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orthogonal function中文是什么意思

  • 正交函數(shù)

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  • 例句與用法
  • Complete orthogonal function system v and points cloud fitting
    系統(tǒng)與點(diǎn)云數(shù)據(jù)擬合
  • On expression of ocean sound profile by layered empirical orthogonal function
    聲速剖面的分層經(jīng)驗(yàn)正交函數(shù)表示
  • The proofs of the two orthogonal function systems formed by first order bessel functions
    由一階貝塞爾函數(shù)組成的兩個(gè)正交系的證明
  • Empirical orthogonal function ( eof ) has been applied in typhoon track forecasting
    自然正交分解( eof )在臺(tái)風(fēng)路徑預(yù)報(bào)中已得到應(yīng)用。
  • The empirical orthogonal function ( eof ) is employed to analyze dekad rainfall in china in recent 44 years
    采用eof方法,將我國(guó)近44年的旬降水量進(jìn)行分解。
  • Ecmwf ( 1977 ) . proceedings of the ecmwf workshop on the use of empirical orthogonal functions in meteorology , 2 ? 4 november , 1977 , european center for medium range forecasts , reading , uk . ecmwf ( 1977 )
    Ecmwf經(jīng)驗(yàn)正交函數(shù)在氣象上應(yīng)用的專題會(huì)議論文集,于1977年11月2 ? 4日,在歐洲中期天氣預(yù)報(bào)中心舉行(聯(lián)合王國(guó),里丁市) 。
  • Chinese minimum and maximum temperature fields are divided respectively by the rotted empirical orthogonal function eleven , twelve sub regions can be taken for minimum and maximum temperatures respectively
    利用旋轉(zhuǎn)主分量分析,分別對(duì)我國(guó)極端高溫和極端低溫場(chǎng)進(jìn)行了客觀區(qū)劃。極端低溫和極端高溫場(chǎng)分別可以分為11 、 12個(gè)變化區(qū)。
  • 2 . doppler frequency shifting and curve fitting differential methods for measuring velocity are analyzed and compared . the least - squares curve fitting methods based on power functions and orthogonal functions are analyzed and compared
    2 .對(duì)測(cè)量速度的兩種方法,多普勒頻移法和曲線擬合微分法作了分析和比較;對(duì)以冪函數(shù)族和以正交函數(shù)族為基底的最小二乘曲線擬合法作了對(duì)比分析。
  • With the rotational complex empirical orthogonal function rceof , we analyzed the spatio - temporal evolvement of the latest fifty years ssta of pacific ocean . came to a result that there are two strong signal center : one at middle and east pacific ocean near equator , the other at 40n . it will take several months to half a year for the signal to reach west pacific ocean from east coast of pacific ocean near equator correspond to enso
    運(yùn)用轉(zhuǎn)動(dòng)復(fù)自然正交展開rceof分析近50年太平洋海溫場(chǎng)的時(shí)空結(jié)構(gòu),得出在赤道中東太平洋和40n附近有兩個(gè)海溫異常強(qiáng)信號(hào)中心赤道東海岸太平洋海溫異常信號(hào)對(duì)應(yīng)enso信號(hào)在幾個(gè)月到半年左右傳播到赤道西太平洋海溫主要周期大部分落在310d的范圍內(nèi),還存在年和準(zhǔn)兩年變化。
  • Based on the empirical orthogonal function ( eof ) , the characteristics of large scale variations of precipitation anomaly during rainy season ( from jun to aug ) in south - west china for the period 1961 1995 is analyzed , and the teleconnection distribution charac - teristics between sea surface temperature ( sst ) over india ocean and precipitation during rainy season in south - west china were studied by using the method of cca
    用自然正交函數(shù)展開方法對(duì)1961 1995年西南汛期( 6 8月)降水大尺度變化特征進(jìn)行分析,并在此基礎(chǔ)上用典型相關(guān)分析方法研究了1 8月印度洋海溫距平場(chǎng)與西南汛期降水場(chǎng)的遙相關(guān)分布特征。
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