Module 1 of 7

Marine Weather Without the Nonsense

Goal: Translate weather jargon into plain English so you can read a marine forecast and know what the boat and crew will actually feel.

Why forecasts often feel like a foreign language

Weather forecasts are written by meteorologists for meteorologists, then handed to sailors. The result is sentences like: "Seas 4 to 6 feet occasionally 8, with a southeasterly swell 3 to 5 feet at 12 seconds, building to 5 to 7 feet through the afternoon."

That sentence contains at least five distinct concepts compressed into one. If any of them is unfamiliar, you'll misread the whole picture. Let's unpack each one properly.

The essential terms

Sustained wind vs. gusts
Not the same number
Sustained wind is the average over 1–2 minutes — it's what the forecast number means. Gusts are short spikes lasting seconds, typically 30–50% higher than sustained in trade wind conditions.

If forecast says "15 knots," expect gusts of 20–22 regularly. If it says "15, gusting 25," you're in lumpier air with uneven loading on the rig and helmsman.

Why it matters
Your sail trim, autopilot, and reefing decisions should be based on gust speed, not sustained. Sustained 15 with gusts to 25 sails very differently from a steady 20.
Sea state vs. swell
Two different wave systems
Wind waves (sea state) are generated locally by the current wind. They're steep, disorganized, short-period, and nasty. Swell is wave energy from a distant storm — it's organized, longer period, and travels hundreds of miles after the generating wind has stopped.

You can have flat local conditions with 8-foot swell rolling through from a three-day-old Atlantic storm. You can also have 12-knot local wind with no swell — a beautiful sailing day.

Think of it this way
Sea state is what's happening at the restaurant right now. Swell is the kitchen cleanup from last night's rush — still affecting you even though that event is over.
Wave height vs. wave period
Height is less important than period
Wave height is the vertical distance from trough to crest. Period is the time in seconds between crests passing a fixed point.

Here's the surprise: a 6-foot wave at 5 seconds is far worse than a 6-foot wave at 12 seconds. Short period means the waves are steep and close together — the boat pitches violently, dishes slide, crew gets sick. Long period means the waves are gentle rollers — the boat rises and falls slowly, often perfectly sailable.

The rule of thumb
Period under 7 seconds: it's going to be uncomfortable regardless of height. Period over 11 seconds: you can usually sail through it even if height sounds alarming. Always check period.
Fetch
Why the Atlantic swell is so developed
Fetch is the unobstructed distance over which wind has been blowing across open water. More fetch → waves have more time to grow → bigger, more organized swell.

The North Atlantic has essentially unlimited fetch for northeasterly storms. A gale sitting off Iceland for three days has been building waves across 2,000 miles of open ocean before that swell arrives at the Mona Passage. This is why the Mona can be violent even when the local wind is calm.

Key insight
The Caribbean is a nearly closed basin — limited fetch — so local wind waves are less developed. But the Bahamas, DR north coast, and Mona Passage are all exposed to North Atlantic swell with enormous fetch. Always check the Atlantic swell separately from local conditions.
Veering vs. backing
Which way the wind is rotating
Veering: wind rotating clockwise — NE → E → SE. In the Caribbean, this typically means trades reestablishing after a lull. Your window is closing.

Backing: wind rotating counter-clockwise — NE → N → NW. This is what happens as a cold front approaches and passes. Often signals an opening window for eastbound travel.

Van Sant's use
He watches for the wind to back from NE toward N or NW — that's his cue that a front has passed and the post-front window is open. When it starts veering back toward NE, the window is closing. Move.
Ridge, trough, squall line
The structures behind weather patterns
Ridge: an elongated area of high pressure between two lows. Like a spine of stable air. Ridges often bring calm, clear conditions — but they also reinforce the trade winds. When a ridge builds strong over the Atlantic, the trades strengthen.

Trough: an elongated area of low pressure. Associated with unsettled weather, wind shifts, and cloud development. A trough moving through can temporarily disrupt the trades — or bring squalls.

Squall line: a line of intense convective storms, often preceding a cold front. Fast-moving, brings brief violent winds (sometimes 30+ knots for 20–30 minutes) followed by relative calm. Not pleasant to be caught in, but they pass.
"Building," "subsiding," "occasionally to"
Forecast weasel words decoded
"Building": conditions getting worse. "Seas building to 8 feet" means they aren't 8 feet now — but they will be. Factor in where you'll be when they arrive.

