Estimated Circumnavigation Time
~330 days
Range: 290 β 380 days
~24,500 nautical miles at an average effective speed of ~3.1 knots
β΅ Vessel Propulsion Specifications
πͺ
3.0 kts
Kite Power
Within 30Β° of downwind
βοΈ
2.0 kts
Solar β Peak
6 hrs/day, high sun
π
1.0 kt
Solar/Battery β Base
18 hrs/day, all conditions
Key rule: Speeds do not stack. At any moment we use the single best available propulsion mode.
Currents are separate β they add to the vessel's own propulsion speed.
With Starlink routing, we continuously adjust course to keep kite runs within 30Β° of downwind and to ride the strongest favorable currents.
π Methodology & Assumptions
Effective Speed = Own Propulsion + Ocean Current
- Kite (3 kts): Available when wind is within 30Β° of dead downwind on our course. Trade-wind belts give us this ~60β70% of the time.
- Solar peak (2 kts): Midday hours with good sun. We count ~5 hrs/day of peak solar (panels may not always face ideal angle).
- Solar/battery base (1 kt): Remaining hours, night and low-sun, running off stored energy.
- Blended own-propulsion average β 1.5 kts over 24 hours when no kite is flying; β 2.5 kts when kite is active (kite overrides solar most of the day).
- Ocean currents: Major surface currents are added to own propulsion. Typical trade-wind currents = 1β2 kts. Gulf Stream & Kuroshio = 2β4 kts.
- Distances are approximate rhumb-line / practical routing distances, not strict great circles.
Constraints
- π Waves generally under 15 ft β stay north of ~40Β°S and out of hurricane basins during storm season.
- π Avoid active tropical cyclones using Starlink forecasts (re-route as needed; small time penalty).
- πΊοΈ No provisioning or sightseeing stops β continuous motion.
- π§ Route optimized in real-time for wind direction, current flow, and weather avoidance.
π§ Circumnavigation Strategy
The fundamental challenge: there is no continuous low-latitude current system that flows
westward all the way around the globe. The ocean gyres create clockwise circulation
in the Northern Hemisphere and counter-clockwise in the Southern Hemisphere, meaning
eastward-flowing segments are inevitable.
Our strategy follows the "Trade Wind Route" β the classic path used by
sailing vessels for centuries:
- Pacific: Ride the North Equatorial Current & NE Trade Winds westward from Panama toward the Philippines.
- Southeast Asia: Thread through the Philippine and Indonesian archipelagos into the Indian Ocean (the only practical low-latitude passage between Pacific and Indian Oceans).
- Indian Ocean: Ride the NE Monsoon winds & South Equatorial Current southwestward toward Africa.
- Africa: Descend through the Mozambique Channel, then catch the Agulhas Current system to reach the South Atlantic.
- Atlantic: Ride the SE & NE Trade Winds and the South/North Equatorial Currents westward to the Caribbean, then through the Caribbean & up the Gulf Stream.
- Return: Cross the North Atlantic (with some eastward-flowing current to contend with) to complete the circuit.
β Favorable β wind & current aligned downwind
β³ Mixed β some days favorable, some not
β Challenging β fighting currents or light/variable winds
πΊοΈ Route Overview
ASIA
ββββββββββββ Indian Ocean AFRICA ATLANTIC
βPhilippinesβ ββββββββββββββββ ββββββββ βββββββββββ ββββββββ
β β β NE Monsoon / βCape ofβ SE Trades / βCarib-β
β Indonesiaβ S. Eq. Current β Good β S. Eq. βbean β
β β β β Hope β Current β β β
βSingapore β βββββ¬ββββ βPanamaβ
ββββββββββββ β ββββ¬ββββ
β β S. Atlantic β
β β Currents β β
ββββββ§βββββββββββββββββββββββββββββββββββ§ββββββββββββββββββββββ§ββββ
ββββββββββββββββββββββββββββββββββββββββββββββββββββββββββββ
NORTH EQUATORIAL CURRENT & NE TRADE WINDS
βββββββββββββββββββββββββββββββββββββββββββββββββββββββββββββββββββ
PACIFIC OCEAN
βββββββββββββββββββββββββββββββ
NE Trade Winds
& N. Eq. Current
β
[Panama β]
Arrows show the general direction of travel. The route forms a rough loop through all three major oceans.
