降水量表 的英文怎麼說

中文拼音 [jiàngshuǐliángbiǎo]
降水量表 英文
hyetology
  • : 降動詞1. (投降) surrender; capitulate 2. (降伏) subdue; vanquish; tame
  • : 名詞1 (由兩個氫原子和一個氧原子結合而成的液體) water 2 (河流) river 3 (指江、河、湖、海、洋...
  • : 量動1. (度量) measure 2. (估量) estimate; size up
  • : Ⅰ名詞1 (外面;外表) outside; surface; external 2 (中表親戚) the relationship between the child...
  • 降水量 : precipitation; amount of precipitation降水量計 precipitation gage; 降水量學 hyetology
  1. The space - time distribution of chinese semi - ari d region surface water is n ' t even, the differences in a year are obvious ; the differences of underground water between years are not so obvious as surface water, but it still has a decreasing tendency, especially in shanxi and sha ' anxi provinces. there is a significant linear correlation between the precipitation and water resources in semi - arid region, the dynamic regularity of water resources is basically same as the dynamic regularity of precipitation

    半乾旱地區地資源時空分佈不均勻,年內分配差別大,地下資源年際間變化率不大,但總體有減少的趨勢,尤以陜西和山西突出。半乾旱地區資源線性相關顯著,的變化規律基本上與資源的變化規律吻合。
  2. Gps observation which is about 2km far away from radiosonde site is comparable to radiosonde with a absolute bias of 2. 13mm on precipitable water ( pw ) observation and 1. 28cm on zenith total delay ( ztd )

    與常規探空觀測相比, gps測的可有很好的代性。在相距2km時,兩種測手段測和總延遲的平均絕對偏差分別為2 . 13mm和1 . 28cm 。
  3. Reof analysis was carried out for summer and autumn rainfall field over zhejiang province. the results indicate that the rainfall fields spatially are classified 3 subregions in summer and autumn, but they include some different place in each subregion

    就夏季而言,浙江北部區最少,浙江東南沿海最多,無論從季節還是月看,浙江北部區夏季現出非常明顯的正趨勢。
  4. Results of comparison indicate that although some oversea study of the transilient theory succeeded in a degree, if the transilient theory is to be used in model mm4, substantial improvement of the expression of the vertical mixing potential is necessary, or an empirical filter should be applied to ameliorate the result of forecasting

    比較的結果證明,非局地方法若要應用於實際預報,還需要作較大的改進,主要是針對決定過渡矩陣的非局地混合潛勢。目前的過渡矩陣達方式使物理在空間的分佈不合理地過于均勻,造成了的減少。
  5. To this area precipitation materials for many years, evaporate materials, surface flow materials, hydrometeorological materials, hydrogeological materials carry on exhaustive analysis, have analysed the state of water resource of the sand district, proceed from the heat of the earth ' s surface is balanced, water yield balanced basic theories, combine the amount of regional water resource set up of the materials, such as scene, hydrology, soil of the sand district, etc. and estimate models, have calculated the surface water, groundwater of this area, has carried on models to examine according to the real data, and has predicted to the state of water resource under different climate change scenes of future that analyse. have put forward the scheme that the water resource in this area utilized rationally, use the non - linear motive force model to predict the precipitation, utilize the materials of actual observation, the natural supply amount of calculating out groundwater of sand ground of balanced principle of the amount of water used at the same time, and can exploiting amount predict to groundwater, district of sand,

    本文以寧夏半乾旱地區鹽池縣沙地資源為研究對象,對該地區多年資料、蒸發資料、徑流資料、文氣象資料、文地質資料進行了詳盡的分析,分析了沙區的資源狀況,從地平衡、平衡的基本理論出發,結合沙區的氣象、文、土壤等資料建立了區域資源估算模型,計算了該地區的地、地下,根據實際資料進行了模型檢驗,並對未來不同氣候變化情景下的資源狀況進行了預測分析,提出了該地區資源合理利用的方案,運用非線性動力模型對進行預測,同時利用實際觀測資料,運用平衡原理計算出沙地地下的天然補給,並對沙區地下可開采進行預測。
  6. In the study of quantitative forecast models, composition analysis for three different time series are firstly investigated by statistic test methods. the conclusions are as follows : there is no evident tendency for above three series, and evident periodicity exist only in precipitation series

    在定預測模型研究中,先對三個不同系列進行時間系列的組成分析,結果明:三個系列均無趨勢存在,系列有明顯周期存在,但年最高潮位系列無周期。
  7. ( 5 ) since 3100 ab. r, through comprehensive analysis of these proxy climatic substitute indexes indicates : this was a dry and cold period in which the temperature fell the precipitation decreased ; the vegetation may be forest prairie ; human civilization further developed and the human " s influence on the environment was greater in intensity and wider in range

