7. Bijkomend materiaal

Hoofdstuk 2. Windgedreven oppervlaktestromen

Wil je meer leren?

cyclone




Het Corioliseffect

earth temperature




Heersende winden (in het Engels)

southern ocean storm




De zuidelijke oceaan (in het Engels)

Antwoorden (in het Engels)

18th century schooner in new york harbour 1. Franklin's question: why the big difference?   Why did the mail ships from London to New York take 2 weeks longer to reach America than the merchant ships sailing from Falmouth to Rhode Island?

Answer:   The mail ships from London to New York sailed further south than the ships from Falmouth to Rhode Island. Approaching America the mailships sailed against the Gulf Stream, while the ships to Rhode Island avoided this, and may even have had help from the continuation of the cold currents south of Nova Scotia.
18th century schooner in new york harbour 2. How can temperature measurements help?  

Answer:   The difference across the front can be as much as 4 °C. This is easy to detect even with very simple bucket measurements. By knowing the average temperature of Gulf Stream water in a particular season, navigators can determine whether or not they are in the current. If they are sailing to America and want to avoid the Gulf Stream, they can plot a more northerly course. If they are sailing from America they can plot a more southerly course and get some help from the current.

Oefeningen / Werkbladen

Plastic ducks in a line on the waves




Oefening c02-01: Het verhaal van het badkuipspeelgoed - feit of fictie?