interannual variability 中文意思是什麼
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Principal modes of interannual and decadal variability of summer rainfall over south america
南美夏季降水的年際，和年代際變化的主要模態。 -
The apparent characteristics of interdecadal variability of interannual relationship between winter sea - ice extent of davis strait and summer, july and august rainfall of north china are : the strongly negative correlation between winter sea - ice extent of davis strait and summer rainfall of north china turns into bad correlation
冬季戴維斯海峽海冰面積與華北7月降水在年際變化尺度上有明顯的反相關關系。冬季戴維斯海峽的海冰面積增多（少） ，同年華北7月降水偏少（多） 。 -
All the turn - point year is around 1974. another feature of interdecadal variability of interannual relationship between winter sea - ice extent of davis strait and summer, july and august rainfall of 160 stations is that the interannual correlation pattern have changed from east - west pattern to " + - + " north - south pattern around 1974. the interdecadal characteristics of correlation distribution pattern of interannual relationship between winter sea - ice extent of davis strait and summer, july 500hpa height of northern hemisphere are : " - + - " pattern from the beginning of novoya zemlya island, by way of balkhash lake to japan sea which is strongly negatively correlated with the rainfall of north china at the same period before 1974 and " + - " pattern from the beginning of ural mountains, by way of bujr lake to hetao basin which is badly correlated with the rainfall of north china at the same period after 1974
冬季戴維斯海峽海冰面積與華北夏季及7 、 8月降水年際關系有明顯的年代際變化特徵：其與夏季總降水的年際關系由1974年前較好的負相關在1974年後變差，與7月降水的年際關系由1974年前較好的負相關在1974年後變弱，與8月降水的年際關系由1974年前較好的負相關在1974年後變差；另一方面，其與中國160站夏季及7 、 8月降水的年際關系在1974年前後發生變化的主要特徵是：與夏季總降水、 7月、 8月降水的年際關系由1974年前的相關系數分佈呈「東西型」變為1974年後相關系數分佈呈「 - + - 」的「南北型」 。 -
The features of the interannual relationship between winter sea - ice extent of davis strait and rainfall of north china and the interdecadal variability of its interannual relationship are analyzed by using uk / gisst sea - ice data - set of hadley, monthly 500hpa height field of ncep / ncar reanalysis data and monthly rainfall data from 160 stations in china
選用英國hadley氣候研究中心的uk gisst海冰面積指數資料集、 ncep ncar逐月再分析資料500hpa位勢高度場資料和中國160站降水資料，分析了冬季戴維斯海峽海冰面積變化與華北夏季降水年際關系及其年代際變化。 -
92km3 in 94 - 95. the comparison indicate that interannual variability of simulated and estimated outflow are very close, both of them have an upward trend in the 20 years. but 20 years average quantity of simulated outflow is less than the quantity of estimated outflow. the simulated outflow is about 90 % of estimated. for study the relationship between temperature and sea ice of arctic and the velocity of wind how to influence arctic sea ice, some ideal modeling are run
與衛星資料反演流出量比較結果表明，模擬流出量和衛星反演流出量的年際變化非常一致，總體上都有增多的趨勢，但在數值上有一定差距，平均而言冬季海冰面積流出量，反演值小於模擬值，而全年則是模擬值小於反演值，約是衛星反演流出量的90 。 -
The precipitation in middle and lower reaches of yangtze river response to the positive abnormal in eurasian continent and it also has the relationship with the interannual variability of the middle and high latitude of north atlantic sst and the west pacific warm pool
長江中下游降水對應于歐亞大陸的位勢高度正異常，長江中下游降水與北大西洋中高緯度和西太平洋暖池sst的年代際變率有關。 -
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 -
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 variation of sensible heat flux is dominated by air - sea temperature difference. interannual variability of turbulent heat fluxes is examined using svd, eof and mtm methods
熱帶太平洋enso事件通過對walker環流的調整減小熱帶大西洋itcz區的風速值，湍動熱通量亦隨之減小。 -
