三期星
日九十月九年四八九一曆公年三十七國民華中 教育化交
華賀
港小
中「梁祝小提琴協奏曲 | J銷超過一萬張,成的廣播節目中演出,並 一,實一且數度被邀作電視演出
謝氏會在不少國家
出少
. 謝家齊於一九七九一
港日藝人合作演出 小提琴結他二重奏
極堂
交响樂團以及他自已組一及元朗共修堂的票仍發 一音樂家合作,包括倫敦一種,現已在荃灣大會堂 曾多次與著名的樂隊放一元、十五元及三十元四 「極出色的演奏者」,他演出,門票分五元,十 | PEKE - D**# ! · TEX÷Z (BES) { 首次在倫敦威克摩爾 的兩斯二和音樂會,
KXEXACE #4 1、將與宋港結他演 的小提琴安之一的西婭
Hazar 結苘包及 ,在南海演公會中,, ,移離羌河北修堂,「小放牛」,「懷念曲一
昨由法領事揭幕 金美莎國畫展覽
年二本音樂會.....
時,在被耐大會堂演出,用一些綠島小夜宇的利丟特列國際出媽一次展出,邀請法熱駐港 二,二人將先在九月,並與西醫求子合多首特殊業,獲得多一八樓展覽館,舉行國一邊久老問師習國畫,曾 全明大會堂繼續展出
光法
起,大
落駐 沙行堂悠
統之入宿班
界塊面中鴨左缩进院。
片,均甚獲好評,而攴 攻西洋畫、畢業後回港一里與也,歡迎各界參觀 ̇她所澍錄的多嗎 國家巴黎美術學院,一見草知其爲州之行
賀陳克華將軍百齡開
令樂府
香港第一台,十五分,「與第二台
I a
(中蠹》七八千
報,天氣報告及華南海
·凌徒安時,新聞
. 六時,節目與第二
第一張」;卅分 六時,新聞簡報,繼續「優悠夜空中」 一時,新間親
四殿一〇三兆 〔立體聲調額)九一悠夜空中」。一
香港第二台 越天氣報告,微導「
: 九時,新出簡報,
八時,交通榖苦,
:七時,一新四大地 皆念茨·娄無大意派亡秦、伏波發業及壯」,八華南海域天氣報 新明商張,交通報告、 5八十年代;卅分。
「
卅分,三更半夜之「它」 曲四重奏」第十间。
卅分,新開簡報
七時,新酒報, 康緻「長光第一線」、
「輕談淺唱不夜天 ——二時,新旧杭然,
...三時,新旧擁報,
夕)晚上八時假大專會堂舉行一場-
滿西域色彩难代」,卅分,新聞位 香港學生轉導中心將於十月二日宀重顯節前-交通段告,繼續「八十
第一線」,卅分,新 交通鞎告,微韆「磊光 商報:交頭報告:
八時,新北報,一攤繳「經該淺唱不变人
」
四時,新北簡報!
· 九時,新簡報;
續「輕淺唱不夜 臺南海域天氣報告,繼
-五時,新出簡報,
頁二第張七第 日四廿月八年子甲膳夏
WAH KIU YAT PO
報日僑華
「鸛朝早精神好」。
·· +!D-SEE* 回,卅分,新出簡報,一卅分,新聞簡報,交通
誰「輕談淺唱不夜犬
J片至六時己。
+E REEK-
雖防守將酸務、類務
來「ALBERT
「香港第五台
「朝朝·特鹂好」,卅
區瑞強!,卅分, Ä 新點滴報。
六超短波調頻》九。
十二時,新聞簡報
_十一時,新鸿簡報
六及一〇五兆赫
KRELAY
SERVICE
BBC WORLD
記一
,新郎簡報:「阿郎
·斯、阿爾班尼士、雞路及羅特整高等作曲家的
DO..
