范文一：MM们保养相关的英文句子

MM 们保养相关的英文句子

I want a facial.

我想做个面部保养.

As you age, the circles can darken and the force of gravity will also make the circles look larger.

随着年龄的增长黑眼圈会更严重, 同时随着地心引力的作用有扩大的趋势.

Stimulating masks promote blood flow and firm up the skin.

刺激性面膜则可以促进血液循环并且是肌肤柔韧有力.

Do you have a good thickening mascara?

你们有浓密型的睫毛膏吗?

What do you have in toner for combination skin?

你们有哪些爽肤水是针对混合性皮肤的呢?

This day cream will moisturize your skin and it has a sun block rating of 8.

这款日霜可以滋润你的皮肤并且有防晒功能, 防晒指数是8.

We have a full range of products from cosmetics to skin cleansers and moisturizers.

我们有一系列的产品, 从化妆品到洁肤和润肤品.

范文二：历史时期长江中游水灾与厄尔尼诺事件的遥相关_英文_

() Article ID :100428227 20050320376205

HISTIROCAL FLOODS IN THE MIDDL E REACHES OF

THE YANGTZE RIVER AND EI Ni1NO EVENTS

1 2 3WU Yi2jin, William A. Go ugh, J IAN G To ng

(1 . School of Urban and Environmental Sciences , Huazhong Nor mal Univer sit y , Wuhan 430079 , China ;

2 . Environmental Science , Univer sit y of Toronto at Scar borough ,1265 Milit at y Trail , Scarborough , Ontario , M1C 1A4 , Canada ;

)3 . Nanjing Instit ute of Geograp hy and Limnology , The Chinese Academy of Sciences , Nanjing 210008 , China Abstract :The basins of middle reaches of t he Yangtze River are t he wor st flood area of whole basin. To st udy t he variatio n regulatio n of t he floo ds in t his area and EI Ninno event s over a lo ng historical period and to identif y t he teleco nnectio n between t hem assure imp rovement in p redictio ns of floods in t he regio n. By using statistics analysis , bot h time series of t he floods and EI Ninno event s since 1525 are st udied. The result s show t hat t he main cycle of flood variatio n is lo nger t han t hat of EI Ninno event s. The latter o bvio usly shows t he fluct uatio ns of abo ut 22year and 3,4 year period while t he former is not so significant but can al so be identified o bvio usly t he perio d of 2 , 8

() and 40 year s at least exceeding t he level of co nfidence 0. 03. By f urt her analyzing t he co upling fluct uatio n of t he two time series , t he significant teleco nnectio ns between t hem at bot h high and moderate f requency sectio ns are fo und. The result t urns o ut t hat t he respo nse of t he floods alo ng t he middle reaches of t he Yangtze River to t he

( ) effect s of El Ninno event s is not o nly immediately delay see o ne yearas many Chinese scientist s believe , but al so

() can be so mewhat lo ng2lived as lo ng as abo ut 8 year s. The result s al so explicate t hat t he sho rter t he interval of EI Ninno event s , t he soo ner t he following flood respo nds. Vice ver sa , flood co uld delay if t he interval time of EI Ninno event s is lo nger .

Key words : historical floods in t he middle reaches of t he Yangtze River ; EI Ninno event s ; teleco nnectio n Document code :A

eastwards t hro ugh cent ral China o n it s way to t he

( ) Do nghai East China Seain Shanghai o n China’s east 1 INTROD UCTION

( ) coast figure 1 . In it s middle sectio n , it passes

t hro ugh t he immense J ianghan Plains f ro m Yichang to A s t he t hird largest river in t he wo rld and t he lar2

Wuhan , named Jingjiang. Because of t he limited ca2 gest o ne in China , t he Yangtze River is so important to

pacit y of floo d discharge , t his regio n is t he wor st human societ y in China t hat it is a mirror of Chinese

flooding area of t he whole Yangtze basin. For in2 histo ry. Since ancient times , people in it s basins have

stance , t he capacit y of flood discharge in J ingjiang is been suffering f ro m and fighting against floo d disaster s

3 abo ut 60 000 m/ s. However , t here were an estimated f ro m generatio n to generatio n. It has lo ng been known

108 disast ro us breaks in t he river embankment s acro ss as“China′s so rrow”for t he lives t hat have been lo st

t he J ingjiang reaches f ro m 1525 AD to 1995 AD and and t he damage do ne by it s f requent and violent

more t han 24 years in which flood discharges have ex2 floods.

