Weather Forecasts and Interpretation
- richard76553
- Jan 7
- 8 min read
Updated: Jan 10
When my student “skipper-of-the-day” is discussing the weather as part of presenting the passage plan, my usual reaction is:“Where did you get this information from?”
The standard answer is: “An app” or “the internet.”When asked about the reliability of this information, “I don’t really know” is the slightly disappointing but common response.
This is a problem. Weather is a critical input during all phases of passage planning:
Appraisal – shall we go or shall we stay?
Planning – shaping a route and timing based on the forecast
Execution – how do we sail the plan safely?
Monitoring – when do we need to adapt or abort?
Simply reading wind direction and speed off a screen is not enough. Good seamanship requires understanding where forecasts come from, what they can and cannot tell us, and how to interpret them in context, while continuously combining them with our own observations.
Observation: The Skipper’s First Weather Model
Before opening any app, the skipper should look outside.
Observation is the starting point of situational awareness and remains the most immediate and reliable source of information we have. What matters is not only what the weather is doing now, but also what the signs are for change.
Questions every skipper should be asking:
Actual wind speed and direction
How it is changing over time (logbook)
Whether the wind is backing or veering
Whether it is steady or gusty
Visibility trend
Development of the sea state
Cloud type and evolution
Barometric pressure trend
Traditional observations used by seafarers for centuries remain valid today, such as:
Red sky at dawn – unsettled weather approaching
High, thin cirrus (“mares’ tails”) – a low-pressure system is arriving
Rapid vertical cloud build-up – squalls or thunderstorms possible
Sudden calm after steady wind – often precedes strong weather and a significant wind shift
Birds flying low – falling pressure and deteriorating weather
What Is a Weather Model?
A weather model is a mathematical simulation of the atmosphere. It divides the world into a three-dimensional grid and calculates how air pressure, wind, temperature, and moisture evolve over time. The model calculates conditions at grid points, not at your exact position.
The Pillars Behind Every Weather Model
1. Observation
All models depend on real-world measurements from land stations, offshore buoys, ships, weather balloons, and increasingly from satellites. If observations are sparse (open ocean, remote areas), forecast confidence is lower.
2. Historical Data
Models are trained and tested against decades of past weather patterns. This is why they perform well in typical situations and less well in unusual ones. The availability of historical data (for example UK waters versus the Indian Ocean) directly affects forecast quality.
3. Science
Meteorology is a rapidly developing science. Large-scale drivers such as El Niño and atmospheric oscillations were only properly understood in recent decades. As scientific understanding improves, so do the models.
4. Computing Power
Forecasting skill is closely tied to computing power. Faster computers allow:
Finer grid resolution
More complex physics
Larger ensemble forecasts
New AI-based models are already showing impressive results, but no model removes uncertainty, especially regarding wind strength and timing at sea.
Resolution in a Weather Model – and Why It Matters
Resolution refers to the distance between grid points and defines the size of the three-dimensional grid cells for which a forecast is calculated.
In a model with a 25 km resolution, the atmosphere is averaged over each 25 × 25 km grid cell. Within that entire area, the model produces one single forecast value for wind, pressure, and other parameters. Every location inside that grid cell is assumed to experience the same conditions.
Global models, such as the widely used American GFS, are designed to cover very large areas. They perform well when the atmosphere is relatively uniform and when no major features disturb airflow — for example over the open ocean, far from land.
Problems arise when local features exist inside a grid cell. Mountains, cliffs, coastlines, headlands, and narrow channels strongly influence airflow, acceleration, and turbulence. A low-resolution model cannot “see” these features and therefore smooths them out.
Only high-resolution models (typically 1–3 km) can represent small-scale phenomena highly relevant to sailors, such as:
Sea and land breezes
Wind acceleration around headlands
Shelter and gusting close to the coast
Local convergence and divergence zones
Thunderstorms and squall lines
Between grid points, the model interpolates values, assuming smooth changes that often do not exist near coasts.
Key lesson:A low-resolution forecast shows the general picture; a high-resolution forecast reveals the essential details for a safe coastal passage.
25 KM RESOLUTION VS. 1 KM RESOLUTION