倫多大學音樂系畢業,獲學學位;闾年在加拿術報告,經濟行情報導「猛褲傳昇」,卅分, 分,「橋懐粘贴一。
天氣報告及華南海域天 ,繼續「生活百合匙」
『明京夢」第五回, 價愍報導,人在實錄之 十五分,一日旦三分镫 」,「生活百合匙」。
分,「今日世界」會
,繼續「阿郎日記」, 卅分,新聞簡報,繼徵
,十二時,新聞簡報
節段」,
電台海海新城及「令鼓 十五分,轉而英國廣播
:七時,新闢簡訊, 岛光共享:醬油活節假
·一個醉半小時」,
· I · FEES ·
新S鑌報。
二時,新聞簡報,
•新超簡潔。
三時,新閒簡報,
「青春交响曲」,卅分】4
INANCIAL N 「猛卅
·四時,新甜篚報, 交通報告,繼續「發光。
三時,新聞簡報,亭」,浙分,「蘭花草
REEF BBC F 九時,新開俑,
八時,新聞簡報,
EWB,保障「從记就
第十一囥,卅分,近
...四時,新聞簡報
五時,新聞簡報, 』,卅分,新出席批。
親,「學而批評一
十時,新開佈報,一
七「死至一九八四年九月二十五日。跌迎各團體,各
『九十分鐘時事廣場。
六時,新聞簡報,
五時,「九十分躓J,卅分,新聞簡報,,絃曲人地之一舞台上
·靑春交吧 曲之「中文榜拙」,卅分,新師簡訊
十一時卅分,戲曲
「粵曲闵誤」,卅分, 新珥簡報,戲曲天地之
一般一時,戲曲天地之一
「天地之一歲朵里移」。
天氣報書及華南海域天一報告。· 六時,新聞報告,10亞菜」,肝分,交通
七時,新聞簡報:
「溯劇」。
二時卅分,新即
分鐘時事廣場),卅分。
:七時,新的海報,一磅樂悠」。
三時,新開
SERIE
音樂人音樂廳之「韭影 美樂集之「就曲世界」
四時,新號 預
·九時,新蝕而報, 八時,新時將報,一古典精華⺥雷射唱片播 民間故事之「血染越王 「台」第七间,卅分,
小時,新間簡報,:頭語節目:「清惕點點
普通話屇習班,九龍彌敦道七八八號利美商業大 繼續「賽馬霄况:一 「學校及各界人上器je 查過佢話;三;八一五二 繼請「馬實」,「天氣報告及莖南梅茲大·」。 三七,二—九一七三七九,查詢地址: 香港一十時,新閎簡報, 氣報告、「八爪魚」。「五時至凌朵二時卅
十一時,新開報告分-BBC WORL
百十二樓賣,一、香港普通話教學中心,九龍,先叫爲止,四十分,十五分,(第一、二) D SERVICE.
二時卅分,
彌敦道七一九號銀都商業大殿七宇撰反省協游湖,「歌曲選撥」。台會合),海髙職位空 十一時,新館報告」缺報導,「獲悠夜空中 HE NED
1985.
Mereuty Dry.bulb thermometer
Mercury thermometer
Mercury in stem.
Muslin
Wet-bulb thermometer
Maximum thermometer with constriction constriction Mercury Max!"
Break in
whter
threach":
中學會考試題預習專欄
地理
Bulb
· PARICAPIĄ
Maximum thermometer with metal index.
Mink. To meat index.
明德出版社
李陽業
提供資料
Mercury
̇藜基施
GEOGRAPHY (1)
Y.Y LEE & K. C. CHOT
MILL & DALE PRESS LTD.
Series of exercises is to help you to get a much better result in the Geography Paper of the School Certificate Examination. Two essay type questions, are each time, with suggestive model answers. They aim at supplying supplemen- tary information as well. as providing revision for you. To acquire the
optimum benefit, student are advised to think of the points carefully by themselves first before reading the model answer. The questions are so carefully set that they. covering almost every item of thes syllabus, not only give you ample information, but also help you. evaluate your ability to observe accurately, interpret systematically and present your ideas logically.
Revisional Questions: 1. If you were given the
task of setting up a 'school weather station
to
measure air temperatures, relative hymidity and rainfall. amounts, what would you buy? How would you set them out? Draw well-labelled diagram to illustrate
your
answer.
Suggested Answers;
a. Air temperatures
To measure air temperature, the following instrument should be bought: 1) An o
An ordinary mercury thermometer to measure: current air temperature "or the temperature at a particular tine.
Maximum thermometer to measure maximuni
temp.
5) Minimum thermometer
to measure minimum temp..
DIAGRAMS TO SHOW THE THREE TYPES OF THERMOMETERS
Minimum thermometer Alcohol. Min To Metal index
Procedure of Setting Up 1) All the above
instrument's should be housed horizontally in a Stevenson Screen. 2) This is done since
shaded temperatures are required."./
3) The Stevenson Screen
is a wooden box, whose roof is double boarded with an air space between so that the heating effect of the sun can be minimzed. The louvred sides allow the air to move. freely so that the ai inside the screen has the same characteris→ tics as the air outside.
5) The screen is painted
white to improve insolation,
6) The song mak
on
is mounted
a stand to avoid heat reflection from
the ground from influencing the thermometers directly.
7). It should be
positioned in the most. open and exposed place with its door opening
to the north to prevent the sun from shining into the screen whilst readings are being taken.
8) The readings should
be recorded daily at a fixed time, pre- ferrable in the morning. After recording, the maximum thermometer should be reset by using a magnet (for the one with a metal index) or by shaking vigorously (for that wịth a' constriction) and the minimum thermometer should be reset, by tilting it gently.
Relative humidity.
To measure relative humidity, a
Wet-bulb
and dry-bulb thermo- meter should be bought
WET-BUĽH AND "DRY-BULB THERMOMETER
Procedure of Setting Up
It should be housed in the Stevenson. Screen, too.
2) The bulb of the wet bulb thermometer should be kept moist all the time by covering it with muslin which dips into a container of water.