( ) ceeded t his capacit y af ter 1892 Table 1, causing great Originating in Tibetan Plateau , t he river flows

Received date :2004210215 ; Revised date :2005205219

( ) Foundation item : Thi s wor k is sponsored by Key project of Knowledge Creativit y Engineering , The Chinese Academy of Sciences KZCX32SW331,

() National Science Foundation of China 40271112, The Opening Research Foundation of Hubei Provincial Waterlogged Disaster s

( ) and Wetland Agricult ure Key Laboratory HN KFJ 2002 T02and Chinese Scholar ship Council

) (Biography :WU Yi2jin 1963, , Male , Professor , Email : wuyijin @p ublic. wh. hb. cn

interannual variabilit y over t he Yangtze River valley

t hat causes yearly rainfall total s fluct uating greatly ,

especially rainfall during t he floo ding seaso n.

El Ninno is a recurring pattern of climate variabilit y

in t he eastern equatorial Pacific t hat is characterized by

ano malies wit h warming perio ds of sea2surface temper2

at ure. As t he remarkable co nnective signal between

t he whole near2glo bal2scale climatic change and sea2

surface temperat ure , EI Ninno event s p rofo undly affect

t he regio nal climate. There have been t hus far many Fig. 1 Middle Reaches of t he Yangtze River Basin st udies o n EI Ninno and it s relatio n to glo bal and re2

( gio nal climates t hro ugh at mo sp heric circulatio n C P damage wit ho ut any exceptio ns.

) Chang , Pat rick Harr , and Jianhua J u , 2001. And al2 by The ext reme flood discharges were caused

so recent research shows t hat EI Ninno event s has so me heavy rainfall over t he upper reaches of t he Yangtze

effect o n regio nal lo ng2term p recipitatio n in China. River valley. It is co mmo nly known t hat t he climate of

China is st ro ngly influenced by t he East Asian mo n2 In t his paper , we attemp t to find t he fluct uating soo n. The p rimary p hysical manifestatio n of t he sum2 regulatio n of bot h floo ds in t he middle reaches of t he mer mo nsoo n is per sistent , heavy p recipitatio n identi2 Yangtze River and EI Ninno event s , and t he teleco nnec2 fied wit h a co herent , well2defined rainband. Because of tio n between t hem based o n histo rical data by using t he variatio ns in mo nsoo ns , t he rainband has ano maly statistic met hods.

3 Tab. 1 Extreme Flood Discharges at Yichang Station Af ter 1892 ( m/ s)

Year Discharge Year Discharge Year Discharge Year Discharge

1892 64. 600 1917 61 . 000 1931 64 . 600 1954 66 . 800

1896 71. 100 1919 61 . 700 1936 62 . 300 1958 60 . 200

1898 60. 600 1920 61 . 500 1937 61 . 900 1974 61 . 600

1905 64. 400 1921 64 . 800 1938 61 . 200 1981 70 . 800

1908 61. 800 1922 63 . 000 1945 67 . 500 1989 61 . 800

1909 61. 100 1926 60 . 800 1946 62 . 100 1998 63 . 600

rect l y aff ect ed by EI Ninno a nd t ho se a rea s aff ect ed

by o t he r un u sual co nditio n s relat e d to t he EI Ninno 2 DATA RESOURCE AND PROCESS

( e . g. t he dro ught s t hat of t e n aff ect so ut hea st er n

() W H Q ui n n a nd V T Neal 1992ha s p re se n2 Pe r u a nd a djace nt p a r t s of Bolivia duri ng a n EI t ed nicel y t he u sef ul dat a a bo ut t he st re ngt h of EI ) Ninno, co veri ng t he p erio d 1525 , 1987 . In t ho se Ninno eve nt s w hic h t hey i de ntified , eval uat e d , a nd hi sto rical EI Ninno eve nt s dat a , t he st re ngt h of EI det er mi ned f ro m ma ny det aile d repo r t s f ro m saili ng Ninno eve nt s a re cla ssifie d i nto seve ral cat ego rie s , ve ssel lo gs , dia rie s of co nqui st a do r s a nd t hei r e n2 ( ) ( ) t hat i s , ve r y st ro ng V S, st ro ng S, a nd mo der2 to ura ge s , mi ssio na rie s , pi rat e s , p rivat ee r s , hi sto2 ( ) at e M. A mo ng t he m , t he S + , M + a nd M2 a re ria n s , geo grap he r s , e ngi neer s , geolo gi st s , hydrol2 a dde d to fit t ho se EI Ninno eve nt s w ho se i nt e n sitie s o gi st s , new sp ap er s , a nd scie nti st s f ro m t he va rio u s a re a ro u nd st a nda r d cat e go rie s. Fo r t he co mpo und o t he r di scip li ne s w hich p ro vi ded a rat her co nti nu2 t yp e of activit y o ve r t he di st a nt p a st , t he si gnal s of o u s so urce of i nfo r matio n o ver bo t h t ho se a rea s di2 M / S o r M 2 / M + a re u sed to co ve r t wo eve nt s of