"Subsiding": conditions improving. But the ocean lags — swell subsides slowly over 24–36 hours after wind drops.

"Occasionally to": this is the sneaky one. "Seas 4 to 6 feet, occasionally to 8" means 8-foot waves will happen regularly. It's not a rare exception. The "occasionally" is statistical — roughly 10% of waves will hit that height. In a two-hour window, you'll feel several of them.

Read it this way
When planning a passage, always mentally upgrade the "occasionally to" number as your planning assumption. "Occasionally to 8" means you plan for 8.
Light winds with ugly seas
Why "light winds" can still ruin your day
The swell doesn't know the wind has dropped. A 3-day gale 600 miles away generates swell that arrives 24–48 hours after the gale dissipates. Your forecast might show 8–10 knots of wind with "residual swell 6–8 feet at 8 seconds."

In light wind with leftover swell, your sails flap, the boat rolls uncomfortably, and the motion is often worse than in moderate wind — at least then the boat is pressed over and tracking steadily. In a light-air slop, you're a cork.

Van Sant's response
He often motorsails in these conditions rather than fighting the slatting. The engine provides the stability the wind isn't. No shame in it.

Putting it together: reading a real-style forecast

Sample forecast: "OUTSIDE WATERS — SEAS 4 TO 6 FEET OCCASIONALLY 8 IN THE NORTHEAST SWELL. WINDS NORTHEAST 15 TO 20 KNOTS. LOCALLY HIGHER GUSTS IN VICINITY OF SQUALLS."

What this actually means: Trades are up. Swell is from NE (the same direction you're trying to go). You'll see 8-foot seas regularly, not occasionally. Gusts will hit 28–30 near squalls. This is a classic "do not depart" day for an eastbound boat. Wait.
Module 2 of 7

The Big Engine of the Route

Goal: Understand the normal weather machine from Florida to Puerto Rico — so you stop seeing weather as random and start seeing the pattern.

The trade wind problem

The Caribbean trade winds blow from the northeast, roughly 10–25 knots, for most of the year. They exist because the Bermuda High — a massive, semi-permanent high-pressure system sitting over the subtropical Atlantic — forces air clockwise and southward. The Earth's spin (Coriolis effect) bends that southward flow toward the west, giving you steady NE winds across the Caribbean basin.

For a boat trying to go east or southeast from Florida toward Puerto Rico, this is the core problem. The wind is coming from exactly where you want to go. You can't sail directly into it. You tack — but with islands, shoals, and current against you, every degree off your intended course costs miles. This is the Thorny Path.

The Bermuda High and trade wind pattern
Bermuda High HIGH PRESSURE NE trades 15–25 kts → Florida start Bahamas Cuba / DR Mona Puerto Rico destination Dashed gold = your desired direction. Blue arrows = wind direction. They are directly opposed.

How winter cold fronts change everything

Between November and April, cold fronts sweep down from North America every 7–14 days. Each front temporarily disrupts the trade wind pattern. As a low-pressure system tracks east across the continent, it pulls warm southern air northward — suppressing or reversing the trades in its wake.

The sequence: before the front arrives, southerly flow often produces light, variable winds — a potential window. During the front, line squalls and shifting winds — stay put. After the front passes, winds back to N or NW and often go light. This is the window. It typically lasts 18–36 hours before the trades reestablish.

Van Sant's core insight: Most sailors wait for the "nice weather" window — a stretch of light easterlies. Those windows are rare and brief. Van Sant waits for the post-front window — NW or N winds that are actually favorable for eastward travel. The sailors hiding in harbor waiting for perfect weather are the ones who never get to Puerto Rico.

Why the route gets harder as you go

The trade winds strengthen and become more consistent as you move south and east. Florida to the Bahamas is the easiest stretch — you're in the transition zone. The Bahamas to the Dominican Republic is harder. The north coast of Hispaniola is a sustained windward grind. The Mona Passage is the most demanding single crossing on the route.

Additionally, the Caribbean topography creates funneling effects. Wind accelerates through inter-island passages and around capes. What's 18 knots in open water can be 28 in the Windward Passage between Cuba and Haiti. Plan for this — always.

