Manila Galleon Voyages


Henry F. Diaz
NOAA/ESRL Physical Sciences Division

Science Writer: Susan Bacon
University of Colorado
Astrolabe

Virtual Voyages

To learn what climatic impacts could be contributing to longer voyages, the team constructed virtual voyages, in which a computer program sailed a ship with the same build and cargo as one of the historical galleons along the historical route, but used climate data measured during the last 50 years to define the winds and storms the virtual ships encountered.

Careful examination of the climate patterns that slowed the ships down or speeded them up showed that the primary explanation for slow voyages was the strength of the southwest winds the ships encountered when arriving in Manila. Traveling eastward to Mexico, the ships rode on the westerly winds. Returning west, the ships would sail with the northeast trade winds.

Link to Figure 3 Image Figure 3.  Wind composites for the 9 slowest and 9 fastest "virtual voyages" between Acapulco and the Philippines. Fast voyages are made when the southwest monsoon trough (dark blue/purple area) is pushed southward, allowing the ships to reach the Strait of San Bernadino with the trade winds. When the monsoon trough is pushed northward, winds are unfavorable, thereby delaying the approach to the Philippines.
The trip west depended critically on the circulation over the western Pacific, and was key in determining the total length of the journey. With stronger trade winds, the ships had a straight shot. But if the monsoon trough moved up and got in the way of the trade winds, the ships would have been slowed considerably.
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