八月二十六號 天氣晴
兩棵玉米還有一棵待開葉 一棵待結果實的茄子
一棵蘿蔔 與一棵花生
喔 忘了說 這是開心農場英文版中種的
不曉得有兩個版本 開了中文與英文版
- 8月 26 週三 200908:16
菜園記
八月二十六號 天氣晴
兩棵玉米還有一棵待開葉 一棵待結果實的茄子
一棵蘿蔔 與一棵花生
喔 忘了說 這是開心農場英文版中種的
不曉得有兩個版本 開了中文與英文版
- 8月 25 週二 200911:57
玉米園
好，我承認。
我承認一開始覺得這個遊戲很無聊。
加入facebook不知道要幹麻，功能不就跟無名、msn space大同小異嗎？
一直到我開始種菜菜….哈…天呀…我好像被菜園制約了，有時會上來看菜是不是好好地。
除草、除蟲、澆水，但最大的快感是去偷別人的菜菜….
好開心唷
其實內心真正想做的是一位快樂的農夫
科科...誰有facebook +我 +我 吧~
- 7月 22 週三 200920:45
太陽咬一口 月亮說yummy
好神奇 書本上說的 跟現實生活中遇到一樣新鮮
太陽 月亮 地球 連成一條線的月全蝕
今天一上班 其實我一直找網站 看哪邊有live演出
真的是分秒必爭呀 用google找不到印度哪有live網站
又找到一個日本網站 沒想到還要安裝有的沒的程式
天呀 我會不會錯過 才去茶水間洗手
沒想到 同事門一個一個在外面
其中一個去現場拿了焊接護目鏡
就這樣大家輪著看月吞太陽的畫面
好在老闆今天不在納
好驚奇唷
http://svs.gsfc.nasa.gov/vis/a010000/a010400/a010452/index.html
Nasa網站也有好多資料 也有以前月偏食畫面唷
- 10月 24 週五 200823:36
黑暗騎士 Joker小丑
裡面中的小丑 演得讓我不寒而慄
真的是很變態 不管他在陳述他小時被受虐或者他虐人也好
我都會避免看這些可怕的畫面
這樣還要看什麼整片灰灰暗暗 說真的我看到我快睡著
就這樣看到一半先跑去睡一下
當他要燒毀所有搶來的錢
人性大考驗要引爆船時
沒想到我對小丑內心的變態感到興趣
很特別的變態 說得話好有哲理
馬上google一下
轉載: http://ordinarycool.pixnet.net/blog/post/20839108
Lighting a match, preparing to burn the pile of bills) You see, I am a guy with a simple taste. I enjoy dynamite, gunpowder, and gasoline. And do you know what they have in common? They are cheap! And you, all you care about is money.--品味單純...他說出口卻很有味道
Do you want to know why I use a knife? You see, guns are too fast. You can’t savor all the little….emotions. In their last moments, people show you what they’re really like. So, in a sense, I know your friends better than you did. Would you like to know which of them were coward?--人性考驗...說得是..
最後他成功搞瘋了人
這樣的人能不可怕嗎?
- 10月 19 週日 200820:06
生活的重心是....
迷失在浩瀚無邊黑暗海域之中
夜的寂靜 就連鬧鐘滴答滴答聲都可以這麼清析
阿娘威 我好無聊唷 晚上到底要幹麻好
電視挑來挑去 沒幾台可看 況且又不愛看八點檔
我到底能幹麻的好呀
日前好不容易看完 浪漫滿屋
還被妙仔笑說 這幾百年前的韓劇妳還在看
頓時失去重心的我 想想還有什麼可以打發的
說時來得碰巧 哥哥送我四本新書
看來可以讓我打發好一陣子了
這個....我不知道我能看得懂多少....應該看不到兩頁 就會進入夢鄉裡吧
- 1月 09 週三 200823:04
風剪-wind stress
好奇 可以殺死好多隻貓 
奇怪 為什麼會有這種要殺貓的說法
剛剛看空中浩劫-哥倫比亞052班機 提到"風剪" 光是看中文就讓我很好奇了 我卻聽成...wind share?! 真的是耳朵有問題
於是
http://www.answers.com/topic/wind-stress?cat=technology
Wind stress
The drag or tangential force per unit area exerted on the surface of the Earth by the adjacent layer of moving air. Erosion of ground surfaces and the production of waves on water surfaces are manifestations of wind stress. Surface wind stress determines the exchange of momentum between the Earth and the atmosphere and exerts a strong influence on the typical variation of wind through the lowest kilometer of the atmosphere. Estimated values of the surface wind stress range up to several dynes per square centimeter (0.1 pascal), depending on the nature of the surface and the character of the adjacent airflow. See also Meteorology.
Significant stresses arise within the lower atmosphere because of the strong shear of the wind between the slowly moving air near the ground and the more rapidly moving air a kilometer above and because of the turbulent nature of the airflow in this region. The turbulent eddies referred to here have characteristic dimensions ranging up to a few hundreds of meters.
Wind pressure is the force exerted by the wind per unit area of solid surface exposed normal to the wind direction and is also known as dynamic pressure. In contrast to shearing stresses, the wind pressure arises from the difference in pressure between the windward and lee sides of the exposed surface. Wind pressure thus represents a substantial force when the wind speed is high. See also Wind.
The drag or tangential force of the wind on the sea is expressed in units of dynes per square centimeter or micronewtons per square meter but is normally taken to represent the mean drag over an undefined area, perhaps several kilometers square, containing many waves. It is usually related to an appropriate time and space average of the wind near the sea surface (at 10 m above the mean level, for example).
