赤道國 的英文怎麼說
中文拼音 [chìdàoguó]
赤道國
英文
the equatorial country- 赤 : Ⅰ形容詞1. (紅色) red 2. (忠誠) loyal; sincere; single-hearted 3. (光著; 裸露) bare Ⅱ名詞(姓氏) a surname
- 道 : Ⅰ名詞(道路) road; way; route; path 2 (水流通過的途徑) channel; course 3 (方向; 方法; 道理) ...
- 國 : Ⅰ名詞1 (國家) country; nation; state 2 (姓氏) a surname Ⅱ形容詞1 (代表國家的) national; of ...
- 赤道 : 1. [地] (地球赤道) the equator 2. [天文學] (天球赤道) the celestial equator
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Like burroughs, researchers compare the equatorial regions of mars to the american southwest
如同巴勒斯一般,研究人員把火星的赤道地區比擬成美國西南部。The united states is north of the equator.
美國位於赤道以北。Embassy of the republic of equatorial guinea ?
赤道幾內亞共和國大使館?Chinese embassy in the republic of equatorial guinea
中華人民共和國駐赤道幾內亞共和國大使館Equatorial guinea, most of which is an island off western africa, will pay for the contract
赤道幾內亞的大部分領土是非洲西部海岸外的一座島嶼,上述合同所需經費將由該國支付。Both banks survived the inter - war years but the world trade slump led to the closure of operations in the canary islands, liberia, the netherlands, and equatorial guinea
兩家銀行都在兩次大戰中存活下來,但是國際貿易的減少使得加那利群島賴比瑞亞荷蘭赤道幾內亞的分行被迫關閉。Uganda is a land locked country, situated in east africa. it shares its borders with the countries of kenya in the east, sudan in the north, democratic republic of congo in the west, tanzania in the south. uganda is crossed by the equator at mid southerly level
烏干達是東非的一個內陸國家,東部與肯尼亞為鄰,北向蘇丹,西臨剛果共和國,南倚坦尚尼亞,而赤道橫過中部稍南處,國家面共197 , 097平方公里,人口達22 , 210 , 000 , 1962年10月脫離英國獨立。The countries south of the equator are in the southern hemisphere
赤道以南的國家是在南半球。It also explain that the correlation between ssta of kuroshio and the change of wind field in equaroral mid - pacific is results of air - sea interaction ; however, when time comes into summer, the instance status of ocean is different from the last winter to next early springtime, the sea surface temperature turn into the definitive factor, so the increase of heat flux in may to jun month which is realized by absorbing more heat from the sun radiation results in the decrease of sst in kuroshio in the season of jun - jul. finally, during the aug to dec season of next year, the sst of kuroshio is increasing again
最後分析了黑潮海溫與夏季東亞大氣環流及我國降水的時滯關系,發現:當前冬黑潮區域海溫異常偏高時,後期夏季亞洲低壓的強度減弱,西北太平洋副熱帶高壓強度加強,而且位置西伸、偏北,梅雨鋒位置偏南,長江中下游地區降水偏多,北太平洋冬季海域的海溫分佈呈+ 、 - 、 +趨勢(順序為赤道中東太平洋、西北太平洋、我國近海) ;反之亦然。Thus, it can be clearly recognized that the global continents located at near equator and southern hemisphere, showed the characteristics of range along latitude ; chinese continental blocks still located among the laurentia, siberia and gondwana in paleozoic ; following the fast moving of siberia plate to northwards, the amalgamation in north - south direction at the western parts of laurentia and gondwana, subducted the lapetus and rheic oceans, until to form the uniform pangea in the late stage of paleozoic ; however australia and india plates in eastern gondwana move and disperse gradually to southwards, to extend crust and form the paleo - tethys ocean ; the chinese continental blocks and adjacent blocks still located in paleo - tethys ocean, preserved the status of dispersion, gradually moving to northwards, showed the characteristics of range along north - south orientation, until carboniferous and triassic a series of local collisions happened in tianshan - hing ' anling, kunlun, qinling - dabie, jingshajiang and shaoxing - shiwandashan zones, thus the most part of chinese continental blocks amalgamated to eurasia continent
