赤道平面 的英文怎麼說

中文拼音 [chìdàopíngmiàn]
赤道平面 英文
equationial plane
  • : 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
  • : 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) ...
  • : Ⅰ形容詞1 (沒有高低凹凸 不頃斜) flat; level; even; smooth 2 (高度相同; 不相上下) on the same l...
  • : Ⅰ名詞1 (頭的前部; 臉) face 2 (物體的表面) surface; top 3 (外露的一層或正面) outside; the ri...
  • 赤道 : 1. [地] (地球赤道) the equator 2. [天文學] (天球赤道) the celestial equator
  1. By translating this real cubic system into a complex planar system, an applicable linear algebraic recursion formula of the equator and the first 6 quantities of the equator are given

    將這類實三次系統轉化為復系統研究,給出了系統環量的易於計算的線性代數遞推公式。
  2. The working projection plane is taken at the equatorial plane corresponding to the ground surface.

    工作投影赤道平面相當于地
  3. Instead of assuming the earth to be a perfect sphere, this function takes into account the actual polar flattening of the earth and the equatorial bulge, which gives a much more accurate computation between the given coordinates

    它沒有假設地球是一個完整的球,而是考慮了地球的極軸扁率和鼓起率,這樣就給出了兩個坐標間更精確的距離。
  4. It is formed by fusion of vesicles from the golgi apparatus, resulting in a flattened membrane - bounded sac spreading across and effectively divding the cell

    高爾基體產生的小泡在上彼此融合而形成有膜包圍的板,即細胞板。
  5. 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,而橫過中部稍南處,國家共197 , 097方公里,人口達22 , 210 , 000 , 1962年10月脫離英國獨立。
  6. During the el nino ( la nina ) events, the negative ( positive ) sst anomaly occurs and the corresponding the olr mjo intensity weakens ( enhances ) in the tropical western pacific ; at the same time, the positive ( negative ) surface westerly anomaly leads to positive ( negative ) mld anomaly, and the corresponding sst mjo intensity weakens ( enhances ) in the equatorial eastern pacific, 4 ) the interdecadal variation of the atmospheric mjo intensity took place distinctly in 1970s in the tropical western, northwest and eastern pacific, with the stronger intensity in the former than the back stage, and the interdacadal variation of sst is its cause

    Elnino ( lanina )事件中熱帶兩太洋sst出現負(正)異常, olr季內振蕩強度出現減弱(增強)的變化。 elnino ( lanina )事件中,洋出現地信風西風分量正(負)異常,並引起熱帶東太洋mld出現正(負)異常,造成熱帶東太洋sst季內振蕩強度出現減弱(增強)的變化。 4 )熱帶印度洋、熱帶西太洋和熱帶東太洋季內振蕩強度在上世紀70年代發生了明顯的年代際變化,均為前弱、后強, sst本身的年代際變化是其原因。
  7. The somali jet and the south china sea ( scs ) cef in the lower level play an important role in the onset of the south china sea summer monsoon ( scssm ). the somali jet is rapidly enhanced two pentads prior to the onset of scssm, thus accelerating the eastward extension of the westerly over the bay of bengal and leading to the eastward retreat of the western pacific subtropical high ( wpsh )

    低層的索馬里和南海越氣流對南海夏季風的爆發有至關重要的作用,在南海夏季風爆發前2候,索馬里急流有一次迅速的增強,這一增強有利於加速孟加拉灣地區西風的向東擴展,並使控制在南海的西太洋副高東撤;同時,南海越氣流的迅速增強也加速副高的北上,共同促使南海夏季風全爆發。
  8. The eni of el nino events is expressed by using differences of sea surface temperature in the area of equatorial east pacific 010s, 90180w. based on eni s definition, 25 el nino events and 26 la nina events from 1870 to 2000 are defined. and the starting and ending time of 1997 s strong el nino event is predicted six months ahead of the event by using eni s three periodical overlapping prediction method. the prediction offers great support to the accurate prediction of the flush flood occurred along nenjiang river in 1998

    使用東太洋010s , 90180w海水表溫度sst距值表徵厄爾尼諾拉尼娜事件指數eni 。根據eni定義出1870 - 2000年期間25次厄爾尼諾事件和26次拉尼娜事件,採用eni三周期疊加預報模式提前6個月預測出1997年強厄爾尼諾事件的開始和結束時間,為較準確預測出1998年嫩江特大洪水提供了預報依據。
  9. By structure the bounded cubic systems in the plane, we prove that : 1 ) the system ( 1 ) have distribution of critical point with 5 - 4 ( 5 critical points with index + 1 and 4 critical points with index - 1 ), 3 - 2, 2 - 1, + 1 ; 2 ) the bounded cubic systems in the plane which has only one critical point with index + 1 have at least 11 structures ; 3 ) the distribution of finity critical points of bounded cubic systems with same topological structure near the equator have different struction