长江流域资源与环境 第 14 卷 378

Tab. 2 Intensity Categories of Historical EI Ninno Events And Corresponding Numeric Digital

( )( )( )cat ego rie s ver y st ro ng V S S + st ro ng S M + mo derat e M M/ S M2 M2/ M +

digit al 3 2 . 5 2 1 . 5 1 0 . 5 0 . 5 0 . 3

diff e re nt i nt e n sitie s beca u se of lac ki ng t he det ailed ba si n f loo d i nde x fo r each yea r . i nfo r matio n to f ur t he r refi ne t he m.

Fo r qua ntit ative p urpo se s , t ho se cat e go rie s 3 CAL CUL ATIO N A ND A NALYSIS a re di gitize d i n t hi s p ap e r sho w n i n Ta ble 2 .

( ) Kevi n E Tre n be rt h 1997 defi ned t he EI 3 . 1 Cycles in EI Ninno events/ f loods Ninon eve nt a s 52mo nt h r un ni ng mea n s of sea sur2 Po wer sp ect r um a nal ysi s wa s app lie d to each

( ) f ace t e mp erat ure SS Ta no malie s i n t he Ninon 3 . 4 of t he me mbe r s of t he EI Nino n eve nt s a nd f loo d s

(serie s . The ma xi mum la g i n t he a nal y si s wa s set at ) regio n 5N?,5S? , 120,?170W?e xceed 0 . 4C? fo r

6 mo nt h s o r mo re . We fi nd t hi s defi ni ng well 80 yea r s. The co mp ut atio nal p roce dure i s t he sa me mat chi ng W H Q ui nn’ s fo r t hei r co mmo n yea r s a s o ut li ne d i n WMO Tec h nical No t e o n cli mat e duri ng mo der n ti me . The refo re , t he EI Ninno e2 ( ) c ha nge 1966 . The po wer sp ect ra fo r EI Ninno ve nt s ti me se rie s defi ne d by W H Q ui n n i s e xt e nd2 eve nt s wa s sho w n i n Fi gure 2 w hic h reveale d t he

hi ghe st p ea k s of po wer sp ect r u m occ ur s at k = 78 , ed to 1995 by a ddi ng t he EI Ninno eve nt s 1991 ,

Kevi n E ,1995 de rived f ro m 48 a nd 41 , all of w hic h e xcee d 0 . 01de gree of co nfi2 1992 , 1993 a nd 1994

Tre nbe r t h′s re sult s.de nce . That t ur n s o ut t he ti me serie s of EI Ninno

A s i s p ro ba bl y well k no w , t he Chi ne se have eve nt s have t he p erio ds of a bo ut 2yea r s , a nd 3,4 t he be st a nd mo st co mp let e p ho nolo gical reco r d s yea r s. Thi s re sult i s a lit t er mo re co nver ge nt t ha n

( ) t hat of A my Cle me nt a nd collea gue s of t he L a m2 t hat e xi st No r ma n J Ro se nber g , 1982 . D uri ng

t he Mi ng a nd Chi ng dyna stie s f ro m t he 15t h o nt2Do her t y Ea rt h O b ser vato r y i n Pali sa de s , New

() t hro ugh t he 18t h ce nt urie s , Chi ne se re gio nal geo2 Yo r k 2001, t hey say EN SO occ ur s ro ughl y ever y

t wo to seve n yea r s a s a re sult of heat a nd e ner gy grap hical reco r ds we re ca ref ull y ma de so t hat a r2

e xcha ngi ng bet wee n t he at mo sp here a nd t he chive s of dat a o n f loo ds , dro ught s , a nd ma ny o t he r

ocea n s. cli matic eve nt s a re no w availa ble fo r st udy. In t hi s

p ap e r , hi sto rical f loo d dat a a re derived f ro m“f loo d Sa me a s t he a nal y si s of EI Ninno eve nt s , t he a nd dro ught di st ri butio n at la s of Chi na i n t he lat e st re sult of smoo t hed po wer sp ect r um fo r f loo d s

