月際變化 的英文怎麼說

中文拼音 [yuèbiànhuà]
月際變化 英文
inter-monthly variation
  • : Ⅰ名詞1 (月球; 月亮) the moon 2 (計時的單位) month 3 (姓氏) a surname Ⅱ形容詞1 (每月的) mo...
  • : Ⅰ名詞1 (靠邊的或分界的地方) border; boundary; edge 2 (里邊; 中間) inside 3 (彼此之間) betwe...
  1. The precipitation of northern hemisphere has a significant negative trend, lapse rate of precipitation during djf is - 0. 028mm / a. for the southern hemisphere, has n ' t pass the statistical significance. the flood / drought years are pick out in 1948 - 2001 for djf over global, northern and southern hemisphere, six large - scale areas, the results point out has significant decadal change in the flood / drought years of global, nh and sh in djf, during 1940s - 1970s global flood in djf occurred frequently and from 1970s - 1990s global drought in djf occurred frequently

    北半球有明顯的降水減少,約為- 0 . 028mm a ,南半球12 - 2降水表現為極微弱的下降趨勢,且在統計上是不顯著的。劃分出了全球、南北半球、全球6個大尺度區域12 - 2旱澇年,指出全球及北、南半球12 - 2的旱澇有明顯的年代。 70年代中期以前是全球洪澇多發期, 80年代到90年代為全球乾旱多發期。
  2. The target of the geography research study, primarily the target of experience, emphasizes the study process of students, the student participation directly and experience personally. therefore, combining with the contents and practice that can be proceeded in high school geography teaching, the general mode, cooperative mode, discoverable mode, applying mode and opening mede have been constructed, and illustrated by the active example of " the changes and causes of the phase "

    地理研究性學習的目標主要是體驗性目標,它強調學生的學習過程,學生的直接參與和親身體驗,因此結合中學地理可進行的研究性學習內容的實,構建了中學地理研究性學習的一般模式、協作模式、發現模式、應用模式和開放模式,並通過「及成因」的鮮活示例加以說明。
  3. The activity of cold air and interannual variation of low level jet are important cause of interannual variation of the rainfall in april. interannual variation of subtropic high is the main cause of interannual variation of the rainfall in may over north china. there is significant negative correlation between interdecadal variation of the rainfall in april and that of sst in the areas of equatorial indian ocean and tropic middle - east pacifi

    華北4降水與熱帶中東太平洋、赤道印度洋海溫年代呈明顯的負相關:華北5降水與熱帶中東太平洋、赤道印度洋海溫年代存在明顯的正相關:熱帶海溫的年代異常引起的副熱帶高壓的年代異常可能是影響華北4 、 5降水異常的重要原因。
  4. The analyzing results show that, in four types of household activities in the scope of village, the disorder effect generated by the secondary industry is strongest, which by commerce and service activities is stronger, and which by agricultural activity is strong, and which generated by household reproduction and live activ ity is relatively weak. from 1990 to 2002, the disorder extent of household activities in three villages becomes increasing in turn. in terms of their seasonal change, the household activities of wugou and hutuo village mostly fasten on two traditional busy seasons in agriculture, however xiaonan village is in the other way, that is to say, the intensity of household activities is weak in the traditional busy seasons, which is strong around chinese new year

    分析結果顯示,在村域農戶活動類型中,以工業生產活動對環境所產生的無序影響最大,其次為農戶商業等活動、農業生產活動、農戶自生產與生活活動;吳溝村、滹沱村、孝南村1990年、 2002年農戶活動無序度均表現出依次增大的特點;在農戶季節活動中,吳溝村、滹沱村農戶活動主要集中於兩個傳統的農忙季節,而孝南村則相反,在傳統的農忙季節里,農戶活動強度反而較小,而在春節前後,農戶活動則較為頻繁;在農戶活動份差異中,滹沱村最大,吳溝村其次,孝南村最小;在農戶活動年中,孝南村最大,其次為吳溝村,滹沱村最小。
  5. 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降水在年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降水偏少(多) 。
  6. 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降水年關系有明顯的年代特徵:其與夏季總降水的年關系由1974年前較好的負相關在1974年後差,與7降水的年關系由1974年前較好的負相關在1974年後弱,與8降水的年關系由1974年前較好的負相關在1974年後差;另一方面,其與中國160站夏季及7 、 8降水的年關系在1974年前後發生的主要特徵是:與夏季總降水、 7、 8降水的年關系由1974年前的相關系數分佈呈「東西型」為1974年後相關系數分佈呈「 - + - 」的「南北型」 。
  7. 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與華北夏季降水年關系及其年代
  8. Figure 5 diurnal variation of uv index on 2 august 1999

    圖五紫外線指數在1999年82日的日
  9. Diurnal variation of uv index on 14 august 2001 a sunny day with some 12 hours of sunshine

    圖三紫外線指數在2001年84日的日
  10. The simulated results of net primary production ( npp ) are similar to other ' s study. the annual, seasonal and daily change of npp can reflect the physiological characteristic of vegetation growing very well and has close relationship with climatological factors

