1th of June 2011
Melbourne
I arrived early this morning after a 22 hour flight straight from London with a quick fuel stop in Hong Kong. It was a little weird to disembark the Boeing 474 leaving your luggage on board heading for the exit and then re-enter after one more serious security check from the Chinese authorities. Seats I had to changes as well. Second place was a little better, with a skinny girl to the left, so more space for me.
...weiterlesen "Melbourne Friday – Monday"

Category description

Rain is liquid precipitation, as opposed to non-liquid kinds of precipitation such as snow, hail and sleet. Rain requires the presence of a thick layer of the atmosphere to have temperatures above the melting point of water near and above the Earth’s surface. On Earth, it is the condensation of atmospheric water vapor into drops of water heavy enough to fall, often making it to the surface. Two processes, possibly acting together, can lead to air becoming saturated leading to rainfall: cooling the air or adding water vapor to the air. Virga is precipitation that begins falling to the earth but evaporates before reaching the surface; it is one of the ways air can become saturated. Precipitation forms via collision with other rain drops or ice crystals within a cloud. Rain drops range in size from oblate, pancake-like shapes for larger drops, to small spheres for smaller drops.
Moisture moving along three-dimensional zones of temperature and moisture contrasts known as weather fronts is…