π Detailed Segment Breakdown
| # |
Segment |
NM |
Own Spd |
Current |
Eff. Spd |
Days |
Conditions |
| 1 |
Panama β 150Β°W (Central Pacific) |
3,500 |
2.5 |
1.0 |
3.5 |
42 |
NE trades + NEqC |
| 2 |
150Β°W β Dateline |
2,500 |
2.5 |
1.0 |
3.5 |
30 |
NE trades + NEqC |
| 3 |
Dateline β Philippines |
2,500 |
2.0 |
0.5 |
2.5 |
42 |
Trades weaken near Asia |
|
Pacific Subtotal |
8,500 |
|
|
3.2 |
114 |
|
| 4 |
Philippines β Singapore |
1,500 |
1.5 |
0.3 |
1.8 |
35 |
Island seas, tidal |
| 5 |
Singapore β Indian Ocean (Sunda St.) |
1,000 |
1.5 |
0.3 |
1.8 |
23 |
Strait navigation |
|
SE Asia Subtotal |
2,500 |
|
|
1.8 |
58 |
|
| 6 |
Indian Ocean β Madagascar (NE Monsoon) |
3,800 |
2.5 |
1.0 |
3.5 |
46 |
Monsoon + SEqC |
| 7 |
N Madagascar β S Madagascar (Mozambique Ch.) |
1,000 |
2.5 |
1.0 |
3.5 |
12 |
Mozambique Current |
| 8 |
S Madagascar β Durban coast |
800 |
2.5 |
1.5 |
4.0 |
8 |
Agulhas onset |
|
Indian Ocean Subtotal |
5,600 |
|
|
3.6 |
66 |
|
| 9 |
Durban β Cape of Good Hope (35Β°S) |
800 |
2.5 |
1.0 |
3.5 |
10 |
Agulhas + SW swell |
| 10 |
Cape β Enter S. Atlantic (35Β°Sβ30Β°S, west) |
600 |
2.0 |
0.3 |
2.3 |
11 |
Westerly transition |
|
Cape Rounding Subtotal |
1,400 |
|
|
2.9 |
21 |
|
| 11 |
Cape Town region β Equator (SE trades) |
2,000 |
2.5 |
1.0 |
3.5 |
24 |
Benguela + SE trades |
| 12 |
Equator β NE Brazil (SE/NE trades) |
1,800 |
2.5 |
1.0 |
3.5 |
22 |
SEqC + NBC |
| 13 |
NE Brazil β Caribbean |
1,500 |
2.5 |
1.5 |
4.0 |
16 |
NBC + NE trades |
| 14 |
Caribbean β Panama Canal |
1,000 |
2.5 |
0.5 |
3.0 |
14 |
Caribbean current |
|
Atlantic & Caribbean Subtotal |
6,300 |
|
|
3.5 |
76 |
|
|
GRAND TOTAL (Panama β Panama) |
~24,300 |
|
|
~3.2 |
335 |
|
Speeds in knots (nautical miles per hour). NM = nautical miles. Own Spd = vessel speed from kite/solar.
Current = estimated average favorable ocean current. Eff. Spd = Own Spd + Current.
Segment days = NM Γ· Eff. Spd, rounded.
π Summary by Ocean
| Ocean / Region |
Distance (NM) |
Avg Eff. Speed |
Time (Days) |
Key Currents & Winds |
| Pacific Ocean |
8,500 |
3.2 kts |
114 |
NE Trade Winds, N. Equatorial Current |
| Southeast Asian Seas |
2,500 |
1.8 kts |
58 |
Variable monsoon, tidal straits |
| Indian Ocean |
5,600 |
3.6 kts |
66 |
NE Monsoon, S. Equatorial Current, Mozambique & Agulhas Currents |
| Cape of Good Hope |
1,400 |
2.9 kts |
21 |
Edge of Agulhas, transition to westerlies |
| South & North Atlantic |
6,300 |
3.5 kts |
76 |
Benguela, S./N. Equatorial Currents, N. Brazil Current, Caribbean Current |
| TOTAL |
~24,300 |
~3.2 kts |
335 |
|
π Range of Outcomes
Best Case (~290 days)
- Perfect timing into Indian Ocean at start of NE Monsoon (November departure from SE Asia)
- Kite flies downwind >75% of the time
- Cape of Good Hope crossed in a 10-day weather window with minimal delay
- Favorable Agulhas leakage provides strong push into South Atlantic
- Average effective speed ~3.6 kts
Worst Case (~380 days)
- Miss the monsoon window, forcing 3β4 week waits in SE Asia or Indian Ocean
- Kite flies downwind only ~50% of the time (more beam reaches, less pure downwind)
- Cape of Good Hope requires multiple weather holds totaling 2β3 weeks
- Encounter eddies or counter-currents in the Atlantic
- Average effective speed ~2.8 kts
Most likely: ~310 β 350 days, with 330 days as the central estimate.