Shoulder season note: May–June and November offer some of the best windows. The trades are transitioning, fronts are still occurring, and hurricanes are either ending or not yet active. Van Sant typically preferred to make the passage in these months.
Module 3 of 7

Reading the Forecast Stack

Goal: Stop depending on one source. Learn to triangulate between multiple forecasts so you can separate "forecast says 15 knots" from "realistically this is going to suck."

Why one source is never enough

Every weather model has a resolution, a refresh cycle, and a set of assumptions baked in. A single source gives you a single model's best guess. Where models agree, you can trust the forecast. Where they disagree, there's genuine uncertainty — and you should know that before leaving the dock.

Van Sant famously consulted multiple sources before every passage. His hierarchy: buoy observations (truth), then text forecast, then graphics, then model output. He treated GRIB files as a planning tool, not a go/no-go decision.

Your forecast stack

NWS Offshore Text Forecast
VHF WX channels / weather.gov
The official marine forecast. Read it carefully — the language is compressed but precise once you know the vocabulary. Updated every 6 hours.
High reliability for 48hrs
NHC Marine Graphics
nhc.noaa.gov / offshore graphics
Visual surface analysis charts showing highs, lows, fronts, and isobars. Essential for understanding the overall pattern — where is the ridge? Where is the front?
Pattern overview
Local Forecast Office Discussion
forecast.weather.gov → AFD
The Area Forecast Discussion is where the meteorologist explains their reasoning — including uncertainty. "Models disagree on front timing" is information you can't get from the summary.
Highest value, underused
Windy.com
windy.com / mobile app
Visual GRIB overlay with multiple model selection (GFS, ECMWF, ICON). Excellent for seeing how different models handle a front. Switch models — if they disagree, uncertainty is real.
Good for days 1–4
PredictWind
predictwind.com (subscription)
Higher-resolution model output with offshore routing. Their PWGFS and PWECMWF models run at finer resolution than the free versions. Useful for wave detail and passage routing.
Best wave detail
NDBC Buoys
ndbc.noaa.gov
Actual measured conditions — not a model. If a buoy near your route shows 8-foot seas at 6-second period right now, that's real. Compare to the forecast. If they diverge, trust the buoy.
Ground truth — always check

The triangulation rule

Before any passage decision: Check NWS text forecast. Check a surface analysis chart for the pattern context. Check Windy with GFS and ECMWF — if they agree, confidence is higher. Check the nearest buoy for ground truth. Read the AFD for uncertainty language. Only then make the call.
The bias to know: Forecasts are systematically biased toward underestimating conditions near islands and in channels. The NWS forecasts open ocean. You are not in open ocean — you are near Hispaniola or in the Mona. Add 20–30% to wind and swell forecasts near land and in passages. Van Sant does this automatically.
Module 4 of 7

Weather Windows for Going to Windward

Goal: Understand the counterintuitive part — why you move in lulls and transitions, and why you start thinking in windows, not dates.

The paradigm shift

Recreational sailors think about departing when the weather is "nice." Van Sant thinks about departing when the weather is less bad than it usually is for an eastbound boat. These are not the same thing.

Normal trade wind conditions — 15–20 knots from the NE, 4–6 foot seas — are perfectly pleasant sailing weather if you're going downwind. They are miserable, slow, and potentially dangerous for a boat trying to make easting. A "nice day" for a Bahamas beach trip is a "no-go" day for the Thorny Path.

The inversion: Your weather window on this route is often defined by conditions that would cause a normal sailor to stay in port. A low-pressure system approaching. A cold front passing. North or NW winds that landlubbers call "blustery." That's your green light.

What makes a window

A valid eastbound window has several components working together:

Wind direction: N, NE, or NW is manageable. E or SE means you're headed directly into it — wait. NW is often the best possible direction for an eastbound boat.

Wind speed: Under 15 knots sustained is comfortable. 15–20 is workable with good sea state. Over 20 on the nose with swell — wait.

Swell height and period: Under 6 feet at 10+ second period is generally acceptable. Over 6 feet at short period — wait, even if wind looks fine.

