December 7,2007
你不乖就不娶你啦!
老廣,是我大學同學,當年他是從香港來台灣念書的「僑生」,學校畢業後他就載譽回港了。以後在香港、大陸擔任高級經理,現移居加拿大卑诗省的“埠仔”“高桂林”市。他不但口才便給,文筆也非常犀利,每每跟他寫信,讓我常常不知如何接詞。
自從此兄到了卑诗省後,他經常來E-mail,有時候附上精彩照片,讓同學們分享他的生活點滴,也告訴我他的私生活趣事(他向來口無遮攔又鹹濕)是益友中的損友,不過,他心地非常善良,又孝順(一直想把高堂從香港接到加拿大奉養),前幾天E-mail告訴我,卑诗省下雪了,今天他又來信說,雪融了!
為什麼雪融的那麼快,真是怪事,原來「菠蘿快車」(Pineapple Express)熱帶風暴的影響。我這學歷史的老同學,這幾天從飄雪、積雪到雪融,他都拍了照片存檔並給寄給我,從沒有在雪地生活的我,看到雪景,雖然未身臨其境,但仍感到興奮異常。
因此我問老同學照片可以貼在我部落格嗎?他說可以,但不能把他的名字和照片曝光,不然,「你不乖就不娶你啦!」呵、呵、呵!親愛的老廣,什麼跟什麼嘛!我只是要照片。
為什麼雪融的那麼快,真是怪事,原來「菠蘿快車」(Pineapple Express)熱帶風暴的影響。我這學歷史的老同學,這幾天從飄雪、積雪到雪融,他都拍了照片存檔並給寄給我,從沒有在雪地生活的我,看到雪景,雖然未身臨其境,但仍感到興奮異常。
因此我問老同學照片可以貼在我部落格嗎?他說可以,但不能把他的名字和照片曝光,不然,「你不乖就不娶你啦!」呵、呵、呵!親愛的老廣,什麼跟什麼嘛!我只是要照片。
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回應文章 
我不住在多伦多啊,宝贝儿。我的蜗居是在卑诗省的“埠仔”“高桂林”市。
对,老广很“咸湿”,可是,任何一个正常的男人都应该咸湿。不咸湿的男人只有以下几种:
1) 还没出生的;
2) 已死掉的;
3) 搞“基”的; 还有
4) 性无能的。
(如果你还想到甚麽别的,告诉我吧。)
再说,如果你早知道我咸湿的话,你不就“甚麽跟甚麽嘛”我啰,何止“我只是要照片”而已?
其实女人也都非常咸湿,不然的话,又怎麽会有“饮食男,女人之大欲也”的这句名言!?
我没有“戴”誉回港,我只是带着一颗破碎的心回去而已矣。
被你这一搞,老广的脸儿都不知道要往哪儿放啦!好啦,好啦,我娶你啦!
对,老广很“咸湿”,可是,任何一个正常的男人都应该咸湿。不咸湿的男人只有以下几种:
1) 还没出生的;
2) 已死掉的;
3) 搞“基”的; 还有
4) 性无能的。
(如果你还想到甚麽别的,告诉我吧。)
再说,如果你早知道我咸湿的话,你不就“甚麽跟甚麽嘛”我啰,何止“我只是要照片”而已?
其实女人也都非常咸湿,不然的话,又怎麽会有“饮食男,女人之大欲也”的这句名言!?
我没有“戴”誉回港,我只是带着一颗破碎的心回去而已矣。
被你这一搞,老广的脸儿都不知道要往哪儿放啦!好啦,好啦,我娶你啦!
Posted by 老广
at December 8,2007 03:20
親愛的老廣:
哈哈哈~~我就機(用廣東話唸)道,你性本善啦!我舉雙手投降了!
好啦,我把您住的地方搬回卑诗省的“埠仔”“高桂林”市。
Posted by 秀堂
at December 9,2007 00:27
咁就乖豬豬嘞. 妳咁乖, 我「鍚」哂妳啦.順便改埋第二段 E-mail 嗰個 1 字啦. 同一段裏仍把尾巴留在多倫多? (妳公司請人做「校對」嗎? 我想應徵啊.)