( ) ( Figure 3sho w s t he hi ghe st p ea k s of po we r sp ec2 500 yea r s ”Chi na Ce nt ral Met eo rolo gy B urea u ,

) t r um occ ur s at k = 65 , 19 a nd 4 , e xcee di ng 0 . 02 , 1989a nd a ca ref ul e xa mi natio n of t he dat a have

bee n ma de fo r t he select ed st atio n s , Yicha ng , 0 . 03 a nd 0 . 01 degree of co nfi de nce re sp ectivel y.

That t ur n s o ut t he ti me serie s of EI Ninno eve nt s J i ngzho u , Yueya ng a nd Wu ha n , a s t hey a re rela2

tive co mp let e ne ss , sp atial di st ri butio n , a nd p ro x2 ha ve t he p e rio ds of a bo ut 2 yea r s , a nd 8 , a nd 40 i mit y to f loo d2seve r a rea s. The dat a a re e xt e nded yea r s.

to t he mo der n ti me by t he met ho ds u sed i n a bo ve 3 . 2 The analysis of cross spectrum

EI Ninon at la s a nd co nve r t ed i nto rai nf all by t he met ho d p ro2 The re sult of cro ss sp ect r um fo r

( ) po se d by Xio ng A nyua n , a nd Wu Yiji n , et al . eve nt s a nd f loo ds Fi gure 4sho w s t hat t he re a re ( ) 1999 . The refo re , bo t h t hree f reque ncie s at w hic h t he si gnifica nt co r rela2 degree s of f loo ds a nd

tio n of t wo ti me se rie s e xce ss 0 . 01 level at t he rai nf all a re calc ulat ed si mult a neit y so a s to c heck if

p ea k s of k = 20 , 26 a nd 80 re sp ectivel y. Fro m t hey a re coi nci de nt .

t hat , it ca n be co ncl ude d t hat t he re spo ndi ng of t he All dat a u se d i n t hi s p ap er i s f ro m 1525 to

1995 a nd sp atiall y wei ght ed u si ng Thie sse n pol y2 f loo ds i n t he mi ddle reache s of t he Ya ngtze Rive r

() go n s L i n sley et al . , 1975to creat e a n all2mi ddle to EI Ninno eve nt s happ e n s no t o nl y at hi gh f re2

( que ncy , but al so at mo de rat e f reque ncie s See o nl y la sti ng up to t wo yea r s a s o t her scie nti st s

) 2 t hi nk . The a bo ve re sult t ur n s o ut t hat t he ocea nTa b . 3. The re sult al so e xp licat e s t hat t he sho r t e r

t he i nt er val bet wee n EI Ninon eve nt s i s , t he soo ne r iceff ect s of El Ni no eve nt s o n t he f loo ds alo ng t he

mi ddle reache s of t he Ya ngtze Rive r i s no t o nl y i m2 t he follo wi ng f loo d wo ul d re spo nd. Vice ver sa , de2

( ) lay ti me of f loo d will be lo nger w he n t he i nt er val of mediat el y delay see o ne yea r a s ma ny Chi ne se

scie nti st s believe , but al so ca n be so mew hat lo ng2 EI Ninno eve nt s i s e xt e nded.

() lived e . g. 8 yea r s.

REFERENCES :

[ 1 ] Cha ng C P , T J G Chen . Tropical ci rculatio n s a ssociat ed wit h

so ut hwest mo nsoo n o nset and we st erl y sur ge s o ver t he So ut h Chi na Sea [J ] . Mo n Wea Rev. 1995 , 123 : 3254,3267 . Fig. 2 Re sult of Po wer Spect r um fo r El ninno Event s [ 2 ] Chi na Cent ral Met eo rolo gy Burea u . The floo d a nd dro ught di s2

t ri butio n atla s of Chi na i n t he lat e st 500 yea r s[ Z] . Met eo rolo2

()gy Pre ss , Beiji ng ,1989 . i n Chi nese

[ 3 ] Cle ment A C , Cane M A & Seager R. A n o r bit all y driven

t ropical so urce fo r a br up t cli mat e cha nge [ J ] . J of Cli mat e ,

2001 ,14 : 2 369,2 375 .

