water anomaly 中文意思是什麼

water anomaly 解釋
天然水異常
  • water : n 1 水;雨水;露;〈常作 pl 〉 礦泉,溫泉;藥水。2 〈常 pl 〉水體;水域;水道;海;湖;河;海域;...
  • anomaly : n. 1. 不規則,反常(現象),異常,破格。2. 畸形物。
  1. Based on analysis of geologic foundation record about pingzhuang basin, a lot of sino - foreign geothermal geology record and investigation of field geology, measuring of ground temperature in person and geo - chemical analysis of ascension spring, gushing water of fault, the fact that the anomaly of geothermal gradient of pingzhuang basin, which is in region of low geothermal gradient, is caused by redistribution of conduction - oriented geothermal heat flow which is result from upheaval and depression of basin foundation bed is pointed out. after the field of ground temperature is simulated under the background of conduction - oriented geothermal heat flow by means of ansys, the characteristic of ground temperature distribution of top surface of basin foundation bed ( yixian team ) is revealed. the sound condition of transmissibility fault and feeding water source, which are imperative in formation of the low - medium temperature geothermal system of convective type, is possessed in pingzhuang basin

    通過對平莊盆地基礎地質資料、國內外大量地熱地質資料的分析和野外地質調查、礦井實測地溫以及上升泉、斷層涌水的地球化學分析等工作基礎上,指出地處低地溫梯度背景區的平莊盆地地溫梯度異常是由於盆地基底隆起和坳陷引起傳導型大地熱流再分配所致;運用州sys數值模擬了大地熱流向地表傳導背景下的盆地地溫場,從而揭示了盆地基底(義縣組)頂界面地溫分佈特徵;闡明了盆地具有形成中低溫對流型地熱系統所必需的導水斷裂、補給水源等的良好條件,中低溫對流型地熱系統是地熱勘查的主要對象;圈定了平莊盆地北部朝陽溝?駱駝營子地熱勘查遠景區。
  2. In order to study the anomaly pattern of summer rainfall in north china and the cause responsible for the anomaly, the climate characteristics of summer rainfall in north china and related circulation pattern, water vapor transport and outgoing long - wave radiation ( olr ) were analyzed in detail in this paper. more attention was paid on studying the relationship between sea surface temperature anomaly ( ssta ) over the north pacific and summer precipitation anomaly in north china and an agcm was utilized to confirm the affection of ssta on the summer rainfall of the north china

    為了揭示華北夏季降水異常規律及其成因,本文詳細分析了華北夏季降水的氣候特徵及有關的環流特徵、水汽輸送特徵和向外長波輻射( olr )特徵,著重研究了北太平洋海溫異常與華北夏季降水異常的關系,並應用大氣環流模式初步驗證了北太平洋海溫異常對華北夏季降水的影響。
  3. For solving the problems that downward continuation of the space gravity anomaly can not be used in downward continuation of sea surface gravity anomaly, on the basis of prey principle used to compute gravity in the surface - layer of the earth, and with considering the density of sea water and sea bottom topography, two new methods are proposed

    摘要針對空間重力異常向下延拓方法不適用於海面重力異常向下延拓的問題,根據珀雷原理求地球表層內部重力的方法、海水密度及海底地形的特徵,提出了兩種海面重力異常向下延拓的演算法。
  4. Seasonal variations of water vapor transport over east asia monsoon region are studied, especially that in summer season. the results indicate that there are four vapor inflow corridors to fetch china : southwest corridor, south china sea corridor, southeast corridor and northwest corridor. it shows impact of south asia monsoon, south china sea monsoon, subtropical monsoon and middle latitude westerly belt on summer rainfall anomaly over china, respectively

    分析了東亞季風區水汽輸送的季節變化,並著重研究了夏季東亞季風區的水汽輸送特徵,指出夏季東亞季風區水汽輸送有四條通道到達中國大陸:西南通道、南海通道、東南通道和西北通道,分別體現了南亞季風、南海季風、副熱帶季風和中緯度西風帶對中國夏季降水的影響。
  5. Almost meanwhile, the north wind anomaly brings epwp warm water to equatorial vicinity by producing north ocean flow, which causes directly nino3 sst increase

