The Eratosthenes Experiment International collaboration A short History The size of the Earth was determined already more than 2000 years ago. This is quite impressive, but was due to a clever observation. The director of the famous library in Alexandria in Egypt, the geographer Eratosthenes (about 276-195 BC.) did the historic achievement. Odense 26.september 2005 Eratosthenes had learned a fascinating fact about the city of Syene in southern Egypt, not far from Aswan: When the Sun was at its highest in the sky in this city on the longest day of the year (today we call it summer solstice), the Sun did not cast any shadows. Actually, the Sun shined into deep wells. The story says that nobody dared to stare into the wells since they could become blinded by the intense light reflected by the water deep down. Odense 26.september 2005 In Syene the Sun therefore had to be in the zenith at this time. In Alexandria, further north in Egypt, Eratosthenes knew from his own experience that the shadow at the same time was 7.2 degrees (see drawings to the right). He could then calculate the circumference of the earth by this simple ratio: Distance between Syene and Aleksandria circumference of the earth = measured angle 360° Odense 26.september 2005 Eratosthenes map Odense 26.september 2005 He could not measure the distance between the cities directly, but estimates of people travelling between the cities and the time they spent, gave a distance of about 5000 stadions. The circumference of the Earth therefore had to be 250 000 stadia. circumference of the earth = 5000*360/7.2 = 250000 A stadium (plural stadia) is a Greek measure of distance equal to 600 Greek feet. Today we don't know the exact length of one stadium. Opinions vary about how long it actually was, with estimates varying from 154 to 215 metres. If we choose 160 m we get that 250 000 stadia correspond to 40000 kilometers. This is close to the correct value, which is 40 074 kilometers! Anyway, the method is correct and can be applied even today to estimate the size of our Earth Odense 26.september 2005 How do we do it today? Odense 26.september 2005 SUN tanα = b/a You measure the solar shadow angle at solar noon a α b Odense 26.september 2005 The GLOBE way! Odense 26.september 2005 And use the result from another school and do the calculations School 1 X X School 2 Distance between latitudes Odense 26.september 2005 Both schools with shadow to the North: D/C = (α - β)/360 Find C. Sun rays Both schools with shadow to the South: D/C = (β - α)/360 Find C. One school with shadow to the North and one school with shadow to the South: D/C = (α + β)/360 Find C. N α β α-β α The Equator β S The Earth Odense 26.september 2005 When and how Register for the experiment Find a partner school Conduct Experiment at Wednesday May 25 +- 2 days Wednesday September 21 +-2 days After the Experiment you register your results Odense 26.september 2005 Results 28 countries 98 schools Average value 41179 km Odense 26.september 2005 Hungary Odense 26.september 2005 Romania Odense 26.september 2005 Deutsche Schule Abu Dhabi Vereinigte Arabische Emiratea Odense 26.september 2005 Puerto Rico Odense 26.september 2005 The Czech Republic Odense 26.september 2005 South Korea Odense 26.september 2005 Where to register www.naturfagsenteret.no/fysikk/eratosthenes/index.html or www.globe-europe.org Join the project! Odense 26.september 2005 FYSIKKÅRET ER TID FOR FYSIKKSTUNT! Odense 26.september 2005 POTETKANON Odense 26.september 2005 PÅ STRAM LINE Odense 26.september 2005 DEI UNGE ER BEST! Odense 26.september 2005 Bøndar og fysikk Odense 26.september 2005 Bemanna vannrakett Odense 26.september 2005 LYKKE TIL! Odense 26.september 2005