Works

At each sample point along your route, PlaneWX defines your usable altitude band: the airspace between safe terrain clearance (terrain + 3,000 ft) and your aircraft's service ceiling. It then calculates what fraction of that band is occupied by frozen IMC (subfreezing temperature + sufficient moisture for cloud).

Crucially, it also checks for two escape routes:

Warm VMC Below

Is there at least 1,500 ft of above-freezing air below the icing layer base? If so, descending below the icing is a real option. This escape is blocked when a warm nose (SLD/FZRA) inversion is detected — warm air above a cold layer is not a safe escape.

VMC Above Cloud Tops

Are cloud tops at least 2,000 ft below the service ceiling? If so, climbing above the icing is a real option. Also considered: if the cruise altitude is already above the icing layer top, maintaining cruise altitude is itself an escape.

The analysis runs separately for three flight phases — departure climb, enroute cruise, and arrival descent — because the escape options are different in each phase. The overall trap classification is the worst of the three.

Trap Classifications

NONE

Less than 20% of your usable altitude band is frozen IMC. Icing is easily avoided by a modest altitude change. Scored on severity and exposure time only.

PARTIAL

20–49% of the usable band is frozen, and an escape route exists. Icing is a real factor but manageable with altitude planning. Modest additional deduction (≈5–15 pts).

SEVERE

50–79% of the band is frozen, or 20–49% with no escape route. Significant unavoidable icing exposure. Larger deduction (≈15–30 pts), halved for FIKI-equipped aircraft.

FULL

50%+ of the band is frozen with no escape route — or 80%+ regardless. Frozen IMC fills the entire flyable envelope. Maximum deduction (≈30–50 pts), halved for FIKI. If the underlying icing severity is also severe, this becomes an automatic NO-GO regardless of FIKI.

FIKI and the Trap

FIKI (flight into known icing certification) halves most trap-related deductions — because a certified aircraft can safely transit icing that would force an unequipped aircraft to divert. However, FIKI provides no exception for severe structural icing, which is always a NO-GO regardless of equipment. And FIKI provides zero mitigation for SLD (supercooled large droplets), which is handled separately.

Why This Matters for Your Score

Without trap analysis, a route with unavoidable frozen cloud end-to-end could receive the same score as a route with a thin icing layer easily avoided by flying 1,000 ft lower. The trap classification ensures that truly inescapable icing is scored much more conservatively than icing you can plan around — which more accurately reflects the real decision a pilot faces.

How Icing Affects Your WX Score

Icing deductions use your personal minimums and aircraft capabilities. The same icing conditions can produce very different scores for different pilots — and that's by design.

Soft / Hard Limit System

PlaneWX uses a two-tier minimums system for icing:

Comfort (Soft Limit)

The icing severity you're comfortable with. Exceeding this puts you in the caution zone with a graduated penalty.

Example: Soft = Light. If forecast shows Light icing, minimal deduction.

Limit (Hard Limit)

The maximum icing severity you'll accept. Exceeding this is unfavorable — score drops to 0% within 12 hours.

Example: Hard = Moderate. If forecast shows Severe icing, unfavorable.

ScenarioImpactExample
Any icing, no FIKIUnfavorable (0%)Light icing forecast, aircraft has no de-ice/anti-ice
Severity exceeds hard limitUnfavorable (0%)Hard limit = Moderate, forecast = Severe
Severe icing (any pilot)Unfavorable (0%)Severe icing is always unfavorable regardless of FIKI or limits
Severity between soft and hardCaution (-5 to -25)Soft = Light, Hard = Moderate, forecast = Moderate
Severity at or below soft limitMinimal (-5)Soft = Moderate, forecast = Light (within comfort zone)

Aircraft-specific overrides: If your aircraft profile has icing limits set, those override your personal minimums (using the more restrictive value). A FIKI-equipped aircraft with icing hard limit set to "Moderate" will use that limit. A non-FIKI aircraft will always be flagged unfavorable for any icing — even trace.

Reading the Icing Section in Your Briefing

The icing section of your briefing contains several key pieces of information, all derived from the multi-model analysis. Here's how to read it:

Icing Layer Boundaries

Your briefing shows the altitude range where icing conditions exist — for example, "Icing Layer: 853 – 14,101 ft". This tells you exactly where you'll enter and exit icing on climb and descent. If your cruise altitude falls within this range, you'll be in icing for the entire cruise.

Cloud Entry / Exit Altitudes

Based on relative humidity profiles, PlaneWX identifies where you'll likely enter and exit clouds. Cloud base and tops are derived from the altitude where RH crosses the 80% threshold. This is especially useful for VFR pilots assessing cloud clearance requirements.

Freezing Level

The altitude where the temperature crosses 0°C. Each model provides its own freezing level, and your briefing shows the consensus. If the freezing level is near or below your departure airport elevation, expect icing from the surface up.

Confidence & Model Agreement

Each briefing includes the multi-model confidence level (HIGH / MODERATE / LOW) and whether models are "unanimous" or "split" at your cruise altitude. This helps you gauge how much to trust the icing forecast and whether conditions might be better or worse than predicted.

Ice Type at Cruise

Based on the temperature at your cruise altitude, PlaneWX predicts whether you'll encounter clear ice, rime ice, or mixed ice. Hover or tap on these terms in your briefing for educational tooltips explaining each type.

Total Icing Exposure

The total time you'll spend in icing conditions, broken down by climb, cruise, and descent. This is computed from your aircraft's performance data and the icing layer boundaries — not estimated by AI. Use this for TKS fluid planning and assessing whether prolonged exposure is within your aircraft's capabilities.

