tropical pacific 中文意思是什麼
tropical pacific
解釋
熱帶太平洋-
Inter - decadal change of sea surface temperature and its interaction between tropical pacific and indian ocean in summer and winter
印度洋海表溫度年際異常的年代際變化 -
The subduct ion sign propagates toward the western tropical pacif ic ; and the decadal sign from the western tropical pacific propagates toward north - east. they meet at about 160 meter in depth in subtropical pacific
從北太平洋窗口區潛沉的海溫年代際信號沿西南路徑傳播到副熱帶地區，在溫躍層160m上下與熱帶西太平洋向東北傳播的海溫異常信號會合。 -
3 ) the upper ocean participates the process of air - sea interaction both in winter and summer in the tropical pacific but only in winter in the north pacific
3 ）淺層海洋參與海氣相互作用在熱帶太平洋區域冬、夏均存在，而在北太平洋區域僅限於冬季。 -
On the surface of msta, there exists true dipole mode in the indian ocean, that ' s to say that if the temperature anomaly in the western indian ocean is positive, it is much likely that there is negative anomaly in the eastern indian ocean. dipole mode also exists in the pacific as that in the indian ocean. by virtue of the walker circulation and the similar circulation above the indian ocean, it is showed that the air - sea interaction events in the tropical pacific and the indian ocean develop with each other at the same time
由於在次表層海溫距平極值面上，熱帶西、東印度洋的海溫距平呈真正意義的偶極子模態，即當西印度洋海溫距平為正（負）時，東印度洋海溫距平為負（正） ，偶極子模態的海溫距平分佈在熱帶太平洋同樣存在，兩大洋海溫距平的偶極子模態間有密切的聯系，結合walker環流和印度洋上空的類似walker環流，進而指出熱帶印度洋和太平洋海氣相互作用事件是協調發展的。 -
4 ) air - sea interaction retain its character throughtout the seasonal cycle in the tropical pacific, but it is not the same in the north pacific ; and there are also relationships in the two areas : 1 ) for the interdecadal time scale, there is the same abrupt change both in the north pacific and in the tropical pacific, especially in winter
4 ）熱帶太平洋區域海氣相互作用有較好的季節一致性；而北太平洋區域海氣相互作用季節差異較大。區域間主要聯系為： 1 ）兩個區域主要的年代際躍變點出現時間接近，這在冬季反映最明顯。 -
If a decadal positive temperature anomaly occurs in the eastern tropical pacific, the atmospheric response excites a anticyclonic wind stress anomaly in the east of australia, which will lead to generate a negative temperature anomaly in the western tropical south pacific
當熱帶東太平洋的海溫為暖異常，它將激發澳大利亞的東部沿岸的大氣產生反氣旋性風應力異常，在這種風場的作用，下方海水向四周輻散，導致熱帶西南太平洋的溫躍層變淺，產生負的溫度異常。 -
Based on ncep / ncar reanalysis sst and wind data set and fsu wind stress data, the dynamical roles of atmosphere over the tropical pacific on ocean are diagnostically analyzed. by using a dynamical ocean model over tropical pacific, the importance of dynamical roles of different areas atmosphere on ocean is studied. in the part iii of this work, a intermediate coupled model ( icm ) is employed to study ssta forecast experiment
本文用ncep / ncar再分析海表溫度、風應力和風場資料就熱帶太平洋地區大氣對海洋的強迫進行診斷分析，並用一個熱帶太平洋動力海洋模式研究不同區域大氣對海洋強迫作用的重要性，在此基礎上用一個中等復雜程度的耦合模式對enso事件進行預報試驗。 -
A simple tropical pacific atmosphere - ocean couple model with enso cycle characteristics
循環基本特點的簡單熱帶海氣耦合模式 -
The correlations between wind stress anomaly over the tropical pacific and ssta using svd analysis shows that the wind stress patterns are corresponding to enso eigenmode. it is suggestive that the explanation, simulation and prediction of el nino / la nina evolution in space - time should not be based on a single eigenmode but on their interaction, with emphasis on the fact that superimposition and phase locking are important factors of the event cycle
對緯向、經向風應力距平與ssta做svd分析赤道太平洋地區風應力異常和海表溫度異常之間的相關關系顯示，經pop分析得到的緯向、經向風應力的空間型與elnino lanina時的ssta具有很好的對應關系。 -
Because the system error is ineluctable for mode, it is necessary to correct the simulation fielde effectively. in this paper, based on the idea of combined eof correction, the interannual simulation of sea surface wind stress anomalies of the tropical pacific ocean by lap two - level atmosphereic model have been corrected, result of corrected erperiment shows that the corrected field is more similar to the observation field, especially on the distribution of the space. three prediction experiments also shew that correcting scheme of combined eof can improve the interannual prediction veracity of model