Grib Files
A GRIB File is a standardised format used to distribute weather model output and display it in weather apps and chartplotters, using Wind Barbs:

Accuracy of Weather Models
Some models perform better than others, but no single model is consistently the most accurate. Key factors influencing forecast accuracy include:
Model resolution
Availability of historical data
Atmospheric stability (unstable air leads to squalls and gusts that are hard to predict precisely)
The chaotic nature of the atmosphere — small uncertainties in initial conditions grow over time
Time horizon (skill is high in the first 24 hours and drops significantly beyond 5–7 days)
Local effects such as mountains, cliffs, and sea-surface temperature
The Critical Role of Official Maritime Forecasts
GRIB files and weather apps are useful tools, but must never be used in isolation. One of the most important and often neglected sources of information is the official maritime forecast issued by national meteorological institutes.
These forecasts are written by human forecasters, not generated automatically. They combine:
Multiple weather models
Observations from ships, buoys, and radar
Local climatology
Human pattern recognition
This interpretation is invaluable.
The British Shipping Forecast – A Gold Standard
The British Shipping Forecast, issued by the UK Met Office and broadcast by the BBC, remains one of the most practical and safety-focused forecasts available.
It provides information that GRIBs often do not:
Wind direction and force (Beaufort scale)
Sea state
Visibility
Significant weather (rain, squalls, thunderstorms)
Pressure trends
These directly affect safety, comfort, collision risk, sail handling, fatigue, and whether a passage is sensible at all.

The forecast issued by the UK Metoffice for today, covering the island of Wight, showing unfavourable, and potentially dangerous conditions