Duration: The window needs to last long enough for your leg. A 40nm night hop needs 8–10 hours. The Mona Passage needs 18–24 hours of good conditions. Don't start a long leg into a closing window.

Interactive: Is this a window?

Seven-day forecast for a boat staged in Luperon, DR, planning to cross the Mona Passage. Tap each day for the call.

Mon
NE 22
kts
Wait
Tue
N 9
kts
Maybe
Wed
NW 12
kts
Go
Thu
NE 18
kts
Wait
Fri
E 25
kts
Wait
Sat
N 8
kts
Go
Sun
NE 16
kts
Maybe
Tap a day above to see the reasoning behind the call.

The night departure principle

Van Sant almost always departs at or just before midnight. This is not arbitrary. It's because the night lee effect — the calming of wind near large landmasses as the land cools — is strongest from roughly midnight to 9am. Departing at midnight lets you:

1. Motor or motorsail in the calm zone during the best conditions
2. Be well offshore by dawn when any wind acceleration begins
3. Arrive at your destination by mid-morning, before afternoon trades build
4. Anchor and rest while the afternoon trades blow past you

Landfall determines departure, not the other way around. Work backward from your destination anchorage. When do you need to arrive? That tells you when to leave. Van Sant never departs based on a calendar — only on the physics of the leg.

Module 5 of 7

Island and Coastal Effects

Goal: Understand the local geography tricks — why two boats in the same region can have completely different experiences, and why forecasts are often "wrong" close to land.

The night lee effect

This is Van Sant's signature technique, and the physics behind it are straightforward once explained.

During the day, the sun heats the land. Warm land heats the air above it, which rises. The trade winds rush in to fill the low-pressure gap — amplifying in the process. Wind near shore is stronger during the day than offshore because of this thermal pumping.

At night, the land cools rapidly. The thermal pump reverses or stops. In the lee of large landmasses — particularly mountainous ones like Hispaniola (peaks over 10,000 feet) and Puerto Rico — the wind calms significantly in a band roughly 5–15 miles offshore. Often 5–12 knots when the offshore forecast shows 18–22.

Night lee vs. daytime thermal amplification
DAY ☀ island / mountainous coast thermal rise strong 20+ kts amplified all the way to shore NIGHT 🌙 island / mountainous coast calm zone 5–12 kts sail here midnight–9am trades still NE katabatic outflow
Critical timing detail: The night lee disappears quickly as the sun rises and the land heats. By 9–10am it's gone. Van Sant's schedule is non-negotiable: depart at midnight, arrive before 10am, anchor and sleep. Anyone departing at dawn misses the entire window.

Katabatic winds — the mountain gift

Katabatic means "flowing downhill." At night, air near mountain peaks cools and becomes denser than the surrounding air. That cold, dense air drains down mountain slopes toward the sea — creating an offshore wind that can reach 15–25 knots near the coast of high islands like Hispaniola.

This sounds counterproductive — but it's actually what creates the night lee. The katabatic outflow pushes against the trades near the coast and suppresses them. It also means that sailing very close inshore at night on the north coast of the DR, you may find the katabatic flow actually filling your sails from behind, helping you east. Van Sant exploits this directly.

Wind acceleration zones — the dangerous flip side

The same geography that creates calm lees also creates dangerous acceleration zones. Wind squirts through inter-island channels and around headlands, sometimes at 150–200% of the open-ocean speed. The Windward Passage between Cuba and Haiti, the gap near Cape Engaño on the DR's northeast tip, and the Anegada Passage further south all funnel and accelerate wind dramatically.

Add the Venturi effect (fluid speeds up when forced through a narrowing) to background trade winds already 20 knots, and you can encounter 35–40 knots in passages where the NWS offshore forecast shows 20. This is not a forecast error. It's local physics that no model resolves well at the island scale.

The local knowledge imperative: This is why Van Sant's route-specific guidance matters so much. He has sailed each passage dozens of times and documented the acceleration zones, the calm pockets, the time of day effects for each specific headland and channel. No general-purpose forecast tool replicates this.
Module 6 of 7

Route Segments & Decision Rules

Goal: Make it operational — build decision frameworks for each leg of the Florida to Puerto Rico route.

The route overview

The Thorny Path is not one passage — it's a series of distinct legs, each with its own character. What works for the Bahamas doesn't necessarily work for the Mona. Click each leg on the route below for its specific go/wait/divert criteria.