在本文中，基於「聯合自然正交展開誤差訂正」的思想，將中科院大氣物理研究所兩層大氣環流模式輸出的熱帶太平洋海表風應力異常的跨年度模擬場進行訂正，訂正試驗的分析結果表明，訂正後的熱帶太平洋海表風應力距平場與相應觀測場年際變率分量的相似程度遠遠好於模式模擬的結果，尤其是在空間分佈方面的改善非常顯著；三組跨年度訂正檢驗結果也表明，訂正後的跨年度預測結果明顯好於模式的預測結果。 -
The negative temperature sign can move to the mid tropical pacific then propagates eastward the eastern tropical pacific and change the original positive temperature anomaly. a similar evolution but with an opposite sign follows subsequently. the whole cycle for the enso decadal variability needs about 14 years
負的海溫異常可向北傳輸到熱帶西太平洋和熱帶中太平洋，然後東傳到熱帶東太平洋，使其原有的暖異常海溫被負的海溫異常取代，然後再進行反位相的循環，整個循環過程所需的時間約為14年。 -
Impacts of sea surface temperature in the tropical pacific on interannual variability of madden - julian oscillation in precipitation
熱帶太平洋海表溫度年際變化對降水季節內振蕩的影響 -
Base on this study, the numerical forecast of 2000 ' s tropical pacific ssta has been done. it shows that it is weak la nina event in 2000
對2000年的熱帶太平洋海表溫度作了試預報，預測結果顯示2000年是弱lanina年。 -
O which commenced in the latter half of 2006 finally dissipated this february. sea surface temperatures over the central and eastern tropical pacific have generally resumed normal figure 1
在2006年下半年開始發展的厄爾尼諾現象已經在今年2月消退，熱帶太平洋中部和東部的海表溫度普遍回復正常圖一。 -
Diagnostic analysis and contrast are performed in air - sea data and their interaction between the north pacific and the tropical pacific by means of harmonic analysis and svd
使用諧波分析及奇異值分解（ svd ）方法分析比較了北太平洋、熱帶太平洋區域的海氣資料及海氣相互作用。 -
2 ) the leading svd modes of interdecadal variability are indicative of stronger statistical significiance in the north pacific than in the tropical pacific, while the conclusion is contrary as for interannual variability
2 ）年代際變化海氣相互作用北太平洋區域較熱帶太平洋區域顯著，年際變化海氣相互作用熱帶太平洋區域較北太平洋區域顯著。 -
The surface of the maximum sea temperature anomaly ( msta ) was constructed from the subsurface sea temperature anomaly data in the tropical pacific from 1955 to 2002. it is quite similar to the depth distribution of the 20 ? c isotherm, which is usually used to represent the center of the thermocline layer
利用1955 - 2002年48年熱帶、副熱帶太平洋地區次表層溫度距平資料，構造了溫度距平極值深度分佈的曲面圖（ msta ） ，它很接近20溫度面的深度分佈，因此有理由認為這一深度曲面很接近熱帶溫躍層的深度面。 -
Diagnostic results show that the westerly wind stress anomaly and convergent meridional wind stress anomaly over the tropical pacific correspond to the every el nino, and the easterly anomaly and divergent meridional wind stress anomaly correspond to the vanishing of el nino
通過研究表明，每次elnino事件在熱帶太平洋都伴隨著西風應力異常以及向赤道輻合的經向風應力異常，東風應力異常及向兩極輻散的經向風應力異常與elnino消亡對應。 -
Results show that the interdecadal anomalies are more significant in the variance of the system anomaly in the north pacific ( np ), and the interannual and interdecadal anomalies are about equivaleut in the tropical pacific ( tp ) ; the interdecadal change characters of the surface ( shallow ) layer of the ocean and the atmosphere aloft are unanimous in the same season and region, and their transition from a low mode to a high mode both occurred from the end of 1970s to the beginning of 1980s, with an exception for july in the np, which is related to the stability of the stratification of sea temperature within the sub - surface layer ; the interannual scale air - sea anomalies are associated with enso, is most typical for january, then july in the tp, followed by january in the np, and there is no visible relationship for july in the np
在海氣系統異常的方差構成中，北太平洋區域以年代際異常為主，熱帶太平洋區域年際和年代際異常相當；表（淺）層海洋與大氣的年代際變化特徵對同一季節、區域是一致的，且20世紀70年代後期到80年代初均發生由低模態向高模態的轉變；北太平洋區域的7月與此不同，這與該季節近表層海溫層結穩定有關；年際尺度的海、氣異常與enso有關，且以熱帶太平洋區域1月最典型， 7月次之，北太平洋區域1月再次之， 7月無明顯關系。 -
Using necp / ncar reanalysis. gisst2. 3b data - set, the inter - decadal variations in the relationship between the tropical pacific and indian ocean inter - annual anomalies are examined
利用ncep ncar再分析資料、全球海溫海冰gisst2 . 3b資料，分析了熱帶海洋地區海氣系統內部聯系的年代際變化特徵。
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