The Cape of Good Hope is the critical bottleneck β a few days' difference there
propagates through the entire Atlantic leg.
π The Cape of Good Hope Challenge
The most demanding segment of the entire voyage. At roughly 35Β°S, we are:
- North of the worst Roaring Forties β seas are typically 6β12 ft rather than 20β40 ft at 45β50Β°S.
- But not immune to Southern Ocean swells β long-period swells from distant storms can reach 15 ft even at 35Β°S. We may need to hove-to for 12β24 hours during the worst pulses.
- The current fight: The Agulhas Current flows southwest along the coast (helpful), but then retroflects eastward around 40Β°S. We need to exit the current system before it turns east, then catch the weaker southward/northward flows into the Atlantic.
- Wind transition: We pass from the SE Trades (blowing toward the Cape) through a zone of variable winds between the subtropical high and the westerlies. Kite may be intermittent here.
Strategy: Follow the South African coast as far as the Agulhas allows (~Durban to Cape Town),
then cut west into the South Atlantic during a weather window when the pressure gradient
gives us manageable westerly-to-northwesterly winds. With Starlink forecasting,
we can time this crossing to take advantage of passing frontal systems.
π
Optimal Seasonal Timing
Timing departure to align with seasonal wind patterns is critical:
| Month |
Location |
Conditions |
| Jan | Panama β Central Pacific | NE Trades steady; good start window |
| FebβMar | Central Pacific | NE Trades remain strong; ITCZ may be slightly south |
| Apr | Western Pacific | Trades still functional; approaching Philippines |
| MayβJun | Southeast Asian Seas | Transition to SW Monsoon; variable but navigable |
| JulβAug | Exit into Indian Ocean | β οΈ SW Monsoon blows against us here β may need to wait for NE Monsoon onset |
| SepβOct | Indian Ocean transit | Transition period; catch early NE Monsoon if timing works |
| NovβDec | Indian Ocean β Africa | NE Monsoon at full strength β ideal window! |
| Jan (Year 2) | Cape of Good Hope | Southern Hemisphere summer β best conditions for Cape rounding |
| FebβMar | South Atlantic | SE Trades strong; fast run to Brazil |
| Apr | Caribbean β Panama | Arrive before Atlantic hurricane season begins June 1 |
β οΈ Key timing risk: Arriving at the Indian Ocean too late (after NE Monsoon ends in March)
means either waiting nearly a year or pushing against the SW Monsoon. A January departure from Panama
targets an OctoberβNovember Indian Ocean crossing to catch the NE Monsoon.
π Tropical Cyclone Avoidance
With Starlink providing real-time forecast data, the vessel can detect and avoid cyclones days
in advance. Key considerations:
- Pacific typhoon season: MayβNovember. Route through the western Pacific should
aim to cross the Philippine Sea before peak typhoon months (AugustβOctober) or use Starlink
to thread between storms.
- Indian Ocean cyclone season: AprilβDecember (peak NovβApr). Our NE Monsoon
transit (OctβJan) overlaps with early cyclone season β Starlink routing keeps us north of typical
formation zones.
- Atlantic hurricane season: June 1 β November 30. We aim to be in the
South Atlantic (south of the equator) during peak Atlantic season, reaching the Caribbean only
after the season wanes in late November or having crossed earlier in the year.
- Mediterranean & South Pacific: Minimal tropical cyclone risk at our latitudes.
The vessel's ability to move 30β70 nautical miles per day gives it several hundred miles
of re-routing capability over a 3β5 day forecast window β more than enough to skirt
any tropical system.