妳昨晚睡得太晚了, 太晚睡對妳的精神固然不好, 對於皮膚更無好處. 早睡早起精神好之外, 皮膚更會「又白又滑」(用廣東東莞口音來讀更佳 -- 我可不是東莞人)呢.
我人雖老但未珠黃, 就未必無因者也.
Posted by 老广
at December 11,2007 14:25
好啦!親愛的老廣,你的眼力果真不錯!要娶我?我要回家問我媽媽還有先生。
Posted by 秀堂
at December 11,2007 15:02
Fun time 已过,现在只谈“正经”事:
以下是有关“菠萝快车”(Pineapple Express)的一点资讯,让你细心参考。(Source: Wikipedia)
Pineapple Express is a non-technical, shorthand term popular in the news media for a meteorological phenomenon which is characterized by a strong and persistent flow of atmospheric moisture and associated heavy rainfall from the waters adjacent to the Hawaiian Islands and extending to any location along the Pacific coast of North America. The Pineapple Express is driven by a strong, southern branch of the Polar jetstream and is usually marked by the presence of a surface frontal boundary which is typically either slow or stationary, with waves of low pressure traveling along its axis. Each of these low pressure systems brings enhanced rainfall.
The conditions are often created by the Madden-Julian oscillation, an equatorial rainfall pattern which feeds its moisture into this pattern. They are also present during an El Niño episode.
The combination of moisture-laden air, atmospheric dynamics, and orographic enhancement resulting from the passage of this air over the mountain ranges of the West Coast causes some of the most torrential rains to occur in the region. Many Pineapple Express events follow or occur simultaneously with major arctic troughs in the Northwestern United States, often leading to major snowmelt flooding with warm, tropical rains falling on frozen, snow laden ground. Examples of this are the December 1964 Pacific Northwest flood and the Willamette Valley Flood of 1996.
A Pineapple Express battered Southern California from January 7 through January 11, 2005. This storm was the biggest to hit Southern California since the El Niño of 1998. The storm caused mud slides and flooding, with one desert location just north of Morongo Valley receiving about 9 inches of rain, and some locations on south and southwest-facing mountain slopes receiving spectacular totals: San Marcos Pass, in Santa Barbara County, received 24.57 inches (624 mm), and Opid's Camp in the San Gabriel Mountains of Los Angeles County was deluged with 31.61 inches (803 mm) of rain in the five day period.
The unusually intense rain storms that hit south-central Alaska in August of 2006 were termed "Pineapple Express" rains locally.
The Puget Sound region from Olympia, Washington to Vancouver, BC received several inches of rain per day in November 2006 from a series of successive Pineapple Express storms that caused massive flooding in all major regional rivers and mudslides which closed the mountain passes. These storms included heavy winds which are not usually associated with the phenomenon. Regional dams opened their spillways to 100% as they had reached full capacity due to rain and snowmelt. Officials referred to the storm system as "the worst in a decade" on November 8, 2006. Portions of Oregon were also affected, including over 14 inches in one day at Lee's Camp in the Coast Range, while the normally arid and sheltered Interior of British Columbia received heavy coastal-style rains.
In British Columbia especially, Pineapple Express systems typically generate heavy snowfall in the mountains and Interior Plateau, which often melts rapidly because of the warming effect of the system. After being drained of their moisture, the tropical air masses reach the Canadian Prairies as a Chinook wind or simply "a Chinook", a term which is also synonymous on the Coast with the Pineapple Express.
The San Francisco Bay Area is another locale along the Pacific Coast which is occasionally affected by a Pineapple Express. When it visits, the heavy, persistent rainfall typically causes flooding of local streams as well as urban flooding. In the decades before about 1980, the local term for a Pineapple Express was "Hawaiian Storm". During the second week of January, 1952, a series of "Hawaiian" storms swept into Central California, causing widespread flooding around the Bay Area. The same storms brought a blizzard of heavy, wet snow to the Sierra Nevada Mountains, notoriously stranding the streamliner City of San Francisco on January 13. The greatest flooding in Northern California since the 1800s occurred in 1955 as a result of a series of Hawaiian storms, with the greatest damage in the Sacramento Valley around Yuba City.