由此可以清晰地看出,在古生代早期全球各大陸的主要部分都位於赤道附近及南半球,大致表現為沿緯度、呈東西向排列的特徵,中國及鄰區的小陸塊群在古生代始終都處在勞倫大陸、西伯利亞與岡瓦納大陸之間;隨著西伯利亞大陸的快速北移,在勞倫大陸與岡瓦納大陸的西部地區發生南北向拼合,亞皮特斯洋和里克洋的消亡,到古生代晚期形成統一的泛大陸;而岡瓦納大陸的東部(澳大利亞和印度等)則逐漸向南移動、離散,地殼張開,構成古特提斯洋;中國及鄰區的小陸塊群則一直處在古特提斯洋中,保持離散狀態,總體上緩慢地向北運移,並逐漸轉為近南北向的排列方式,石炭紀到三疊紀才在天山興安嶺、昆侖山、秦嶺大別、金沙江和紹興十萬大山等地段發生一系列局部性的陸陸碰撞,使中國大陸地塊的大部分逐漸併入歐亞大陸。This paper reported the general situations of tuna fishery in indian ocean in recent ten years, and studied die fishing efforts, catch, cpue, and fishing grounds of two long - line crafts from zhonglu oceanic fishery co. ltd in equatorial waters of indian ocean in 2002, in order to gave the new fishery information to the producer, and to improve the technique of our tuna long - line fishery
為提高我國遠洋金槍魚延繩釣漁業的技術水平,並為我國相關生產企業提供產業發展的最新信息,本文報道了印度洋海域金槍魚漁業近十年的生產概況,並以中魯遠洋漁業股份有限公司兩條大型金槍魚延繩釣漁船2002年的生產數據為基礎,對印度洋赤道附近海域金槍魚延繩釣漁業的捕撈努力量、漁獲量、單位捕撈努力量漁獲量及作業漁場等進行了初步研究。( 4 ) the correlations are significant between the sth position index and the general circulation. in the westerly ( easterly ) year, equatorial westerly is weaker ( stronger ), cross - equatorial flow is weaker ( stronger ), south china sea summer monsoon is weaker ( stronger ), the yangtze river valley westerly is stronger ( weaker ), which has the positive ( negative ) effect on the maintenance of rain band over the yangtze river valley, so the rainfall is more ( less ) in this area and it is hit by floods ( droughts ), vice versa
( 4 )本文運用定義的副高指數研究了六月份副高偏東偏西年份的大型環流特徵及其對我國東部天氣的影響,風矢量場和相關場分析結果表明:副高偏西(東)年,赤道西風減弱(增強) ,越赤道氣流偏弱(增強) ,南海夏季風偏弱(強) ,而長江流域西風增強(減弱) ,有(不)利於雨帶在江淮流域維持,該地區降水偏多(少)易澇(旱) 。Further, correlation analysis is used to the summer rainfall and four seasonal north pacific ssta, the results suggest north pacific ssta which notability cause the summer rainfall anomaly over eastern china are prophase winter ssta of kuroshio region of northwestern pacific, prophase spring ssta of middle and eastern equatorial pacific and summer ssta of west wind drift region
進一步對上述東部夏季降水異常區夏季降水與春夏秋冬太平洋海溫異常作相關分析,表明對中國東部夏季降水有顯著影響是:西北太平洋黑潮海區前期冬季海溫異常、赤道中東太平洋前期春季海溫異常、中高緯太平洋西風漂流區同期夏季海溫異常。The tobacco steep d in rum, only i did not take so much as before, nor did i chew any of the leaf, or hold my head over the smoke ; however, i was not so well the next day, which was the first of july, as i hop d i shou d have been ; for i had a little spice of the cold fit, but it was not much