The Windy App is producing a very different picture for today. A different wind direction, and no sign at all of a Southwesterly Gale (Force 8)
Why Sea State and Visibility Matter More Than Wind Speed
A GRIB showing 15 knots tells only part of the story:
15 knots against strong tide can produce short, steep seas
Residual swell can make conditions uncomfortable or dangerous
Poor visibility greatly increases collision risk
Fog can turn a routine passage into a high-stress exercise
These factors are explicitly addressed in official maritime forecasts and often absent from GRIB displays.
Weather and Passage Planning – A Practical Guide
For my passage planning, I use a structured, layered approach.
Appraisal – Shall We Stay or Shall We Go?
I start with the big picture:
Wind visualisation apps to see system movement
Synoptic charts to identify pressure systems and fronts
If the big picture does not look right, the passage stops here.
Planning
1. Model comparison: compare several forecast models to assess consistency and uncertainty. When models disagree, I assume greater uncertainty and plan conservatively. Predictwind is my favourite tool, allowing for easy comparison between models in both spot and map views.
2. Local maritime forecast:For Spain and the Canary Islands, I always consult the official maritime forecast issued by AEMET. Sea state, visibility, and warnings often outweigh wind speed.
3. Offshore passages: For longer routes (e.g. Lanzarote–Madeira), I use weather routing, as provided by LUCKGRIB as a planning aid — never as an instruction.
Execution
On the day of departure:
Check updated forecasts and compare them with earlier versions
Note changes and update timing
Observe actual conditions, clouds, pressure trend
When possible, look beyond the harbour wall
Monitoring
During the passage:
Continuously observe wind, sea state, clouds
Monitor VHF forecasts and warnings (Channel 16)
Update forecasts and compare them with reality
The Seamanship Rule
Carry on when conditions match expectations — but change the plan early when they do not.
Good passage planning is not about sticking to a plan.It is about recognising when assumptions are no longer valid and decisions must be made.
This is where forecasts, observation, and experience come together — and where good skippers distinguish themselves.
Comparing Weather Models – Strengths and Limitations
One of the major strengths of PredictWind is that it provides access to several different weather models. This allows skippers to compare forecasts rather than blindly trust a single output.
No model is “best” in all situations. Each is built differently and performs better under certain conditions, regions, and timeframes.
ECMWF (European Centre for Medium-Range Weather Forecasts)
Strengths
Widely regarded as one of the most accurate global models
Excellent representation of large-scale pressure systems and fronts
Strong performance in the 2–7 day range
Limitations
Global resolution limits coastal detail
Can smooth out gusts and local acceleration
Best used for:Understanding the overall synoptic pattern and medium-range planning.
GFS (Global Forecast System – USA)
Strengths
Free and widely available
Frequent updates
Useful for identifying trends and changes over time
Limitations
Low resolution (25 km)
Can underestimate wind strength in some situations
Less reliable or unreliable near complex coastlines
Best used for:Cross-checking trends and spotting model agreement or disagreement.
PWG (PredictWind Global)
Strengths
Tuned specifically for marine use
Often more responsive to stronger wind scenarios
Useful counterbalance to GFS and ECMWF
1 km resolution deals with coastal and land effects
Limitations
Based on the GFS model
Best used for: Coastal and near-offshore passage planning where local effects matter.
PWE (PredictWind European)
Strengths
Higher resolution than global models
1 km provides good and usually accurate representation of coastal effects
Often very useful for short-range forecasts (0–3 days) in European waters
Limitations
Shorter forecast horizon
Best used for:Coastal and near-offshore passage planning where local effects matter.
ICON (German Weather Service)
Strengths
Modern global and regional modelling system
Often performs well with wind direction changes and pressure evolution
Good alternative perspective to ECMWF and GFS
Limitations
Like all global models, limited resolution near the coast
Local effects still smoothed
Best used for:Comparing synoptic evolution and timing of systems.
UK Met Office Models
Strengths
Very strong regional models for UK and nearby waters
Excellent handling of frontal systems and wind shifts
Closely aligned with official maritime forecasts
Limitations
Limited geographical coverage
Less relevant outside NW European waters
Best used for:Coastal and offshore planning in UK and adjacent sea areas.
Spire (Data-Driven Model)
Strengths
Uses large volumes of satellite and observational data
Often reacts quickly to changing conditions
Can perform well in data-rich regions
Limitations
Less transparent methodology
Performance can vary by region
Best used for:An additional independent perspective, especially when models disagree.
ARPEGE (France – Global Model)
Strengths
Global model operated by Météo-France
Good representation of large-scale pressure patterns and frontal systems
Often performs well in European and North Atlantic waters
Limitations
Global resolution limits coastal and small-scale detail
Like other global models, local effects are averaged out
Best used for:Understanding the synoptic situation and medium-range planning, particularly when sailing in or near French forecast areas.
AROME (France – High-Resolution Regional Model)
Strengths
Very high resolution (typically 1–2.5 km)
Excellent representation of:
Coastal acceleration
Sea and land breezes
Convective weather and thunderstorms
Particularly strong close to land
Limitations
Short forecast range (usually 36–48 hours)
Limited geographical coverage (based on covering French territory and surroundings
Less suitable for offshore planning
Best used for:Short-range coastal decision-making, harbour departures, and understanding local wind behaviour — especially in summer and in complex coastal terrain
AI-Based Weather Models (Emerging)
Strengths
Extremely fast computation
Increasingly good pattern recognition
Already outperforming traditional models in some scenarios
Limitations
Limited track record
Still rely on the same observational data
Do not remove uncertainty or local effects
Best used for:Early scenario exploration, not final decision-making.
The Key Lesson for Skippers
The real value of comparing models lies not in selecting one “best” model, but in comparing several.
When models broadly agree → confidence increases
When models disagree → uncertainty is high
When uncertainty is high → plan conservatively


Comments