1981-10-08 — Page 24

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頁四第張六第日一十月九年酉辛歷夏

東方表行

W

東方表行

門市部

郭日僑華

WAH KIU YAT PO $1915.

·四期星

*育教聞港

日八月十年一八九一曆公年十七國民華中

一八〇四主報名登记。

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(

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1982

中學會考試題預習專欄

地理 (=)

明德出版社李隱業 提供資料

Geography (2)

IV Leet

Mill & Dale Press Ltd.

Questions for Revision:

3. The figure below shows. the temperatures of three cities and their Tocations. Discuss the various factors, giving rise, tu thé differences in their temperatures.

CITIES Jau, T-Jul T. Tokyo 3.0°c 25.4 Lanchow 0.5°0 28.3%

Foochow 11.6 6 27.90

LANCHOW

FOOCHOW

Suggested Answers:

C

can be felt at eqas vai

Whale Fanchrow, on the

other hand,

city as in Tokyo.

experiences more

extreme temperature

because of its

interior position I

winter, the heat of

land,

Water body is lost more slowly- than ;) so there is warming effect brought along by the onshore wind and affects Tokyo. But, for Lanchow, the warming effect cannot be felt and because land loses beat merej rapidly, it is bug ti colder than Tokyo. Ocean current.

The temperatures of a cuastal city as Tokyo can also be affected by warm und cold ocean turrents a such as the. Kuro-Shi o and Oya Shio, so the temperatures are not so extreme as those of Lanchov.

ISOTHERMS OF CONTINENT

LAND

HIGH LATITUDE

TOKYO

OCEAN

OCEAN.

3. PACTORS GIVING RISE TO

DIFFERENCES" IN

TEMPERATURES:

-4) Latitude

Ponchow is warmer than Tokyo and Lanchow in, winter and hotter. than they in summer*. It is because they are Located at different Latitudes. Foochow, being located at las lover Intitude than the other two cities,

is beater more intensively by the sun in both seasons. The sun's rays, which foll on Foochov at a larger angle, bring more heat since they have traveiled through: shorter distance ru Lie atmosphere and spread over a smaller

LWO area. The other eities, on the ither are located at higher latitudes. so tire

sun's rays fall more obliquely and Less beat can be absorbed.

B) Distance from sea

Temperatures of Tokyo and Lanchow are not the same although they are Located at the same latitude, Tokyo is warmer.in winter and cooler iu

Senior the lancho It is because air. temperature of a place can also be affected. by its distance from sea. Tukyo is located along the coast. Since water surface heats up more slowly than sea insurer', it is cooler. than the latul surface If there is oushore wi ud cooling effect

Low

LATITUDE

Winter Isotherm

Summer Isotherm

Above is a generalized pattern of distribution for summer and winter isotherms as they may appear on as

hypothetical continent

in the Vorthern Hemisphere.

Describe the

characteristics of summer and winter temperatures as shown by the pattern.

Account for such distribution pattern...

Suggested Answers:

Characteristics: Comparisuh between the coast and

interior

The isotherms, though in general run east-west, do nac follow the parallels exactly. In winter,

isotherms bend strongly equatorward, which hess that e temperatures along the cousts are warmer than those of the interior. In subsiel", the reverse is true - Isotherris. bend strongly poleward, indicating that the coasts chich cooler than the interior (Pige Fig. 1(a)

wre

CHARACTERISTICS OF VINTED. I SETITRUS

OCEAN

LAND

OCEAN

Winter

A: 10°C

B-10 C

(A & C are warmer tlian.

Bin winter)

Fig. 2(b)

CHARACTERISTICS OF

SUNNIER ISOTHERMS:

Summer

A:10

LAND

OCEAN

(A & C are cooler than

Bin summer)

2) Comparison between

the West and East coasts

The isotherms strikë the western coast at a much higher Latitude thau the east – winter temperatures along the western coast. are warmer, tlián the

east:

(Fig. 1(a), A is

warmer than C). i)The

SULINE r

the

isotherms skew to? the west. summer. temperatures on western coast are

cooler than tife.

east.

(Fig. 1(b), A cooler than C).

Reasong

1) Reasons for the

more extreme

temperatures in the interior-

The coastal regions experience warmer winter

temperatures and

cooler sunmer

Lemperatures since they can be g modified by the ocean. Water codies are always warber in winter ande cooler in summer since they warm and cool 'more slowly than do land areas. There are three primary reasons for the contrasts in Land and water temperatures:

i) Water Is mobile and experiences both vertical and

horizontal movements-vhich

distribute, heat" energy absorbed at the surface.

throughtout its mass whereas insolation. is absorbed by land muly at the surface and is transmitted downward slowly by conduction,

The specific heat of water is higher than that of land. That is,ủ given mass of water requires more heat, energy to raise its temperature 1 than does an equal mass of dry, landk、; Consequently, the

satie amount of

insolation will

produce a higher temperature on a

and surface tuan on a water surface. Conversely, in

ng, water vill cooling.

have to lose a greater arount of heat than Vi11 Fand Lo

produce the same drop in temperature

The general effect of the contrast in heating

of land and water areas is to produce. colder winters and hotter sumpers in the

CONSUL than

along coasts and over oceansi Coastal or marine climates tend to be moderate, expetencing: no great extremes in either daily or annual temperature. changes.

