Wednesday, August 19, 2009
SAs tomorrow .___. ♥
7:13 PM
boooooooo SAs tomorrow! plus after that we still have oral, both english and chinese, LIT PT O: and french controle! That is so depressing!! hahaa i finally blogged on the 110 blog after stopping for O; 4 months?!
i love dramas. as in, the shows. japanese/korean/taiwanese/english dramas are all nice! but real-life-drama is .____. ewww. life should just stay normal and fun and happy! (: and maybe i should try BOLLYWOOD 8D wait. is that how you spell it? and today, i went to this gifts shop in coro to buy presents for my guides seniors (DD:) but all of them were SO EX LAH WTFREAK.
oh and i just realised i owe wanling $1 (wanling!!! how did it get to one dollar?!) for saying too many ohmygods DD: boo. got back lit FA today! the 'evacuee' one :D quite satisfying. so hopefully, tomorrow's lit SA won't be so bad....? anyway, i am just concentrating on history and geog. but what exactly is a metaphor? i still am not sure
ohhh no rs today, we got chosen for roleplay next week .___. it's not like our interview questions were good; it was just because we were 2nd to go up to present! LOL WHO IS GOING TO BE OUR INTERVIEWEE?! limin. lewin?
oh no. let me try to remember what i mugged for geog - the convectional and relief rain part!
i don't care. after SAs today, must go relaxxxxx!
CONVECTIONAL RAIN
On a hot day, air in contact with the warm ground is heated up by conduction. The warm air expands and becomes lighter than the surrounding air, and is said to be unstable. This unstable air, which can hold a lot of moisture, rises in a convectional current. As it rises to great heights, it cools. Further cooling after saturation at dew-point causes the water vapour to condense into water droplets. The water droplets then coalesce to form towering cumulonimbus clouds. When the water droplets become too heavy to be suspended, convectional rain falls.
RELIEF RAIN
When the onshore air is forced to rise up the mountain slope, the rising air expands and cools. Further rising and cooling causes the water vapour to condense into water droplets to form clouds. When the water droplets become too heavy to be suspended, relief rain falls on the windward side of the mountain. No or little rain falls on the leeward side, as the wind would have lost almost all of its moisture by the time it reaches the leeward side. Hence, the leeward side is also known as the rainshadow area.
oh wheee! done. (: and it's correct phew. okay better go mug now!
GOOD LUCK FOR YOUR SAs!
;cherlene.