The result also shows that the heat storage anomaly in the scs has an obvious long - term variability which is a stable interannual variability from 1992 to 1998, an abrupt change to a high stage in 1998 continuing till 2001, and a tendency to reduce after 2002
本文得到的結果還顯示南海熱含量異常具有明顯的長周期變化，表現為： 1992 ~ 1998年基本保持比較穩定的年際變化特徵， 1998年之後，熱含量出現明顯的躍變，這一躍變一直維持到2001年，在2002年開始出現熱含量的遞減趨勢。 -
Based on the observation data such as coads and soda, the main climatological features of the tropical indian ocean and relationships of sea surface temperature ( sst ), heat budget with ocean dynamics and thermodynamics processes are analyzed ; the seasonal and interannual variability of the tropical indian ocean are well simulated using a ocean general circulation model ; based on the thermal equation and model output data, the variation mechanism of sst and heat budget are investigated in the tropical indian ocean ; besides, the effect of seasonal variation of wind stress, ekman pumping and horizontal diffusivity on the ocean current and heat budget are studied, using both ideal model and complex model
本文根據coads 、 soda等實際觀測資料，較全面的分析了熱帶印度洋主要的氣候特點，並研究了海表面溫度（ sst ） 、熱收支與海洋動力、熱力過程的聯系；利用全球海洋環流模式較好地模擬出熱帶印度洋的季節和年際變化；基於熱力學方程和海洋環流模式輸出結果，探討了熱帶印度洋sst和北印度洋熱量收支的季節和年際變化機制，進一步揭示了海洋動力過程在北印度洋熱平衡中的重要作用；在此基礎上，利用理想化的數值試驗與數值模擬結果相結合的方式，證實了風應力的季節變化和ekman抽吸，以及水平熱量擴散系數對北印度洋海洋環流和熱收支的影響。 -
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。 -
Based on the importance of heat flux variability to the earth ' s climate change and the dependence of the study about heat flux variability on the accuracy of heat flux data, this study will focus on the quality evaluation of heat flux datasets available and seasonal and interannual variability of latent and sensible heat fluxes in the tropical atlantic ocean
基於海表潛熱和感熱通量的時空變化在全球變化中的重要性和海表潛熱和感熱通量研究對熱通量資料產品精度的依賴性，本文重點就現有熱通量資料產品的質量和熱帶大西洋海表潛熱和感熱通量的季節和年際變化開展較深入的研究。 -
Interannual variability of the indonesian throughflow - preliminary simulated results of a variable - grid global ocean model
一個全球變網格海洋模式的初步模擬結果 -
The analysis of the probability of maximum temperature in south china during the summer of 2003 revealed that this event can ' t be considered as a reflection of long time trends, but rather than an episode under interannual variability
分析最高氣溫的概率分佈特徵，得出2003年夏季江南、華南地區出現的極端酷熱天氣，只是年際變化的表現，而不是長期變化趨勢的反映。 -
The results show that although there are somewhat systematic errors in the coupled model, the model simulates the basic features of seasonal cycle and interannual variability of sea surface height to the considerable extent, in order to examine the impact of indonesian through flow ( itf ) on the seasonal cycle and interannual variation of sea surface height, a sensitivity experiment is accomplished, in which the indonesian passage is closed fully in the coupled model
結果表明，盡管耦合模式存在一定的系統誤差，但仍然能相當程度上夠模擬出海面高度季節和年際變化的基本特徵。同時為檢驗模式中印度西亞穿越流（ itf ）對海面高度季節和年際變化的影響，本文還進行了印度尼西亞海道完全關閉的敏感性試驗，與控制試驗結果對比表明，印尼穿越流對季節變化的影響不大，但可以顯著影響熱帶太平洋和印度洋年際變化的特徵。 -
Analysis on characteristics of interannual variability of the south asian summer monsoon
南亞夏季風年際變化特徵分析 -
An analysis of the interannual variability of precipitation in the tropical indian ocean
熱帶印度洋降水的年際變化特徵分析 -
At the same time, the ability of simulating the sst ' s interannual variability of the model was examed
同時還檢驗了模式對海溫年際變化的模擬能力，得到了較好的結果。 -
It is shown that olr spread eastward more clearly in the eastern hemisphere, and the x is persistently spread eastward in both hemisphere ; the interannual variability of the spread of mjo is evident, with the intensity weakening during el nino events and sometimes spreading westward in individual years
氣候上，在沿赤道的傳播中， olr東半球較西半球明顯， x東、西半球無顯著差別；兩種要素季內振蕩沿向東南路徑的傳播較向東北路徑的傳播特徵明顯。異常表現為季內振蕩強度在elnin 。
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