[ 4 ] Cha ng C P , Pat rick H ,J u J H . Po ssi ble role s of atla ntic ci rcu2 Fig. 3 Result of Po wer Sp ect r um fo r Follds latio ns o n t he wea keni ng i ndia n mo nsoo n rai nf all2EN SO rela2

tio n ship [J ] . J of Cli mat e ,2001 , 14 : 2 376,2 380 .

[ 5 ] J aco bs Ga , H url burt He a nd Ki ndle et al . Decade2scale t ra ns2

p acific p ropagatio n a nd wa r mi ng eff ect s of a n El2Ni no a no mal y ( ) [J ] . Nat ure ,1994 , 370 6 488: 360,363 .

Li nsley R K , Ko hler M A and Pa ul hu s J L H . Hydrolo gy fo r [ 6 ]

( ) engi neer s a nd edn[ M ] . New Yo r k : Mc Graw2Hill , Inc ,1975 . No r ma n J R. Agricult ural met eo rolo gy i n Chi na [ J ] . Bull A2 [ 7 ] Fig. 4 Calculated Re sult of Coagulato n Functio n ( ) mer Met e Soc ,1982 ,63 3: 250,257 .

Tab. 3 Coincidence Coagulatio n Functio n Trenber t h K E. The defi nitio n of El Ni no [J ] . Bull A mer Met e [ 8 ] ( ) Soc ,1997 , 78 12: 2 771,2 777 . Pea k s wit h Diff erent Perio ds

Q ui nn W H a nd Neal V T. The hi sto rical reco r d of EI Ninno e2 [ 9 ] ( )Ha r mo nic Val ue k 20 26 80 vent s[ A ] . i n : Raymo nd S B a nd Philip D J Ed . Cli mat e si nce ( )Perio d yea r 8 6 2 A . D. 1500 [ C ] . Ro utledge ,1992 . 623,648 .

[ 10 ] WMO . Cli matic cha nge [ R ] . Tech Not e No . 1966 . ( )1994 J u st a s J aco b s Ga , et . al de mo n st rat ed [ 11 ] Xio ng A Y , Wu Y J a nd Cai S M . Reco n st r uctio n of rai nf all i n t hat si gnifica nt local eff ect s of El Ni no eve nt s i n rai ny sea so n ba sed o n hi sto rical dro ught / floo ds grade s[J ] . Ad2

t he Pacific Ocea n ca n be e xt re mel y lo ng2live d , no t ( ) va nces i n At mo sp heric Science s ,1999 ,16 1: 147,153 .

长江流域资源与环境 第 14 卷 380

历史时期长江中游水灾与厄尔尼诺事件的遥相关

1 2 3 吴宜进, Willia m A . Go ug h, 姜彤

(1 . 华中师范大学城市与环境科学学院 ,湖北 武汉 430079 ;2 . 多伦多大学士嘉堡分校环境科学中心 ,安大略 M IC 1A4 ,

)士嘉堡 ,加拿大 ;3 . 中国科学院南京湖泊地理研究所 ,江苏 南京 210008

摘 要 :长江中游历来是长江流域水灾最严重的地区 ,研究历史时期这一地区水灾发生的变化波动并找出其与厄尔 尼诺事件的遥相关 ,将有助于对长江中游水灾发生的预测 。对这二个时间序列自 1525 年以来的数据进行了统计学 分析 。结果表明 ,水灾发生的主要周期比厄尔尼诺事件发生的周期要长 : 后者主要表现为 2 年和 3,4 年的振动 ,而

( ) 前者的主要周期为 2 年 、8 年和 40 年 ,其显著性也没有后者明显 但都超过了 0 . 03 的置信度。通过进一步分析历 史时期长江中游水灾与厄尔尼诺事件的耦合振动 ,发现它们之间存在显著的遥相关 。结果表明 ,长江中游水灾对厄

() ( 尔尼诺现象的响应不仅存在着如许多中国学者相信的短期滞后 如 :1 年,而且还存在着比较长时间的滞后 最长可) 达 8 年。研究结果同时表明 ,如果厄尔尼诺事件发生的相距时间愈短 ,这一时期长江中游水灾响应的滞后时间也愈 短 ,反之亦然 。

关键词 :历史时期长江中游的水灾 ; 厄尔尼诺事件 ;遥相关

更正 :