π Expected Sea States
| Region |
Typical Wave Height |
Worst Expected |
Compliance |
| Pacific trade wind belt (10β20Β°N) | 3β6 ft | 10 ft (near ITCZ squalls) | β
Under 15 ft |
| Southeast Asian seas | 2β5 ft | 8 ft (monsoon transitions) | β
Under 15 ft |
| Indian Ocean (5β20Β°S) | 4β8 ft | 12 ft (cyclone swell) | β
Under 15 ft |
| Mozambique Channel | 4β8 ft | 14 ft (strong Agulhas interaction) | β
Usually under 15 ft |
| Cape of Good Hope (33β36Β°S) | 6β12 ft | 18 ft (strong frontal passage) | β οΈ Occasional exceedance β shelter or wait |
| South Atlantic trades | 4β8 ft | 12 ft | β
Under 15 ft |
| Caribbean / North Atlantic | 3β6 ft | 10 ft | β
Under 15 ft |
The only segment that consistently risks exceeding the 15-foot threshold is the
Cape of Good Hope rounding. By timing this passage for the austral summer
(DecemberβFebruary) and using weather windows between frontal systems, we can minimize
exposure to the largest seas.
β±οΈ How Does This Compare?
| Vessel / Method |
Avg Speed |
Circumnavigation Time |
Notes |
| Sailing yacht (typical) |
6β8 kts |
~100β120 days |
Fast cruising catamaran |
| Sailing yacht (conservative) |
4β5 kts |
~150β200 days |
Monohull, full-time crew |
| ε€ͺι³θ½/ι£ηζ΅·εΊ (this analysis) |
~3.2 kts |
~330 days |
No crew fatigue, continuous motion |
| Slow expedition vessel |
2β3 kts |
~350β450 days |
Small engine, weather-dependent |
| Clipper ship (historical) |
5β8 kts |
~80β100 days |
Optimal conditions, experienced crew |
Our seastead performs comparably to a conservatively sailed monohull,
without any fossil fuel consumption for propulsion. The key advantage:
no crew fatigue β the vessel can maintain continuous motion
24/7 for months without rest, unlike a small human-crewed sailboat.
π¬ Sensitivity Analysis
Small changes in assumptions can significantly affect the total time:
| Parameter Change |
Impact on Total Time |
Revised Estimate |
| Baseline (central estimate) |
β |
~330 days |
| Kite flies 80% of time (vs. 60%) |
β30 days |
~300 days |
| Kite flies 40% of time (vs. 60%) |
+40 days |
~370 days |
| Average current 0.5 kt stronger |
β25 days |
~305 days |
| Average current 0.5 kt weaker |
+30 days |
~360 days |
| Cape rounding takes 15 extra days (weather holds) |
+15 days |
~345 days |
| Miss monsoon window by 3 weeks |
+21 days |
~351 days |
Bottom line: Even in the pessimistic scenario, the circumnavigation completes in
roughly 13β14 months. In the optimistic scenario, under 10 months. The kite's
effectiveness and seasonal timing are the two biggest variables.
π Eddy Currents & Fine-Scale Routing
Ocean mesoscale eddies (rotating water masses 50β300 km across) can provide bonus speed
of 0.5β2 knots when favorable, or significant drag when unfavorable. With Starlink and
satellite altimetry data (freely available from missions like Sentinel-6), real-time
sea surface height maps reveal eddy locations and strengths.
How We Exploit Eddies
- Western boundary currents (Gulf Stream, Kuroshio, Agulhas, Brazil Current)
are intense and often have favorable eddies spinning off their landward side. Riding these
can add 1β3 knots for days at a time.
- Tropical instability waves in the Pacific and Atlantic create alternating
eddy pairs along the equator. Smart routing can pick up westward-flowing eddy patches.
- The Agulhas Retroflection sheds large warm-core eddies into the South Atlantic.
Timing our Cape crossing to catch one of these could provide a significant boost (2+ knots
for a week) into the Atlantic.
- Mediterranean outflow and other sub-surface features generally don't affect
a surface vessel significantly.
π‘ Eddy exploitation adds an estimated 5β10% speed bonus (reducing time by 15β30 days)
for a vessel with real-time routing capability. This is already partially accounted for in
our "optimistic" scenario.
Final Estimate: Westward Circumnavigation
~330 days
290 β 380 days (80% confidence interval)
~24,300 nautical miles β’ ~3.2 knots average effective speed
β’ Pacific: 114 days | SE Asia: 58 days | Indian Ocean: 66 days
| Cape: 21 days | Atlantic: 76 days