暖水表 的英文怎麼說

中文拼音 [nuǎnshuǐbiǎo]
暖水表 英文
warm water meter
  • : Ⅰ形容詞(暖和) warm; genial Ⅱ動詞(使東西變熱或使身體變溫暖) warm up
  • : 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...
  • : Ⅰ名詞1 (外面;外表) outside; surface; external 2 (中表親戚) the relationship between the child...
  • 水表 : water meter; watermeter; water-flowmeter水表玻璃管 gauge glass; 水表井 water meter chamber
  1. They are said to be “ undersaturated. ” shallow, warm surface waters are described as “ supersaturated ” with respect to both calcite and aragonite, meaning that these minerals have no tendency to dissolve

    海洋淺層的溫,對方解石和霰石則為過飽和,代這兩種礦物不傾向溶解。
  2. R. yushensis is an aquatic plant in the lake of zhangcun at that time and indicates a brackish, clear, tranquil and shallow lake in this region in late pliocene. the smooth endocarp surface further suggests a warm temperate or temperate palaeoclimate

    榆社川蔓藻果實和種子的大量出現說明該植物可能在該域形成了單一的優勢類群,其光滑的內果皮面指示當時當地為溫帶或溫帶氣候。
  3. There is no perspicuity verge between the west and the east of qinling mountains, so we have to draw a line to divide it into two parts. by analyzing the chang of observation spot " s precipitation in summer and in autumn on the same latitude, we can make a conclusion that 108 ewill be the line possibly. the paper was going on under the background of global chang by compairing the variation characteristics of norm annual air temperature and norm annual precipitation, and by compairing air temperature and precipitation over the season,

    秦嶺東部地區氣候變化總體趨勢為降減少、氣溫遞增,其中近50年的時間里,氣溫共遞增0 . 185 ,同時降減少75 . 35mm ,現為干化特點,其化的特點現在冬半年的冬尤其是冬季增溫強烈,干化則主要集中在夏季降的銳減;而秦嶺西部地區則降減少的同111氣溫下降,近50年來,氣溫共下降0
  4. Based on the two ctd data sets from the cruise of the summertime in 2000 and wintertime in 2001 in bohai sea and the collected historic observed thermohaline data, we analyse systemically the distributional characteristics of temperature, salinity and density in wintertime and summertime in the bohai sea and the results reveal that the current hydrologic characteristics of the bohai sea have some obvious variances relative to the previous research results. in summer there are three low - temperature centers in the middle - layer and underlayer of the middle parts of the bohai strait, liaodong bay - mouth and bohai bay - mouth, but there is a uniform high - temperature center in the middle part of the bohai sea. in winter the isotherms extend westward and northward to the bohai sea from the warm core of the bohai strait and a cold - water tongue off the qinhuangdao spreads southeastward out, so the saddle - like isotherm pattern is formed in the middle part of the bohai sea

    利用2000年夏季和2001年冬季渤海兩次ctd資料和以前收集的渤海溫鹽調查資料,分析了渤海冬、夏季溫鹽密度的分佈特徵,結果明,渤海現有的文特徵與以往研究結果相比發生了明顯的變異:夏季在渤海海峽、遼東灣口和渤海灣口中部中、下層存在三個低溫中心,在渤海中部則出現一個上下均勻一致的高溫中心;冬季等溫線以渤海海峽中心向西和向北兩個方向伸入渤海,而從秦皇島外海有一冷舌向東南方向伸展,在渤海中部海域形成「馬鞍狀」等溫線結構。
  5. Using the matlab tools, a computer program is compiled to solve this mathematic model, by which simulations to the thermal environment of the heated space under different heating style are carried out. the simulations results and their analysis show that for different space with the same thermal comfort index, the energy consumption of low - temperature water floor radiant heating system is less than that of convection heating system

    基於上述採空間的熱網模型,運用matlab數學軟體編程,對低溫熱地板輻射採方式和對流採方式下房間的熱環境進行動態分析,並對這兩種採方式下採系統的能耗進行計算機模擬計算,結果明低溫熱地板輻射採系統相對于對流採系統有顯著的節能性。
  6. Based on the epwp and wpwp in conjunction with abnormal north and west wind, a new possible iii mechanism is provided for the evolution of the 1997 / 1998 el nino. to be specific, the warm kelvin wave propagating to east excited by the abnormal west wind can suppress the cold upwelling flow in the eastern pacific, which, in turn, is favorable to the eastern pacific sst increase ; abnormal west wind can make the warm water of the wpwp east edge extend to east, which is conductive directly to eastern pacific sst increase ; the abnormal west wind propagating to east can make the sea surface warm water near two equatorial laterals converge to the equator by ekman drifting, which, in rum, strengthens the downwelling flow near the equator, leading to eastern pacific sst increase

    將東、西太平洋池及異常北風、西風一併結合起來考慮,提出1997 1998elnino事件發生、發展的一種新的可能機制:異常西風激發東傳的kelvin波對東太平洋的冷上翻流有抑制作用,從而有利於東太平洋海溫度增加;異常西風驅動西太平洋池東端向東伸展直接有利於東太平洋海溫度增加;東傳的異常西風可以通過埃克曼漂流效應將赤道兩側的海向赤道輻合從而加強了赤道附近的下沉流,也有利於東太平洋赤道附近海溫度增加。
  7. At the same time, the effects of dragging force from fall of hydrometeors and latent - heat release from phase transfer are tested. from the analyses we conclude that the distributing of the cloud particles relates with temperature closely. huanan heavy rainfall and mei - yu front heavy rainfall have mixed - phase process with vapor phase, liquid phase and ice phase