本刊 2005 年第 2 期刊发蒋莉等作者撰写的《生态足迹影响因子的定量分析》论文中文和英文副标题有

() 误 ,应为 “: ———以中国大陆各省 区市1999 年生态足迹为例”和“A CA S E S TUD Y O F C H IN A′S PA R T I Y

P ROV IN C ES ECOL O GICAL FOO T P R IN TS IN 1999”。

特此更正 。

《长江流域资源与环境》编辑部

范文三：与世界历史相关的中国历史

与世界历史相关的中国历史

1、 三次工业革命对中国的影响（见表） 2、 两次世界大战对中国的影响 一战：

A 由于帝国主义放松对中国的侵略，中国的民族资本主义进入黄金时代

B 一战中，中国加入协约国集团作战，是战胜国之一，但是巴黎和会外交失败，引发了五四运动，无产阶级登上历史舞台，新民主主义革命开始；华盛顿会议对中国实行宰割。 C 一战中，日本提出灭亡中国的二十一条，形成独霸中国的局面。 二战：

中国是世界上最早抗击法西斯，也是世界上最后一个获得胜利的国家，抗日战争是世界反法西斯战争的重要组成部分，有力支援了世界反法西斯战争，二战后期，中国参加开罗会议、波茨坦会议，《开罗宣言》和《波茨坦公告》宣告台湾是中国不可分割的一部分。 3、 十月革命对中国的影响：

十月革命一声炮响，给中国送来了马列主义，最早宣传马列主义的是李大钊，他著有《布尔什维主义的胜利》、《庶民的胜利》等文章。

在十月革命的推动下，中国掀起了猛烈的反帝反封建斗争，五四运动、中共诞生、北伐战争是典型事例。 4、1929—1933年经济危机对中国的影响

为了挽救危机，日本建立法西斯专政，对内专政，对外侵略扩张，为此发动九一八事变；而英国法国采取纵容绥靖政策，致使日本侵略不断加剧。中日矛盾成为中国当时的主要矛盾。

5、二战后，美国成为世界霸主，在全球推行霸权主义政策，期间在亚洲推行热战，对华采取扶蒋**、发动侵略朝鲜的战争。

在两极格局中，中国属于社会主义阵营，在美苏争霸过程中，双方根据自己的实力对比变化而采取不同的对华政策，而中国则始终奉行独立自主的外交政策，始终坚持社会主义道路，坚持改革开放、取得了举世瞩目的成就！

（三）两次世界大战简表

三次工业革命简表

范文四：口语必备：乘飞机的相关英文词汇和句子

口语必备:乘飞机的相关英文词汇和句子 基础词汇

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需课税商品 Dutiable Goods

观光 Sightseeing

行李提取 Traveling - luggage claim 机场费 airport fee

出站(出港、离开)departures

国际机场 international airport 登机手续办理 check-in

国内机场 domestic airport

登机牌 boarding pass (card)

机场候机楼 airport terminal

护照检查处 passport control immigration 国际候机楼 international terminal 行李领取处 luggage claim;baggage claim 国际航班出港 international departure 国际航班旅客 international passengers 国内航班出站 domestic departure 中转 transfers

卫星楼 satellite

中转旅客 transfer passengers 入口 in

中转处 transfer correspondence 出口 exit;out;way out

过境 transit

进站(进港、到达) arrivals

通关时 Traveling - at customs 报关物品 goods to declare 不需报关 nothing to declare 贵宾室 V. I. P. room

海关 customs

购票处 ticket office

登机口 gate;departure gate 付款处 cash

候机室 departure lounge 出租车 taxi

航班号 FLT No(flight number)

出租车乘车点Taxipick-up point 来自…… arriving from

大轿车乘车点 coach pick-up point 预计时间 scheduled time(SCHED)

航空公司汽车服务处 airline coach service

实际时间 actual

租车处(旅客自己驾车) car hire 已降落 landed

公共汽车 bus;coach service 前往…… departure to

公用电话 public phone;telephone 起飞时间 departure time 厕所 toilet;W.C;lavatories;rest room 商务签证 Business Visa

旅客登机报到处 Check in Counter 观光签证 Tourist Visa

在飞机上 Traveling - on plane 盥洗室 Lavatory

使用中 Occupied

无人 Vacant

女空服员 Stewardess

男空服员 Steward

机内免税贩卖 In-Flight Sales

常见对话

我的座位在那里?Where is my seat?