以下是有关“菠萝快车”(Pineapple Express)的一点资讯,让你细心参考。(Source: Wikipedia)
Pineapple Express is a non-technical, shorthand term popular in the news media for a meteorological phenomenon which is characterized by a strong and persistent flow of atmospheric moisture and associated heavy rainfall from the waters adjacent to the Hawaiian Islands and extending to any location along the Pacific coast of North America. The Pineapple Express is driven by a strong, southern branch of the Polar jetstream and is usually marked by the presence of a surface frontal boundary which is typically either slow or stationary, with waves of low pressure traveling along its axis. Each of these low pressure systems brings enhanced rainfall.
The conditions are often created by the Madden-Julian oscillation, an equatorial rainfall pattern which feeds its moisture into this pattern. They are also present during an El Niño episode.
The combination of moisture-laden air, atmospheric dynamics, and orographic enhancement resulting from the passage of this air over the mountain ranges of the West Coast causes some of the most torrential rains to occur in the region. Many Pineapple Express events follow or occur simultaneously with major arctic troughs in the Northwestern United States, often leading to major snowmelt flooding with warm, tropical rains falling on frozen, snow laden ground. Examples of this are the December 1964 Pacific Northwest flood and the Willamette Valley Flood of 1996.
A Pineapple Express battered Southern California from January 7 through January 11, 2005. This storm was the biggest to hit Southern California since the El Niño of 1998. The storm caused mud slides and flooding, with one desert location just north of Morongo Valley receiving about 9 inches of rain, and some locations on south and southwest-facing mountain slopes receiving spectacular totals: San Marcos Pass, in Santa Barbara County, received 24.57 inches (624 mm), and Opid's Camp in the San Gabriel Mountains of Los Angeles County was deluged with 31.61 inches (803 mm) of rain in the five day period.
The unusually intense rain storms that hit south-central Alaska in August of 2006 were termed "Pineapple Express" rains locally.
The Puget Sound region from Olympia, Washington to Vancouver, BC received several inches of rain per day in November 2006 from a series of successive Pineapple Express storms that caused massive flooding in all major regional rivers and mudslides which closed the mountain passes. These storms included heavy winds which are not usually associated with the phenomenon. Regional dams opened their spillways to 100% as they had reached full capacity due to rain and snowmelt. Officials referred to the storm system as "the worst in a decade" on November 8, 2006. Portions of Oregon were also affected, including over 14 inches in one day at Lee's Camp in the Coast Range, while the normally arid and sheltered Interior of British Columbia received heavy coastal-style rains.
In British Columbia especially, Pineapple Express systems typically generate heavy snowfall in the mountains and Interior Plateau, which often melts rapidly because of the warming effect of the system. After being drained of their moisture, the tropical air masses reach the Canadian Prairies as a Chinook wind or simply "a Chinook", a term which is also synonymous on the Coast with the Pineapple Express.
The San Francisco Bay Area is another locale along the Pacific Coast which is occasionally affected by a Pineapple Express. When it visits, the heavy, persistent rainfall typically causes flooding of local streams as well as urban flooding. In the decades before about 1980, the local term for a Pineapple Express was "Hawaiian Storm". During the second week of January, 1952, a series of "Hawaiian" storms swept into Central California, causing widespread flooding around the Bay Area. The same storms brought a blizzard of heavy, wet snow to the Sierra Nevada Mountains, notoriously stranding the streamliner City of San Francisco on January 13. The greatest flooding in Northern California since the 1800s occurred in 1955 as a result of a series of Hawaiian storms, with the greatest damage in the Sacramento Valley around Yuba City.
Posted by 老广
at December 12,2007 03:16