    今,綜合多氣候代用指標和本期人類活動明顯加強情況的分析明:本期氣候再次出現溫度低、減少的變化,在趨于乾冷氣候條件下,在前期氣候較適宜期發育的森林植被發生了退化,當時的植被可能為森林草原或乾草原。
  8. ( 3 ) 6000 - 5000ab. p, through comprehensive analysis of these proxy climatic substitute indexes indicates : this was a dry and cold period in which the temperature was the lowest and the precipitation was the least ; the vegetation may mainly be forest prairie ; in the early stage of the period appeared yangshao middle culture - the prosperous culture of miaodigou type, and in the late stage there was yangshao late culture - the culture of xiwang village type

    P出現了老官臺文化,中後期即本區老官臺文化之後,出現了仰韶早期文化。門) 6000 5000ab p ,綜合多氣候代用指標的分析結果明:本期氣候為全新世以來溫度最低、最少的最乾冷時期,在這種乾冷氣候條件下,在前期氣候最適宜期發育的森林植被發生了退化,當時的植被可能以森林草原為主。
  9. Normally water resources is affected by human activities and climatic change, but it is affected mainly by climatic change in runoff forming regions located in the high and middle mountainous area in the northwestern china. river runoff in the hexi inland arid region all originates from the qilian mt. area and the change of mountainous runoff resulted from global weather warming up and will bring an important effect to the development of society and economy in the hexi region. so the response on mountainous runoff and its changing trends are analyzed on the basis of the measured data of precipitation, air temperature, and discharges observed from some weather and hydrologic stations in the studied area. the results show that seasonal variation of mountainous runoff in the hexi inland region is mainly affected by the river ' s geographical location and supply source, and the yearly change by precipitation and that in the west of the region by air temperature besides precipitation. there are some obviously regional differences in the influences of climatic change on surface runoff in the hexi inland arid region, that is, rivers runoff in the west of the hexi area have been increasing and rivers in the east part have been decreasing, and the rivers runoff in the central part presented slowly increase trend, such as the heihe river, but it is not quite obvious

    一般情況下,資源的變化主要受氣候變化和人類活動的影響,但在位於我國西北內陸乾旱地區的中高山地帶,徑流的形成主要受前者的影響.甘肅省的河西內陸乾旱區是該省重要的工農業生產和經濟開發區,這里各項社會和經濟活動與出山徑流的變化都有著十分密切的關系.因此,筆者根據有關文氣象臺站的、氣溫和徑流觀測資料,分析了以黑河、昌馬河、西營河等主要河流為代的河西內陸區出山徑流的變化特徵與規律.結果明,河西內陸區出山口徑流的季節變化主要受地理位置和河流補給來源的影響,而年際變幅則受山區年際變化及變幅的影響十分明顯.目前,梨園河以西河流處于上升階段,梨園河以東的河流則處于下的階段;以黑河幹流鶯落峽文站年徑流為代的走廊中部地區的出山口徑流正處於1990年開始的枯段的上升段.但總體而言,河西內陸乾旱區出山口徑流的變化相對比較穩定.預計今後若干年內,河西內陸乾旱區東段河流出山口徑流的變化以偏枯為主,中段、西段河流出山口徑流的變化以平或平偏豐為主
  10. Secondly, precipitation from the radar estimating precipitation model ( rep ) are verified using a rain - gage network of 127 stations in order to show the effects of five methods : zi, optimal interpolation joint of optimal interpolation and kalman filter, kalman filter, and average method. the results show that the method of optimal interpolation and the method of joint have the lowest rms errors and the method of zi has the highest rms errors

    結果明:將地面雨計值作為真值,則聯合校準法和最優插值校準法得出的計算精度最高,卡爾曼濾波校準法和平均校準法的計算精度低於聯合校準法和最優插值校準法, zi關系法的精度最低。
  11. The changing climate, pointing to agriculture, will have a remarkable influence on the crop producing

    結果明,近50年來,越南氣溫升高,顯著變少。
  12. It is found that the mesoscale mountain has significant influence on the location and intensity of the heavy rain area, and the bell - mouthed area and the riverway area of xichang are favorable to the occurrence and development of mesoscale disturbance and heavy rain

    地形梯度分析明,西昌地區所處的河谷地形和場區所處喇叭口小地形,有利於中小尺度氣壓擾動的發生、發展和暴雨的產生,當地形梯度減弱時,相應減弱。
  13. The result shows that annual rainfall in the 15 coming years will increase by about 6 %, annual rainfall fluctuation will increase and rainfall concentration in a year tends to increase, which will make flood and sediment increased

    結果明:未來比多年平均值增加6 %左右,且年際波動性增大,年內分佈更加集中,洪和輸沙有增大的趨勢。
  14. According to our analysis, the farmers in quzhou are in the second phase, which means they already have enough food and put much more inputs for earning high yield and high income. ( 4 ) the ground water table was getting down, caused by precipitation decreasing, no river water coming due to the upstream reservoir, complete drainage in rainy season and irrigation using groundwater