Time in Cloud (IMC) Bar — Temperature Overlay

The IMC bar below the icing section shows where you'll be in cloud during cruise. Hover any segment for a card-style tooltip showing temperature at cruise altitude, relative humidity, and cloud cover percentage. When the temperature is at or below 0°C and you're in cloud, a snowflake indicator appears — giving you an immediate in-cloud icing signal without needing to cross-reference the separate icing analysis.

Full Transparency: Weather Sources Panel

PlaneWX believes in showing its work. Every briefing includes a Weather Sourcespanel where you can see the raw model data that powered the icing analysis.

What You'll Find in the Forecasts Tab

  • Model overview: Which models were queried (HRRR + GFS + ECMWF), overall confidence, max severity, and icing layer range
  • Per-sample-point tables: Each sample point along your route shows a table with altitude, temperature, relative humidity, icing probability, severity, and model agreement
  • Freezing levels per model: HRRR, GFS, and ECMWF freezing levels shown side by side at each sample point
  • Cloud highlighting: Altitude levels with RH ≥ 80% are highlighted to show where you're likely in clouds
  • Fetch timestamp: Exactly when the model data was retrieved, so you know how current it is

Why do we show raw data? Most aviation weather apps present conclusions without evidence. PlaneWX shows you exactly what data we used and how we arrived at our assessment. This builds trust, enables independent verification, and helps you become a better weather decision-maker over time. If you disagree with our assessment, you can see the underlying data and make your own judgment.

Section-Level Sources

Every section of your briefing — icing, turbulence, ceilings, winds — has a Sources button. Tapping it reveals exactly which weather products contributed to that specific section, along with raw data snippets.

Icing Section Sources Include:

  • CIPCurrent Icing Product nowcast — observation-fused icing severity, probability, and SLD potential (for departures within 4 hours)
  • IFIDAFS Icing Forecast Integration — aviation-specific icing probability, severity, and SLD potential at 3-km resolution (for departures 4–18 hours out)
  • HRRR3-km resolution model sounding at sample points along your route
  • GFS13-km global model sounding at sample points along your route
  • ECMWFEuropean Centre 9-km model sounding — independent verification and extended range
  • ICON EUDWD 7-km European regional model — used for European routes instead of HRRR
  • ICON D2DWD 2-km central European nest — highest-resolution model in the suite for covered regions
  • G-AIRMETActive G-AIRMET Zulu (icing) advisories along your route
  • PIREPsRecent pilot reports of icing within your route corridor

Educational Tooltips

PlaneWX is designed to make you a better weather decision-maker, not just tell you what to do. Throughout your briefing, you'll see aviation terms and model names that are interactive — hover or tap to see educational definitions.

Terms with Tooltips:

HRRRGFSECMWFICON EUICON D2G-AIRMET ZuluG-AIRMET SierraG-AIRMET TangoCIPDAFS IFIClear iceRime iceMixed iceSLDWarm noseFIKITKSEDROATTASDAPAARTCC

These terms appear underlined with a dotted border in your briefing. Hover (desktop) or tap (mobile) to see the full definition without leaving your briefing.

How This Compares

PlaneWX's multi-model icing analysis provides significantly more detail and transparency than traditional aviation weather tools.

CapabilityPlaneWXTraditional
CIP/IFI nowcast-forecast fusion0–18 hoursNot available
Multi-model comparison3–5 modelsSingle product
Confidence scoringYesNo
Route-specific sampling3–7 pointsBroad areas
Cloud layer boundariesYes (RH-derived)Not provided
Ice type predictionClear/rime/mixedNot provided
SLD / warm nose detectionYesSLD AIRMETs only
Total icing exposureClimb/cruise/descentNot calculated
Personal minimums integrationSoft + hard limitsGeneric severity
Raw data accessFull transparencyConclusions only
Altitude-specific assessment20 pressure levelsAltitude range only

Limitations & Important Notes

Model Data Is a Forecast

Model soundings are forecasts, not observations. They predict where icing conditions will be, not where they are right now. Real-time PIREPs and current METARs always take precedence for imminent flights. PlaneWX includes both in your briefing.

Severity Is Derived, Not Measured

Icing severity is derived from temperature and humidity profiles using proven meteorological relationships. It is not a direct measurement of ice accumulation rate on your specific aircraft. Actual accumulation depends on aircraft speed, airfoil shape, droplet size, and exposure time.

HRRR Coverage Is U.S. Only

The HRRR model covers the contiguous United States only. For flights outside CONUS, the analysis falls back to GFS and ECMWF. For European routes specifically, ICON EU and ICON D2 are added to provide high-resolution regional coverage — so European pilots benefit from up to four independent models rather than just two.

Not a Substitute for Official Briefing

PlaneWX's multi-model icing analysis supplements — but does not replace — official weather products. Always cross-reference with current G-AIRMETs, SIGMETs, and PIREPs. The pilot in command is always responsible for the final go/no-go decision per 14 CFR 91.3.

About This Documentation

PlaneWX's icing analysis is continuously improved based on pilot feedback and model verification. For US domestic routes, the system uses HRRR, GFS, and ECMWF (via Open-Meteo) as the NWP backbone, with the FAA/NWS Current Icing Product (CIP) nowcast for 0–4 hours and the DAFS Icing Forecast Integration (IFI) for 4–18 hours. ICON EU and ICON D2 (DWD) replace HRRR for European routes. CIP and IFI data are fetched hourly from NCEP/NWS infrastructure, decoded, and cached on PlaneWX servers before delivery to your briefing.