3) The difference
between the two read. ings is an indicator. of the humidity of. the air:
if there is no difference - the
air is saturated
if the difference
is large e
humidity is low
if the difference is small. -humidity is high The actual value of relative humidity is obtained by checking the reading from, a book of tables.
c. Amounts of Rainfall
To measure the amount of rainfall, a rain gauge is necessary.
A PAIN GAUGE
-Funnel
-Copper cylinder.
∙Glass bottle.
Outer copper
case
Procedure of Setting Up
In setting up the rain gauge, the following points must be noted: 1) It must be put on level ground."
2) It must be placed in an exposed position, far away from any objects which might affect the amount of rainfall collected. If the buildings and
trees
are present, the gauge must be positioned away from them at a distance of at least twice the height of these objects.
3) It must be sunk in
the ground to prevent it from being blown or knocked over.
4) The top of the funnel must be 5.08 cm (12") above ground-level, to prevent rain nearby splashing into the jar
2. Below are diagrams
showing information
of rainfall in Hong
Kong. With the aid of diagram, account for
and the seasonal geographical
distributions of rainfall in Hong Kong.
Fig. I
RAINFALL DISTRIBUTION OF HONG KONG
"Over 2500 mm 2000-2250 mm
1760-2000 mm below 1750 mm
Fig. II TEMPERATURES & RAINI ALL OF HONG KONG.
བྱ ོ ན ཞེ ཚོ མི ཡ
2
Rainfall fam
JFMAMIJASOND.
Suggested Answers: The Seasonal Distribution of Rain- fall in Tong Kong
From the Climatic: graph, we can see that the rainfall in Hong Kong, with an annual total of about 200. 2500 mm, does not distribute evenly. About 80% of the rain. occurs in the summer months from May to Sept. A monthly total of over 250 mm in the summer rainy season. is not uncommon. While in winter, it is relatively dry.
The summer maximun of rainfall in Hong Kong can partly be explained by the influence of monsoons. Hong Kong lies in the Asian monsoonal wind belt. In summer, a low pressure belt is formed over Mongolia, while a high pressure belt is found over the sea. As a result, the wind blow inland from the sea. They are therefore moist and they bring heavy rain to Hong Kong. In winter, the winds blow
offshore because the low pressure
over
Mongolia is by now
replaced a high
pressure system. Thus
the winds that
influence Hong Kong are quite dry. (Fig.
Fig. A
A).
THE SUMMER MONSOON OF ASTA
IN TEKISE
LOW
PRESSURE
HORSE AT HIGH
Besides the monsoons', the seasonal distribution
of rainfall in Hong Kong is also greatly affected by typhoons. The typhoons, which attack Hong Kong mostly from May to Sept, are always accompanied by torrential rain (Pig. B).
Fig. B
MAIN TYPHOON TRACKS IN THE WEST PACIFIC OCEAN The Geographical
Distribution of lainfall in Hong Kong
Fig. II is the annual rainfall may of long Kong. The map shows that the areas with maximum rainfall (over 2200 mm) coincide with highland areas, e.g. Tai Mo Shan region and Lantao Shan region. The areas with the lowest amount of
rainfall (belgw 1200 mm) lies.on the west, e.g. the northwest lowland around Deep Ray, the southwest of Lantan Island and the Tsing Yi Island. Such a a geographic distribution indicates an orographic effect. This is because, as mentioned above, most of the rain in Hong Kong is brought by onshore monsoon which blow mainly in an easterly direction from the sea. As the moistureladen winds meet the mountains they will be forced to rise. They are then cooled, condensation thus occurs and clouds are formed. Being subjected to much the same process as those in the rising air currents as heated, water droplets fall down at last. Thus the mountain regions, especially the east- facing slopes in Hong kong. have more rain
because of
this
orographic effect.
By the
time the winds reach the lowlying western part, they are depleted of moisture. As they decent the leeward slopes, they are warned by compression consequently, there is little rain and these areas are referred to as rain shadow areas (Fig.
Most of the tropical cyclones are formed to the E of Philippine
Furthermore, the high
summer
temperatures Hong Kong (with an
average around 27°C) are likely to induce rainfall too. When the land surfaces are overheated strong vertical air currents set up. As the air asends, its temperature is reduced until condensation takes place and clouds are formed. The water droplets in the clouds will become bigger with further ascent, which means further cooling..
In Lime the water droplets in clouds become too big and heavy to be saturated, rain begins to fall. This type of ruin is known as convectional rainfall. Hong Kong, being situated in the tropical latitudes, the convectional rainfall is especially characteris- tic in sumper (lig. C).
Fig. G FORMATION OF CONVECTIONAL RAINFALI
Cumulo-
nimbus clouds
level
•DESCENDING
··RISING
COCLER
RAIK!
WARM
DENSER
AIR
LAND SURFACE HEATED BY THE SUN.
Fig. D
THE FORMATION OF OROGRAPHIC relif) RAIN
L.C
As air ascends. it becomes cualer/ and saturated
R.Hvises
SEA
Winkisia
Mountain mas
"As ait.
descends.
it composted
and become" AWatmes
AR.H. falls RAIN
SHADOW