    ( 4 )自然低、上游庫的攔蓄,使平原失去了獲得源的機會;內部防洪排瀝體系的完善,致使入滲補充地下減少;耕地灌溉率的增加,導致農業用不斷加大,這些因素共同作用使區域資源失去平衡,引起地下位的下,從而促使鹽漬土層脫鹽。
  15. The paper explored the pdf of the spatial distribution of the day precipitation. the result shows that the weibull distribution is good on describing the heterogeneous of the spatial distribution of the day precipitation in china. the exponential distribution is n ' t ideally suited to the day precipitation

    利用負指數分佈和weibull分佈擬合全國范圍內的逐日平空間概率分佈模式,發現負指數分佈模式並不能很好的擬合大范圍區域逐日場空間分佈型,而weibull分佈的擬合效果很好,明用weibull分佈描述中國區域逐日空間分佈非均勻性的分佈律是非常適宜的。
  16. The results indicate that in the earlier stage of the development of a hailstorm, an artificial restraint with a common intensity can highly influence the development and precipitation of the hailstorm, increasing its surface precipitation, especially the hailfall amount, but in the later stage of the hailstorm development, the restraint has a small influence on the precipitation

    結果明,在雹雲發展階段的早期,對雲中上升氣流施加人工抑制將對冰雹雲的發展和過程產生明顯的影響,使地面增加,尤其是使顯著增加;而在雲發展階段的後期,這樣的抑制不會導致地面明顯的增加。
  17. In the first part of the paper, on the basis of the weather processes of huai he basin from june to august in 1998, the difference and reliability of the two reanalysis data game and ncep from the fields of basic element, derivative, precipitation, and surface flux were studied by diagnostical and statistical methods. the results showed that the game reanalysis data is more reliable than ncep / ncar reanalysis data at the bottom and mid - high levels of troposphere, and at the precipitation and surface flux fields the case is just the same. in addition, the paper revealed that the game reanalysis data can show the evolution of the southwest vortex but the ncep / ncar reanalysis data cannot do so

    在第一部分,本文以1998年6 - 8月我國江淮地區的天氣過程為背景對game和ncep兩組不同的再分析資料的基本要素場、導數場、場和地面通場用氣候診斷和統計的方法進行了對比分析,結果明,在對流層低層和中高層game再分析資料的基本要素場及地面的場和通場較ncep再分析資料更為準確; game再分析資料能很好地反映出西南渦東移並影響江淮大暴雨的重要天氣特徵,而ncep資料則反映不出這一現象。
  18. ( 2 ) parts of the area show apparent local climatic properties because of the influence of topography, landcover, and so on. precipitation in mountainous and forest area is usually more affluent than in vicinity, this creates a typical mosaic structure of precipitation distribution like the islands. ( 3 ) soil water is the most significant form of water resources, which is the only water for vegetation uptake

    分析結果顯示: ( 1 )黃土高原地區的分佈自東向西、自南向北逐漸減少,東南部可達900多毫米,西北部最低則僅約100毫米,現出顯著的大陸性氣候特徵; ( 2 )由於地形等因素的影響,山地森林等局部地區小氣候特徵明顯,高於周圍地區,結果形成的島狀鑲嵌結構; ( 3 )土壤是黃土高原最重要的資源之一,它是該區植被分利用的重要資源。
  19. Grey correlation analyses show that at the time axis, the factors influencing the diversity of plants strongly are primary productivity, annual precipitation, relative humidity, mean temperature in january, and potential evaporation etc. the spatial distribution pattern of terrestrial vertebrates including mammals, birds, reptilians and amphibians were studied with methods similar to those for plants. 7 d

    通過d以排序明, d以第一軸與多個環境因子均呈顯著相關,其中與經度、年均溫、年均、年均相對濕度、潛在蒸發、初級生產力呈正相關,與緯度、海拔、年均風速、寒冷指數、年均日照率呈負相關。
  20. Research manifests that : ( 1 ) allocation in the year of precipitation is very uneven, and yearly precipitation is different in great scope, negative anomaly of precipitation appear concentratly in the 1990s, the precipitation in the 1990s decreased in different degree ; ( 2 ) close positive correlation exists between runoff and precipitation, runoff is abundant in the year with prolific precipitation, and generally in the year with scarce rain the volume of runoff is not enough ; ( 3 ) there is 20 % margin in their changes amplitude, this mainly resulted from high frequent human activities

    結果明: ( 1 )流域內年內分配極其不均;年際變化劇烈,進入90年代后負距平集中出現, 20世紀90年代較多年均值有較大程度的減少; ( 2 )流域內河川徑流與之間存在密切的正相關關系,多的年份,河川徑流豐富,反之較枯; ( 3 )河川徑流積極響應的變化,然而河川徑流變化幅度卻比變化幅度大20 % ,這個偏差主要是由於頻繁的人類活動的干擾造成的。
分享友人