赤道波 的英文怎麼說

中文拼音 [chìdàobō]
赤道波 英文
equatorial wave
  • 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） ...
  • 波 : Ⅰ名詞1 （波浪） wave 2 [物理學] （振動傳播的過程） wave 3 （意外變化） an unexpected turn of even...
  • 赤道 : 1. [地] （地球赤道） the equator 2. [天文學] （天球赤道） the celestial equator
  1. Based on the epwp and wpwp in conjunction with abnormal north and west wind, a new possible iii mechanism is provided for the evolution of the 1997 / 1998 el nino. to be specific, the warm kelvin wave propagating to east excited by the abnormal west wind can suppress the cold upwelling flow in the eastern pacific, which, in turn, is favorable to the eastern pacific sst increase ; abnormal west wind can make the warm water of the wpwp east edge extend to east, which is conductive directly to eastern pacific sst increase ; the abnormal west wind propagating to east can make the sea surface warm water near two equatorial laterals converge to the equator by ekman drifting, which, in rum, strengthens the downwelling flow near the equator, leading to eastern pacific sst increase

    將東、西太平洋暖池及異常北風、西風一併結合起來考慮，提出1997 1998elnino事件發生、發展的一種新的可能機制：異常西風激發東傳的暖kelvin波對東太平洋的冷上翻流有抑制作用，從而有利於東太平洋海表溫度增加；異常西風驅動西太平洋暖池東端暖水向東伸展直接有利於東太平洋海表溫度增加；東傳的異常西風可以通過埃克曼漂流效應將赤道兩側的海表暖水向赤道輻合從而加強了赤道附近的下沉流，也有利於東太平洋赤道附近海表溫度增加。
  2. A preliminary analysis shows that the east - west asymmetry in the heliospheric equatorial plane is mainly attributed to the spiral structure of the interplanetary magnetic field

    初步分析表明，行星際磁場的螺旋結構是產生日球赤道面內雙重激波對結構東西不對稱性的主要原因。
  3. In order for the tide waves to move fast enough at the equator to keep up with the moon, the ocean would have to be about 22km deep

    即使潮波在赤道上移動的速度跟得上月亮，海洋深度必須為22公里左右。
  4. 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。
  5. This will include the kind of violence that is normally associated with pole shifts, the continents going up and down, huge tidal waves that are 100 feet high, the entire south pole moving to the equator at 1300 miles an hour and these kind of things, this may still occur

    這將包括這類猛烈，通常與磁極轉換聯系在一起，大陸上下起伏，巨大的潮汛波有100英尺高，整個南極以每小時1300英里的速度移向赤道以及這類的事情，這一切或許還要出現。
  6. A data assimilation experiment is carried out through combination the model with temperature measurements from the 165 e moorings on the equator, which collected by tao / triton ( tropical atmosphere and ocean project ) array of bugs

    並通過在赤道太平洋， 165 e ，熱帶大氣和海洋（ tropicalatmosphereandoceanproject ） ，即tao triton錨系浮標陣列觀測點，選取一段時間觀測資料，進行kalman濾波試驗。
  7. On the western side of the central normal of the disturbance source in the heliospheric equatorial plane, the double shock pair structure is more evident, and the longitudinal span is wider than those on the eastern side

    雙重激波對在子午面內相對擾動源中心法線基本對稱，而在赤道面內則不對稱：擾動源中心法線西側雙重激波對結構更為明顯，所跨經度范圍寬于東側。
  8. Such a response depends on the strength of the interplanetary shock : for a stronger shock, the new region current gets stronger, extends for a longer distance towards the equator, and reaches a lower latitude

    這一響應過程和行星際激波強度有關：激波強度越強，新生的區場向電流也越強，它向赤道方向延伸的距離也越大，能到達的緯度也越低。
  9. The east asia summer monsoon anomoly can affect the atmosphere circulation and climate in the east asia and pacific ocean regions through the western pacific subtropical anticyclone and the epa wavetrain. in the strong cross equator flow of 90 e years, there has more precipitation in the middle and lower reaches of yangtze river valley regions while there has less precipitation in the northeast china regions

    夏季低空90 e附近越赤道氣流較強時，東亞夏季風較強，西太平洋副熱帶高壓位置偏北， epa （東亞太平洋美洲）波列伸展緯度偏北，造成長江中下游夏季降水偏少，東北地區夏季降水偏多；夏季低空90 e附近越赤道氣流較弱時，情況則相反。
  10. In the same cloud band above the equator, the small swirls in the left - hand image have morphed into larger wave - like features in the right - hand photo

    在左圖赤道上同一雲帶中的小漩渦變形成了右圖中較大的波狀結構。
  11. Although the bivalve lineages dr jablonski studied spread out from the equator in waves, they did not become extinct in the wake of these waves

    盡管捷布朗斯基博士所研究的雙殼類世系隨著波濤從赤道開始蔓延擴散，但它們並沒有隨著波濤的消亡而一同絕滅。
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