    幾乎與此同時,北風距平通過產生北風吹流將東太平洋暖池暖水由北向南輸送至赤道附近直接導致nino3區海表溫度增加。
  6. Using monthly mean rainfall and temperature data in north - west of china ( nwc ), the characteristics of rainfall anomaly at rainy season in nwc and the inter - annual varieties of drought / flood are diagnosed by means of eof, reof and wavelet analysis et al. and the ncep / ncar monthly reanalyzed data are employed to analyse the evolution character of water vapor flux and it ' s divergence flux, 500hpa height and u, v wind field. results show that ( a ) the space distribution of rainfall anomaly can be separated into seven climate sensitive areas, the first and the third region have the same rought / flood trend

    本文使用西北(區) 168個站1961 2000年6 9月(主汛期)月平均降水、溫度資料,運用eof 、 reof 、小波分析等方法診斷了主汛期月降水異常和旱澇的年代際變化;同時利用ncep ncar月平均資料,分析了強(弱)季風年西北空中水汽通量及其散度場、 500hpa高度場、 u 、 v風場的演變特徵,結果表明: ( a )西北汛期降水可分為七個氣候異常區,第一、三異常區旱澇趨勢相同。
  7. On the paas - normalized plots, the parent granite and the granite weathering crust are enriched in lree without ce anomaly. while the groundwaters are also enriched in lree, they display significant negative ce anomaly, indicating the fractionation of ce during water - rock interaction. based on the study of two profiles of granitoid weathering crust, we concluded that ree concentrations in the groundwaters from the granitoid weathering crust are likely related to the continued chemical weathering, as well as the ree concentrations in the crust near the water table, clay concentration and the wate r ph values

    地下水與母巖、風化殼稀土的paas標準化分佈模式基本相似,呈lree富集型,母巖中無ce異常,而水樣中有ce負異常,表明ce在水巖作用過程中發生明顯的分異;通過研究兩個典型花崗巖風化殼剖面發現,地下水的稀土含量與連續的化學風化,以及水位附近剖面上的稀土含量、粘土礦物含量以及水的ph值等有關。
  8. In this paper, the authors studied a method, in which the anomaly parameter of seismic precursor is abstracted form the observed data of underground water level, and the spatial distribution patterns of the anomaly parameters in north china was scanned from 1984 to 2002 by using the parameters abstracted as inputs, and than, every pattern was superposed with the numerical pattern or quantitative evaluation about the tectonic activity and seismic risk in north china, to realize combining the spatial scanning of precursor anomaly with active tectonic background

    摘要對地下水位地震前兆異常開展了參數提取方法的研究,並以其提取的結果為輸入,對1984 ~ 2002年華北地區地下水位異常參數分佈做了全時空掃描,繼而將全部圖像與華北地區構造活動性量化評估的數字化圖像進行了疊加,實現了地下水位異常動態掃描與區域構造活動性背景的結合。
  9. Because of the alternate between warm and cold water around the circuits, the positive ( negative ) anomaly signal in equatorial western pacific coexists with negative ( positive ) anomaly signal near 10 in eastern pacific before the burst of el nino ( la nina ) event

    冷、暖海水沿msta在北平球熱帶海洋中形成一個冷、暖水相交替的環路,而在赤道上就表現為elni (
  10. 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/負海溫距平信號的分佈和傳播「軌跡」 ,發現如果以暖池次表層為起點,則一般來說,暖水或冷水先是沿赤道的極值深度面向東、向上「傳播」或運動,到達赤道東太平海盆邊界附近后,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、北半球以赤道為一邊, 「傳播」或運動路徑形成扁的閉合環路,溫度距平運動一圈需時2 - 4年。
  11. On the above - mentioned basis, the analysis was made entirely for the evolution of short - term patterns of underground water before m55. 0 shocks which took place since 1985 in north china, so the discriminative criteria of anomaly zones and the characteristics of spatial evolution of short - term precursors of underground water level before strong shocks in north china was established

    在此基礎上,對1985年以來華北地區5級以上地震前的地下水位短期圖像演化情況做了全面分析,提取出了判別異常區的指標以及地震短期異常區的演化特徵,並最終建立了華北地區強震前地下水位短期前兆的判別標志。
  12. Research on fluent in water flowing circulation in anomaly garden water

    軟體在園林不規則池塘人工水力循環中的應用
  13. This paper applied fluent, a commercial cfd software, to simulate the water flowing driven by a pumping system in anomaly garden water in classical gardens of suzhou

    摘要以蘇州古典園林為依託,運用fluent軟體計算實施人工水力循環時不規則園林池塘水體的運動規律。
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