Voyage 1
Trip Itinerary and approximate latitude: Havana, Cuba to London, England
Travel time: 9 Days
Direction traveling: North East
Were you successful? Yes
How many attempts? 3
How were you successful? Focused on winds and direction
What winds did you take advantage of or compete with during your travel? Prevailing Westerlies
Voyage 2
Trip Itinerary and approximate latitude: San Francisco, United States to Sydney, Australia
Travel time: 13 Days
Direction traveling: South West
Were you successful? Yes
How many attempts? 4
How were you successful? I payed attention to the winds
What winds did you take advantage of or compete with during your travel? I took advantage of the Trade Winds and competed with the Prevailing Westerlies
Voyage 3
Trip Itinerary and approximate latitude: Lima, Peru to Cape Town, South Africa
Travel time: 15 Days
Direction travelling: East
Were you successful? Yes
How many attempts? 2
How were you successful? Payed attention to winds and Straits of Magellan
What winds did you take advantage of or compete with during your travel? I took advantage of the Prevailing Westerlies
Thursday, November 20, 2008
Monday, November 17, 2008
Tuesday, November 11, 2008
Ozone
The ozone is a layer inside the stratosphere that protects Earth from UV radiation. Without the ozone, we would all be burned due to UV radiation. Ozone depletion is when a hole in the ozone appears. This is a sign of global warming caused by smog and other gases.
Greenhouse Effect
The greenhouse effect is when light from the sun travels into a glass like containment. The light gets into the glass like containment and tries to get back out. The glass protects the light so it will never come out until the light is absorbed. This is what happens with atmosphere. The sunlight travels to Earth and tries to go back out. But the troposphere acts like the glass of the Earth. The sunlight is either absorbed into the Earth, goes back out to space, or gets absorbed into gas molecules.
Tuesday, November 4, 2008
London Type Smog
London-type smog was caused mainly by air pollution due to combustion of coal and emission of sulphur dioxide (SO2) and dust. Such pollution mixed with fog can produce droplets of sulphuric acid (H2SO4) suspended in the air. When in 1952, in London, the concentration of SO2 during a smog event exceeded 3.5 mg per 1m3 of the air (or 3500 ug per 1m30), it caused massive cases of decease(Note: 1mg is 0.001g; another unit is 1 ug which is equal to 0.000001 g. So 1g=1000 mg or 1000000 ug).
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