Fig. 2

GCEAN CURRENTS AND PREVAILING WINDS

LAND

OCEAN

Warm Oce a fi. Current

Cold Ocea Current

Prevailing Winds

LAND

Westerlies

NE: Trades

SE Trades

Westerlies

above

cau see

From the diagram, we that winser temperatures of the western coast, especially in Higher látitudes, can be raised by the worm ocean current, of which warm air is brough

to the land by unshore Westerlies', In the northern part of the eastern

coast, cold ocean current is following along, su

temperature is: lower.

In summer, the southern part of the eastern coast is much hotter than

otter

asons for the tre favourable climate of the zesterul coast:

The western coast of u continent always experiences a more clinate, with a cooler sunner and wormer winter the east. It prímurily due. La the effect of ocean. current, of which the effect is made more signigi cant by

the onshore prevailing winds,

Through the

horizontal

transport of

ocean

water in the form

of currents and heat is

drifts, f

carried from one part of the earth. "to" another. As al of us know that an ocean current travelling towards a pole will warm sir which passes over it, producing air temperatures Bigher than that: would normally he expected for the latitude. However, it should be noted that neiter oceans nor nor ocean currents.. can have the i maximum effect upon temperature unless

the prevailing winds blow from water to the land. Prevailing wind direction and the movemeuls of air masses have a direct influence upon the average Lemperature of; an areo. Below is a simplified diagram showing the flow of ocean currents and direction of prevailing winds (Fig. 2):

in corresponding latitude on west side of the

continent since the

Varm air above the

warm water is

brought landward

by the store. NE

trades.

生物

「明德出版社梁永華 提供資料

BIOLOGY (2)

MILE & DALE PRESS LTD)

LEUNG

WOW..

fit: 2. Energy and Organic

Matter

In a chemical analysis of food substances X, Y, and 2, the following results are obtained.

Food Substance.

No. of atoms/

molecule

.C 20

36 18 2

22 12 11

32. 44 8

a)Which of the above

substances is carbo hydrate? Give your rea-

son.

b Describe one test client confirms your answer (A).

c)Nane three other

elements other toan carbon, oxygen and hydrogen which can be ⠀⠀ found an proteins.

The following dingran shows an apparatus used to investigate the energy

food- content of common stuffs.

Thermometer

To filter

pump

water

paper towel

Crucible

Sti

Electric coil to ignite food

xygen

a)Name the apparatus. b)What was the use of

paper towel surrounding the metal cant

In an experiment to find the energy content of sucrose, 0:5g of sucrose was completely burnt.

ater

50cm

25 C 40 C

Volume of wat Initial temp. Pinal tenip.

(1)liat was the temp-

erature rise of the

water?:

(ii)If 1g of water re-

quires 4.2 Joules. of heat to raise 168 temperature by 1 C, and if heat. absorbed by the metal can and the copper coil was. neligible,

how much

heat was produced. by complete burning. of the 0.3 g of sucrose?

(water density=

1g/cm2).

d)(i)Calculate the energy value determined in. this experiment. (ii)Explain why the

above value is, different from the value given in re- ference books (17.2KJ/x).

Describle the energy conversion in this exeriment.

Auswers:

)Substance Y.

The reason is that the ratio of hydrogen atoms to oxygen atoms is

to 1.

b)Since the number of

carbon atvas per mole- cules indicates that Y is a double sugar, the. following test can be. carried out, Y is first boiled with hydrochloric acid for about 5 minate minutes, and then sodium

carbonate is added. The solution turns brick- red when heated with Fellings solution. c)Nitrogen, sulphur and

phosphorus,

a Food calorimeter. b)The paper towel acts as

an insulator to reduce heat loss in the surroundings.

c)(i)The Lemperature -ise

of the water was (40°C-25°C)=15°C.. (11)The amount of heat

produced was (50x15 x462)-3150(Jou Fes) difi)The energy value

5150 joules/0.39m2 10500 joules/g or 10.5 kg i)It is because a Targe: amount of energy released in this experiment had been used to warui up the glass tube and the air inside the metal cab,

e)Store

cuenii cal energy was converted into hest energy and light energy

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