Leg-by-leg decision framework

Florida East Coast & Gulf Stream Crossing

The Gulf Stream runs north at 2–4 knots between Florida and the Bahamas (roughly 50nm). Wind against current — any northerly component to the wind — creates steep, dangerous breaking seas in the Stream. This is the first serious commitment of the voyage.

Distance: ~50nm to Bimini or ~90nm to Nassau area. Typically motored or motorsailed.

Go
Light to moderate S, SE, or E winds 10–15 kts. No fronts within 48 hours. Stream running normal (check NOAA current charts).
Wait
Any N or NE component to wind while in or crossing the Stream. Front approaching within 24 hours. Forecast seas over 4 feet in the Stream.
Divert
If conditions deteriorate mid-crossing, turn and run south in the Stream to a Florida inlet. Do not try to push through north winds in the Gulf Stream.
Module 7 of 7

The Skipper's Weather Routine

Goal: Turn everything you've learned into a repeatable process. You are no longer "checking weather." You are running a system.

Why process beats judgment alone

Good judgment comes from experience. But on a passage you haven't made before, experience is exactly what you lack. A repeatable process fills that gap. It forces you to check all the sources, ask all the questions, and make the decision systematically — not based on optimism, impatience, or a vague feeling that "it looks okay."

Van Sant's philosophy, decoded: he doesn't just wait for weather. He watches weather with a specific process, on a specific schedule, until the pattern he's looking for emerges. Then he moves immediately.

The daily weather cycle

Horizon What you're doing Sources Decision
72-hour outlook Watching the pattern. Where are the fronts? Is a window forming or closing? This is planning, not committing. NHC graphics, Windy (GFS + ECMWF comparison), AFD for uncertainty language Tentative go/no-go for the leg. Alert crew.
48-hour check First real commit decision. Models should be aligning if the window is real. Diverging models = uncertainty = wait. All sources. Compare models. Read the buoy trends for your area. Commit or don't commit. Provision and fuel if committing. Rest.
24-hour update Verify the window is still there and hasn't shifted. Check swell specifically — especially for the Mona. NWS text forecast (most current), PredictWind wave detail, buoys. Final go/wait call. Departure time confirmed.
Departure check 30–60 minutes before casting off. Final state of the atmosphere. Any squalls in the area? Barometer trend? VHF WX, visual sky assessment, barometer reading and recent trend. Go or hold. No pride here — a hold is free. A mistake is expensive.
Underway (every 4–6 hrs) Update against unfolding reality. Are conditions matching forecast? Is swell building faster than expected? VHF offshore forecast, visual sea state assessment, Windy if offshore connectivity. Continue, modify speed/course, or identify bail-out harbor.
Bail-out criteria Pre-defined before departure. If conditions exceed X, you go to Y harbor. Decided with clear head, not in the middle of a nasty night. Chart — pre-marked bail-out anchorages for each leg. No discussion required. If criteria met, you go. Period.

The skipper's pre-departure checklist

Before every departure, answer these seven questions:

1. What is the wind direction and speed for the full duration of my leg?
2. What is the swell height and period — and what was the Atlantic weather 48 hours ago?
3. Are there fronts within 36 hours that could change conditions mid-passage?
4. Do the GFS and ECMWF models agree on the forecast?
5. What does the nearest buoy currently show?
6. Where is my bail-out harbor if conditions deteriorate?
7. Am I departing at the right time to maximize the night lee?

If you can't answer all seven confidently, you're not ready to go.

The mindset: patience is strategy

Van Sant's most important lesson is not meteorological — it's philosophical. The sailors who get hurt on the Thorny Path are almost always on a schedule. A flight home. A haul-out appointment. A rental car return. The weather doesn't care.

The sailors who arrive safely — and have a good time doing it — have built genuine flexibility into the passage. They budget 3–6 weeks for what might take 3 days in ideal conditions. They enjoy the anchorages. They treat a 10-day wait in Luperon as part of the cruise, not a failure.

Course complete.
You now have the mental model that Van Sant spent decades building the hard way. The weather machine from Florida to Puerto Rico is no longer mysterious — it's a pattern you can read, anticipate, and exploit.
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