我能将手提行李放在这儿吗?Can I put my baggage here ?

是否可替我更换座位?Could you change my seat, please?

我是否可将座位向后倾倒?(向后座的乘客说)May I recline my seat?

我是否可抽烟?May I smoke?

需要什么饮料吗?What kind of drinks do you have?

机上提供那些饮料?What kind of drinks do you have?

咖啡、茶、果汁、可乐、啤酒和调酒。We have coffee, tea, juice, coke, beer and cocktails.

晚餐想吃牛肉、鸡肉或是鱼?Which would you like for dinner, beef, chicken or fish? 请给我加水威士忌。Scotch and water, please.

请给我牛肉。Beef, please.

我觉得有些冷(热)。I feel cold(hot).

请给我一个枕头和毛毯。May I have a pillow and a blanket, please? 我觉得有些不舒服，是否可给我一些药?I feel a little sick, Can I have some medicine? 还有多久到达檀香山?How much longer does it take to get to Honolulu? 这班班机会准时到达吗?Will this flight get there on time? 我担心能否赶上转机班机。I'm anxious about my connecting flight. 请告诉我如何填写这张表格?Could you tell me how to fill in this form? 我要订9月15号到纽约的班机。I'd like to make a reservation for a flight to New York on

September 15th.

408次班机何时抵达,What time does Flight 408 arrive?

机票多少钱,How much is airfare?

我想要确认我预订的机位。I’d like to reconfirm my plane reservation please.

盥洗室在哪里,Where is the lavatory,

你有中文报纸吗,Do you have Chinese Newspaper,

我会冷，请给我一条毯子好吗,I feel cool， may I have a blanket,

可不可以给我一副扑克牌,May I have a deck of playing cards,

请出示您的护照。May I see your passport， please,

您要在美国待多久,How long are you going to stay in America,

我会留在美国一个星期。I will stay for one week.

您此行的目的为何,What is the purpose of your visit,

您有任何东西要申报吗,Do you have anything to declare,

我没有东西申报。I have nothing to declare.

对不起，哪里是行李提领区,Excuse me, where is the baggage claim area? 行李遗失申报处在哪里,Where is the lost luggage office? 我可以在哪里找到行李推车,Where can I get a luggage cart? 我要把一万元台币换成美金。I'd like to change NT$10,000 into U.S. Dollars, please.

你能告诉我在哪里兑换外币吗,Can you tell me where to change money? 你们接受旅行支票吗,Can you accept travelers checks? 汇率是多少,What's the exchange rate?

范文五：与动物相关的英文谚语

与动物相关的英文谚语

[真诚为您服务]

1.Bird

(1) Kill two birds with one stone. 一箭双雕;一举两得。

(2) A bird in the hand is worth two in the bush. 双鸟在林不如一鸟在手。

(3) Birds of a feather flock together. 物以类聚，人以群分。

(4) It ;s an ill bird that fouls own nest. 家丑不可外扬。

(5) Fine feathers make fine birds. 人要衣装，马要鞍。

(6) A bird is known by its note， and a man by his talk.

听音识鸟，闻言识人。

(7) Each bird loves to hear himself sing. 鸟儿都爱听自己唱。(自我欣赏)

(8) You cannot catch old birds with chaff.(粗糠)。 用粗糠捉不住老鸟。(有经验的人难骗。)

(9) Birds in their little nests agree. 同巢之鸟心儿齐。

2. Cat

(1) A cat has nine lives.猫有九条命;吉人天相。

(2) Cats hide their claws. 知人知面不知心。

(3) All cats are grey in the dark…… 黑暗之中猫都是灰色的。(人未出名时看起来都差不多。)

(4) A gloved cat catches no mice. 戴手套的猫，老鼠抓不到。(不愿吃苦的人成不了大事业。)

(5) When the weasel and the cat make a marriage， it is a very ill presage. 黄鼠狼和猫结亲，不是好事情。)

(6) Who will bwll the cat, 谁去给猫系铃,(谁愿意为大家冒风

险,)

(7) The cat shuts its eyes when stealing cream. 帽偷吃奶油的时候总是闭着眼睛。(掩耳盗铃)

(8) There are more ways of killing a cat than by chokingit with butter. 杀猫的办法很多。(达到目的的途径很多。)

(9) Care kill a cat. 忧虑愁死猫。

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