    摘要通過構造有界的三次系統,證實了( 1 )其有限奇點的5 4 ( 5個奇點指標為+ 1 ,另4個奇點指標為1 ) 、 3 2 、 2 1 、 + 1四種分佈均可實現; ( 2 )僅有一個指標為+ 1的有限奇點的有界三次系統至少有11種類型; ( 3 )附近軌線拓撲結構相同的有界三次系統它們有限奇點的分佈可以有不同類型。
  10. The integrability conditions and coefficient conditions for the appearance of 5 and 6 limit cycles from the neighborhood of the equator are obtained. an example of cubic system with 6 limit cycles bifurcating from the equator is given for the first time

    同時計算出系統的前6個環量,得到了系統在鄰域的可積性條件及在附近分支出5個和6個極限環的系數條件,從而首次給出了一個三次系統在附近分支出6個極限環的計算實例
  11. On the other hand, the methods of reof analysis was also used to north pacific ssta on spring and summer. the middle and eastern equatorial pacific and the kuroshio region of northwestern pacific are two mostly anomaly regions

    另一個方,對太洋春季、夏季海表溫度進行reof分析,表明太洋海表溫度分佈具有明顯的區域特徵,其中最強的異常分佈區是中東太洋和西北太洋黑潮海區。
  12. If the axis of the cone(cylinder or plane)lies in the plane of the equator the aspect is transverse.

    如圓錐(圓柱或)軸位於赤道平面內,則成為橫軸。
  13. This was due largely to the development of an el nino in the year, which was characterized by above normal sea surface temperatures in the equatorial eastern and central pacific. the associated change in atmospheric steering flow caused tropical cyclones over the western north pacific to turn towards the north before entering the south china sea

    厄爾尼諾是指在洋東部及中部出現海溫度異常變暖的現象,它導致大氣環流的改變,將北太洋西部的熱帶氣旋引導向北移動,相對減少了它們向西移入南海的機會。
  14. ( 5 ) the spring greenland sea - ice extent is larger ( smaller ) : then during the following summer the high of the japanese sea is stronger ( weaker ), and the low of the asian land is stronger ( weaker ), which make the pattern of low west and high east easily ( uneasily ) form ; the ascending movement over north china is strengthened ( weakened ) ; the summer monsoon of east asia is stronger ( weaker ), then the southeastern, warm and damp airflow towards the north china is stronger ( weaker ), and the cold airflow of the high level over the north china is also stronger ( weaker ), which make the convergence of the cold and warm air over north china easily ( uneasily ) form ; the sst of the east pacific ocean is lower ( higher ), while the sst of west wind drift is higher ( lower )

    ( 5 )春季格陵蘭海冰積偏大(小) :後期夏季日本海高壓偏強(弱) ,而大陸上低壓也偏強(弱) ,易(不易)形成西低東阻的形勢;華北地區的上升運動增強(減弱) ;東亞夏季風偏強(弱) ,向華北地區輸送的西南暖濕氣流偏強(弱) ,而對應高空華北地區上空冷空氣活動偏強(弱) ,利於(不利於)華北上空冷暖空氣的交匯;夏季東太洋海溫偏低(高) ,西風漂流區海溫偏高(低) 。在以上的環流背景下,華北夏季降水偏多(少) ,易澇(旱) 。
  15. It lies on the map like the top half of a broken cane, parallel with the equator but a long, long way north.

    它在地圖上就象一根破爛手杖的上半節,和南行的遙遙相望。
  16. The working projection plane is taken at the equatorial plane corresponding to the ground surface

    工作投影赤道平面?相當于地
  17. Computer programming realization of the projection figure of pole point on equator plane of cubic crystal system plane

    極射赤道平面投影圖的計算機實現
  18. Any of the imaginary lines representing degrees of latitude that encircle the earth parallel to the plane of the equator

    緯線,緯度圈與赤道平面行且環繞地球用來表明緯度高低的許多假想線中的任意一條
  19. Material in the equatorial region of the cloud ? that is, in the plane perpendicular to the rotation axis ? moves inward more and more slowly as rotation starts to balance the pull of gravity

    當轉動開始與重力的向內拉力衡時,位在整團雲氣的區域,垂直於轉軸的上的物質,會逐漸減緩向內移動的速率。
  20. Based on the analyses, it was found that if the subsurface warm pool is regarded as the beginning point, the warm or cold signal propagates initially eastward and upward along the equatorial surface of msta to the eastern pacific and stays there several months and then turns north, usually moves westward near 10 to western pacific and finally propagates southward to return to warm pool to form an off - equator closed circuit. it takes about 2 to 4 years for the temperat ure anomaly to move around the cycle. if the smta of warm ( cold ) water is strong enough, there will be two successive el nino ( la nina ) events during the period of 2 to 4 years

    ) a事件下/負海溫距信號的分佈和傳播「軌跡」 ,發現如果以暖池次表層為起點,則一般來說,暖水或冷水先是沿的極值深度向東、向上「傳播」或運動,到達東太海盆邊界附近后,分別轉向向北和向南運動,然後在南、北緯10左右再折向西運動,並在暖池的經度范圍內再作經向運動傳到暖地,即在南、北半球以為一邊, 「傳播」或運動路徑形成扁的閉合環路,溫度距運動一圈需時2 - 4年。
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