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decade scaling中文是什么意思

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  • 例句與用法
  • “ but what about forecasting earthquakes on the year - to - decade scale
    “但是,對地震進行一年至十年數(shù)值范圍的預(yù)測如何?
  • With this paradigm in mind , forecasting on the year - to - decade scale would be immensely useful
    考慮到這個范例,對地震進行一年至十年標度的預(yù)測將非常有用。 ”
  • Seeing from the nine - year smoothing curve , there is obvious variation in inter - decade scale for frequency of landing tropical cyclone in summer
    從其9一年平滑曲線來看秋季登陸越南的熱帶氣旋頻數(shù)具有明顯的年代際變化特征。
  • There are obvious 10 - 15 years and 25 - 40 years decades scale periodic change and 1 year , 2 years and 4 years or so annual scale periodic change in heilongjiang ' s precipitation variations
    存在著明顯的10 15a和25 40a的年代際尺度的周期性變化和1a 、 2a和4a左右的年際尺度的周期性變化。
  • There are obvious 10 - 20 years and 40 - 55 years decades scale periodic changes and 1 year , quasi - biennial , 4 years and 6 - 8 years annual scale ones in heilongjiang ' s temperature variations
    存在著明顯的10 20a和40 55a的年代際尺度的周期性變化和1a 、準2a 、 4a和6 8a左右的年際尺度的周期性變化。
  • In autumn , the variation of frequency of the landing tropical cyclone is also great , the biggest is nine , the smallest is only zero . seeing from the nine - year smoothing curve , there is obvious variation in inter - decade scale for frequency of landing tropical cyclone in summer . there is a clear positive relationship between frequency of landing tropical cyclone in summer and summer rainfall of some north city and middle part of vietnam
    夏季登陸越南熱帶氣旋頻數(shù)與同期越南北部個別城市降水有顯著正相關(guān)關(guān)系;夏季登陸越南熱帶氣旋頻數(shù)與越南中部夏季降水有比較顯著的正相關(guān)關(guān)系,夏季登陸越南熱帶氣旋偏多,越南中部夏季降水亦偏多,反之亦然;秋季登陸越南熱帶氣旋頻數(shù)與同期越南北部降水有顯著正相關(guān)關(guān)系,同時與同期越南中部降水也有非常顯著正相關(guān)關(guān)系,即秋季登陸越南熱帶氣旋頻數(shù)偏多,則秋季越南中部和北部降水有偏多趨勢,反之亦然
  • The precipitation character of the middle part of viet nam and its relation to the atmospheric circle . the autumn precipitation of the middle part of viet nam has obvious variations in inter - annual and inter - decade scale with clearly quasi 6a , 10a , 15a period ; in heavy rainfall years , there are a positive anomaly over the north - west pacific and a negative anomaly over japan ; while in deficient rainfall years , the anomaly distribution is on the contrary ; 4 . the precipitation character of the south part of viet nam and its relation to the atmospheric circle . the research finds that the rainfall of the south part of vietnam usually concentrates in the autumn every year and a clear difference of atmosphere condition exists between that of flood and drought years
    越南中部降水變化特征及其與大氣環(huán)流和海溫的關(guān)系越南中部秋季降水具有明顯的年際、年代際變化特征,具有明顯的準6a 、 10a 、 15a左右的周期;越南中部多雨年, 500hpa高度距平場在熱帶西北太平洋為正距平,日本附近上空為負距平;而少雨年則相反;越南中部多雨年,熱帶中東太平洋海溫異常偏高,西太平洋海溫異常偏低;少雨年則相反;越南中部多雨年,登陸越南的臺風頻數(shù)偏多;而少雨年則相反。
  • ( 2 ) it shows strong positive correlation at 32 years periodic scale between the precipitation and sst in nino3 , while the periodic characteristics are more distinct at 4 years though it is mostly positively correlative then ; in a shorter time scale period , the correlation between the precipitation in heilongjiang and soi is the regular transforming of positive and negative correlations , while at a longer annual or decades scale , the correlations , though mostly negative , are periodically positive
    黑龍江省降水與nino3區(qū)海溫的相關(guān),在32a周期尺度上,表現(xiàn)為較強的正相關(guān),而4a尺度上雖以正相關(guān)為主,但相關(guān)的階段性比較明顯;在較小的年際尺度周期上,黑龍江省降水與soi之間表現(xiàn)為正、負相關(guān)有規(guī)律的轉(zhuǎn)換;而在較大的年際尺度和年代際尺度上,兩者的關(guān)系則以負相關(guān)為主,但也存在階段性的正相關(guān)。
  • Based on the longtime hydrological observation records during the years from 1956 to 1995 , properties of precipitation of weihe basin in shaanxi province of different time scale ( including month , year and decade scale ) is analyzed by the method of contrasting properties , correspondingly change characteristics of runoff are also discussed by means of statistics , hence response relationship between runoff and precipitation is revealed , and the main reasons affecting amount of runoff are pointed out
    摘要根據(jù)1956 - 1995年的實測水文資料(降水和河川徑流量資料) ,采用特征值對比方法,對陜西省境內(nèi)渭河流域不同時間尺度內(nèi)降水特征進行分析,并對流域內(nèi)多年徑流變化也做了相應(yīng)的統(tǒng)計分析,從而揭示河川徑流對降水變化的響應(yīng)關(guān)系,并確定出河川徑流變化的主要原因。
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