    年npp的模擬結果與國內的一些其它類似研究結果接近, npp的模擬結果能較好地反映出植被生長的生理特點npp的、日及年對氣候因子有不同的響應。
  11. 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(主汛期)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降水異常和旱澇的年代;同時利用ncep ncar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。
  12. Workshop on the network system for monitoring and predicting enso event and sea temperature structure of the warm pool in west pacific ocean. 5 - 7 february, 2001, macao

    2002熱帶海洋環境與氣候研討會,三亞, 226日31日。王東曉(南海環流模式比較初步結果、太平洋年代的強迫因子、南海環流的多渦結構) 。
  13. Its interannual variation ' s main period is about 4 ~ 5a and the 7 ~ 8a ' s period exist too ; the interdecadal variation ' s main period of the australian high is about 15a. the interannual variation of australian high ( aah ) has correct correlation with antarctic oscillation and enso, and the enso ' s 4a period has the most important influence on the aah. ( 2 ) when the ah becomes stronger, the members of the whole aamcs are stronger following it. that is to say, in the years that the ah is stronger ( compared to the weak years of ah ) and on the horizontal circulation, the members of aamcs, including the ah, the cross - equator flow ( cef ) between 100 and 160 e, the south china sea south - west monsoom ( ssm ), the south sea monsoon rough, the tropical easily flow, subtropical high ( sh ), the mei - yu front, the mid - latitude effect, become stronger, and their positions are more southward ; in the meridional - right circulation, there are five circulations including classic monsoon meridional - cirle circulation and hadley circulation that become stronger in the strong years of ah than in the weak years of ah

    本文採用ncep ncar再分析平均的全球海平面氣壓場、高度場、海表溫度場、高雲量和cmap全球降水資料,以及中國160站逐降水資料,分析了1948 2002年期間澳大利亞高壓(以下簡稱澳高)的年和年代以及澳高年對亞澳季風環流系統的影響,結果顯示: ( 1 )澳高存在明顯的年和年代,澳高年以4 5年的周期為主,同時兼有7 8年左右的周期,而澳高的年代則以15年左右的周期為主:澳高年同時與南極濤動和enso有正相關,並且enso的4年左右的周期對澳高年影響最大。
  14. There is the same characteristics of interannual and interdecadal variation between the first characteristic vecter and corresponding percent of the rainfall anomaly ; the second characteristic vecter which is the most obvious in may has interannual variable characteristics in each month

    華北春季及各降水量第一特徵向量和相應時期的降水距平百分率具有相同的年及年代特徵;春季及各的第二特徵向量均存在年特徵, 5最明顯。
  15. In this article, based on the rainfall data over north china in spring and respective month, atmospheric circulation data ( ncep ) and the sea surface temperature data ( sst ), the methods of eof analysis, yamamoto analysis, mesa analysis, correlation analysis and composition analysis are used to study totau spatial and temporal distribution characteristics of the rainfall in spring and respective month over north china, investigate correlation with interannual andinterdecadal variation of sea surface temperature and atmospheric circulation, and analyse mechanism of influence

    本文用華北春季及春季各降水資料, ncep資料以及coads海溫資料,採用eof分解、 yamamoto分析、最大熵譜分析、相關分析、合成分析等方法研究了華北春季、各降水的總體分佈特徵及時空分佈特徵,並從總體上探討了其與海溫、大氣環流年、年代的關系及其影響機制。
  16. The monthly change about the percentage of positive cg lightning is opposite to that of total lightning

    正地閃比例的月際變化與閃電次數正好相反。
  17. The monthly changes, daily variety regulations and survival environment differences of llj in northeast china and south china are also large

    東北、華南兩地的低空急流,其月際變化和日規律以及生存環境差異也很大。
  18. Second, the bar of the frequency - distribution and the curve of lorenz and the g coefficient are talked about the spatial distribution of day to day precipitation. the results show that the heterogeneous of day precipitation is strong on every day in a year. the spatial distribution model is left skew all in four seasons and it is different from the monthly precipitation

    其次利用全國700個測站逐日降水資料的空間分佈頻數直方圖及洛倫茲曲線和基尼系數闡述了我國逐日( 24小時)降水非均勻性的事實,直方圖顯示全國范圍內逐日降水的水平空間分佈型在四季都是一種明顯左偏態型,與降水量的水平空間分佈型略有不同;基尼系數值的月際變化也與降水量的相反。
  19. 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異常為主,熱帶太平洋區域年和年代異常相當;表(淺)層海洋與大氣的年代特徵對同一季節、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;北太平洋區域的7與此不同,這與該季節近表層海溫層結穩定有關;年尺度的海、氣異常與enso有關,且以熱帶太平洋區域1最典型, 7次之,北太平洋區域1再次之, 7無明顯關系。
  20. The trend of variation in the south region of jianghuai valleys is obvious in comparison with that in the north region, but tow regions have remarkable characteristics of interannual and interdecadal change in recent 50 years

    ( 2 )近50年來江淮地區5 7降水都呈上升趨勢,均具有顯著的年代特徵,但南區趨勢比北區明顯。
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