The drag coefficient over the sea is an important quantity in both meteorology and oceanography since it relates the wind speed to the drag, which generates ocean waves, drives the ocean currents, and sets the scale of the atmospheric turbulence that transfers water vapor and heat from the ocean to the atmosphere to provide the energy for clouds and weather systems. The drag coefficient of the sea surface depends on the wave field and on the turbulent structure of the flow in the air and the water. Present knowledge of the complicated fluid mechanics involved is not sufficient to allow theoretical calculation of it. See also Atmospheric general circulation; Maritime meteorology; Ocean circulation; Ocean waves.
There is substantial agreement that the drag of the wind on the sea is small relative to that of a fixed soil surface with the same geometry. It is largely independent of the fetch and so seems to depends less on the larger waves than on the short waves and ripples. Surface-active agents, which affect the shortest waves, may therefore be important.
另一個
http://oceanworld.tamu.edu/resources/ocng_textbook/chapter04/chapter04_05.htm
The wind, by itself, is usually not very interesting. Often we are much more interested in the force of the wind, or the work done by the wind. The horizontal force of the wind on the sea surface is called the wind stress. Put another way, it is the vertical transfer of horizontal momentum. Thus momentum is transferred from the atmosphere to the ocean by wind stress. Wind stress T is calculated from:
T = ñ CD U210
壓力還可以算出來耶…傑克這是太神奇的有趣呀!!!
奇怪 為什麼會有這種要殺貓的說法
剛剛看空中浩劫-哥倫比亞052班機 提到"風剪" 光是看中文就讓我很好奇了 我卻聽成...wind share?! 真的是耳朵有問題
於是
http://www.answers.com/topic/wind-stress?cat=technology
Wind stress
The drag or tangential force per unit area exerted on the surface of the Earth by the adjacent layer of moving air. Erosion of ground surfaces and the production of waves on water surfaces are manifestations of wind stress. Surface wind stress determines the exchange of momentum between the Earth and the atmosphere and exerts a strong influence on the typical variation of wind through the lowest kilometer of the atmosphere. Estimated values of the surface wind stress range up to several dynes per square centimeter (0.1 pascal), depending on the nature of the surface and the character of the adjacent airflow. See also Meteorology.
Significant stresses arise within the lower atmosphere because of the strong shear of the wind between the slowly moving air near the ground and the more rapidly moving air a kilometer above and because of the turbulent nature of the airflow in this region. The turbulent eddies referred to here have characteristic dimensions ranging up to a few hundreds of meters.
Wind pressure is the force exerted by the wind per unit area of solid surface exposed normal to the wind direction and is also known as dynamic pressure. In contrast to shearing stresses, the wind pressure arises from the difference in pressure between the windward and lee sides of the exposed surface. Wind pressure thus represents a substantial force when the wind speed is high. See also Wind.
The drag or tangential force of the wind on the sea is expressed in units of dynes per square centimeter or micronewtons per square meter but is normally taken to represent the mean drag over an undefined area, perhaps several kilometers square, containing many waves. It is usually related to an appropriate time and space average of the wind near the sea surface (at 10 m above the mean level, for example).
The drag coefficient over the sea is an important quantity in both meteorology and oceanography since it relates the wind speed to the drag, which generates ocean waves, drives the ocean currents, and sets the scale of the atmospheric turbulence that transfers water vapor and heat from the ocean to the atmosphere to provide the energy for clouds and weather systems. The drag coefficient of the sea surface depends on the wave field and on the turbulent structure of the flow in the air and the water. Present knowledge of the complicated fluid mechanics involved is not sufficient to allow theoretical calculation of it. See also Atmospheric general circulation; Maritime meteorology; Ocean circulation; Ocean waves.
There is substantial agreement that the drag of the wind on the sea is small relative to that of a fixed soil surface with the same geometry. It is largely independent of the fetch and so seems to depends less on the larger waves than on the short waves and ripples. Surface-active agents, which affect the shortest waves, may therefore be important.
另一個
http://oceanworld.tamu.edu/resources/ocng_textbook/chapter04/chapter04_05.htm
The wind, by itself, is usually not very interesting. Often we are much more interested in the force of the wind, or the work done by the wind. The horizontal force of the wind on the sea surface is called the wind stress. Put another way, it is the vertical transfer of horizontal momentum. Thus momentum is transferred from the atmosphere to the ocean by wind stress. Wind stress T is calculated from:
T = ñ CD U210
壓力還可以算出來耶…傑克這是太神奇的有趣呀!!!
- 1月 08 週二 200813:32
騎鐵馬的利與弊
最近可能是被電視洗腦的多....還是真的反應現在目前市場
麵粉 沙拉油 奶粉 就連水果也是誇張的漲價....
只有遠傳說的是..."你的薪水沒有漲"
為什麼不鏽鋼一直降...連人客也很愛用原料下降來殺價
每加油一次 我就心痛一次 阿~~~為什麼油 夭壽貴 NT30.1/per公升
害得妙仔差一點去喝汽油
雖然 我是騎歐兜邁 從家裡到公司只要兩分鐘
但是身為普通老百姓的我 深深覺得什麼都漲的日子真得是很難過活耶
開始認真想過騎鐵馬....曾經有過跟家人一起騎著14km...
這不到一公里的路程應該不算什麼才對
不過.....好像有點難
首先 我要七早八早起床 還沒騎到公司 我可能那天就累死了 (太久沒運動的後遺症)
再者 要是有人客來 總不能穿著制服短裙外加高跟鞋騎著鐵馬吧 這太ㄅ一ㄤ、 那我包包怎麼背呀
再來 晚上回家怎麼辦?! 這邊是工業區 騎著騎著被外勞拉去一起喝酒怎麼辦?!
坦白說 晚上騎車好恐怖唷 
且只有我一個人耶
且只有我一個人耶好吧....想想就好
還是平常六日騎鐵馬當休閒運動好了