晚上,我又喝了點浸了煙葉的甘蔗酒,因為我感到,正是昨天喝了這種藥酒,身體才好起來,這次我喝得不多,也不再嚼煙葉,或烤煙葉熏頭。第二天,七月一日,我以為身體會更好些,結果卻有穿越赤道不會失去時間。在這里,魯賓遜也許頭腦里想到的是日界線,即83國際日期變更線。Data used in this work are north pacific ssta, 160 stations precipitation of china, and ncep reanalysis data. main results are as follow : ( 1 ) it is found that a apparent transition of north pacific ssta in later 1970 ' s : eastern and middle - equatorial pacific ssta turns from cold to warm with area extending, and mid - latitude pacific ( west wind drift zone ) turns from warm to cold. during this transition of ssta, different characters also appear in el nino and la nina : before 1976, la nina happens more frequently, and its duration is longer, el nino zone develops from negative ssta in the early stage ; after 1976, el nino happens a little bit frequent and longer with more intensity than before, el nino zone develops from positive ssta in the early stage ; the course of ssta variation has an enso cycle of 2 - 6 years, annual oscillation of 8 - 9 years, and decadal variation of about 22 years
本文採用1950 - 1999年北太平洋海表溫度( sst ) 、中國160站夏季降水和ncep再分析的歐亞500hpa高度場等資料,利用eof 、 svd 、小波分析、合成分析和相關分析等方法,在分析北太平洋海溫時空分佈特徵的基礎上,著重探討了海溫異常及其年代際變化對我國東部降水的影響,並對降水、高度場和海溫三者之間的關系進行了分析,以試圖尋找三者異常之間可能的聯系,主要結論如下: ( 1 ) 1976年前後,北太平洋海溫經歷了一次明顯的轉變,赤道中、東太平洋厄爾尼諾海區由冷轉暖,暖水范圍增大,中緯度西風漂流區海溫由暖轉冷;在這樣的年代際背景下,厄爾尼諾、拉尼娜事件在不同的時期也有不同的特徵:在76年前,拉尼娜事件發生頻率高,持續時間長,事件起始於負海溫距平;而76年後,則是厄爾尼諾事件發生頻率略高,持續時間長,強度增大,事件起始於正海溫距平。Those running around the world, parallel to the equator, are called lines of latitude
那些國境線著地球,和赤道平等的線叫緯線。Remarkable areas are the equatorial west pacific, north china, equatorial central america, north of bengal gulf and nepal, eastern australia, west india and south pakistan, east of lena river and west europe and wilkes in antarctic
顯著的地區是:赤道西太平洋區、中國的華北、赤道中美洲區、孟加拉灣北部及尼泊爾、東澳大利亞區、印度西部及巴基斯坦南部、勒拿河以東地區,西歐及南極的威爾克斯等區域。The features of interannual relationships and the decadal variabilities of interannual relationships between summer 850hpa cross equator flows of eastern hemisphere and enso and china summer rainfall are analyzed by using ncep / ncar reanalysis data, sea surface temperatures data of hadley center and rainfall data of 160 stations of china
利用1948 2002年ncep ncar再分析風場、高度場和海溫資料, 1951 2000年中國160站降水資料,分析了東半球夏季低空各支越赤道氣流與enso循環及中國夏季降水的關系及其年代際變化。The relationship between cef and china summer rainfall and that between cef and tropical cyclone frequence ( tcf ) in the northwest pacific ( nwp ) are investigated. lt is found that the several branches of cross - equatorial flow have different interannual variability. periodicity and interdecadal variability. the five channels in the lower troposphere in the monsoon region of the eastern hemisphere have different relationships with china summer rainfall. the results also show that there are obvious relation between the interannual variatin of cef and tcf from july to october in the northwest pacific
確定了東半球季風區對流層高低層各支越赤道氣流通道的位置,並探討了越赤道氣流與我國夏季降水和西北太平洋上熱帶氣旋發生頻數的年際變化之間的關系。結果表明:季風區夏季的幾支越赤道氣流具有不同的年際變率、周期以及年代際的變化特徵。夏季季風區對流層低層的5支越赤道氣流的強度與我國夏季降水呈不同的相關型。Mpri developed an integrated team of defense, security, and coast guard experts to provide a detailed set of recommendations to the government of equatorial guinea concerning its defense, littoral, and related environmental management requirements, as well as detailed implementation processes
Mpri制定了綜合組的國防安全,和海岸警衛隊專家提供一套詳細的建議,赤道幾內亞政府關于日本的防衛,濱海,以及相關的環境管理需求,以及詳細的實施進程分享友人