    詳細分析了形成降的雲物理過程,探討了源匯項對凝物的貢獻,並通過敏感性試驗,考察了雲物理過程對降熱力動力過程的反饋作用,研究結果明:華南區暴雨和長江梅雨鋒暴雨的雲物理過程具有汽、、冰三相混合雲特徵。
  8. Moreover, the aid of gray interrelation analysis and the plural regression model are applied to discuss the reason of runoff decrease and abrupt changes. for over 40 years, under the background of climatic warming, river runoff of shaanxi - gansu - ningxia region has showed a generally reduction trend

    40多年來,在氣候干化的背景下,陜甘寧地區地資源變化總趨勢為減少,現為自1950年代末以來河川年徑流量的顯著減少傾向,而且貧化也日趨嚴重。
  9. Our conlusion is : during the coruse of the nov in el - nino year ( start from the westerly anomalous ) to apr of next year, it is just the intensity of east asian monsoon that influents the sst variety in kuroshio region. the heat flux is the bridge links the two facts. and the gene which affects winter monsoon is the pea circumfluence

    分析還顯示影響黑潮海溫異常的主要機制有:由赤道中太平洋西風異常而產生的pea遙相關、夏季太陽輻射的加強、低緯向高緯輸送的增加及黑潮自身海的輻合。
  10. Data used in this work are north pacific ssta, 160 stations precipitation of china, and ncep reanalysis data. main results are as follow : ( 1 ) it is found that a apparent transition of north pacific ssta in later 1970 ' s : eastern and middle - equatorial pacific ssta turns from cold to warm with area extending, and mid - latitude pacific ( west wind drift zone ) turns from warm to cold. during this transition of ssta, different characters also appear in el nino and la nina : before 1976, la nina happens more frequently, and its duration is longer, el nino zone develops from negative ssta in the early stage ; after 1976, el nino happens a little bit frequent and longer with more intensity than before, el nino zone develops from positive ssta in the early stage ; the course of ssta variation has an enso cycle of 2 - 6 years, annual oscillation of 8 - 9 years, and decadal variation of about 22 years

    本文採用1950 - 1999年北太平洋海溫度( sst ) 、中國160站夏季降和ncep再分析的歐亞500hpa高度場等資料,利用eof 、 svd 、小波分析、合成分析和相關分析等方法,在分析北太平洋海溫時空分佈特徵的基礎上,著重探討了海溫異常及其年代際變化對我國東部降的影響,並對降、高度場和海溫三者之間的關系進行了分析,以試圖尋找三者異常之間可能的聯系,主要結論如下: ( 1 ) 1976年前後,北太平洋海溫經歷了一次明顯的轉變,赤道中、東太平洋厄爾尼諾海區由冷轉范圍增大,中緯度西風漂流區海溫由轉冷;在這樣的年代際背景下,厄爾尼諾、拉尼娜事件在不同的時期也有不同的特徵:在76年前,拉尼娜事件發生頻率高,持續時間長,事件起始於負海溫距平;而76年後,則是厄爾尼諾事件發生頻率略高,持續時間長,強度增大,事件起始於正海溫距平。
  11. The above analysis showed that this heavy rainfall event took on obvious meso - scale characters and was the combination of the three flows, so we can deduce : ( 1 ) surface southeasterly wind and topography may play the main role in this event ; ( 2 ) the easterly cold air rushing into the southern shaanxi province in the lower troposphere was strongly relative to the form of surface cold - front type of occlusion ; ( 3 ) there were two reasons for the secondary circulation ' s strengthen in the evening, one was the effect of a mountain - valley wind and the other may be latent heat leading to ascending motion ; ( 4 ) the shape of potential instability stratification corresponded well with the development of the warm - moisture advection ; and ( 5 ) the vapor providing essential thermodynamics was transported by a southwesterly low - level jet from the bay of bengal and the south china sea. furthermore, with the effect of terrain, the southern shaanxi province became the center of this extremely heavy rain process

    中尺度結構分析明,本次暴雨具有明顯的中尺度特徵,是由三支氣流共同作用的結果,分析發現( 1 )地面東南風和地形在這次大暴雨過程起主要作用; ( 2 )東路冷空氣主要是通過中低層侵入陜南地區的,並與地面冷式錮囚鋒的形成密不可分; ( 3 )夜博士論文:中尺度地形對陜南暴雨的影響研究間垂直次級環流發展加強可能有兩個原因,一個是由於地形山谷風的作用,另一個是降的潛熱釋放激發了上升運動: ( 4 )位勢不穩定層結的形成與低層濕平流的發展有很好的對應關系; ( 5 )本次暴雨的汽主要靠偏南風急流將孟加拉灣和中國南海的汽輸送至西北地區東部,為暴雨的發生提供了必要熱力條件。
  12. Everything under his paint brush, the graceful lotus leaves, mountain birds roosting in flowers, orchid blossoming on rock cliff, ducks in warm river in spring, are well distilled and recreated by the painter, shining with glowing look of life

    那亭亭出的荷葉,花間棲息的山禽,山崖吐芳的幽蘭,春江的群鴨,無不是經過了畫家的精心提煉和再造,煥發出灼灼的生命神采,而這種神采,又恰恰是作者情思的白、性靈的宣洩。
  13. Gunagzhou panyu rongxiang faucet co., ltd. was opened in 1998, the new factory locates in shiji town panyu district guangzhou city, the area is 1, 5000 square meters. it has more than 800 staff and 18 professional workshops now. they are founding workshop, forging workshop, punching workshop, cnc workshop, claming workshop, soldering workshop, polishing workshop, assembling workshop, mould workshop, polishing workshop, electroplated workshop, test workshop etc. we have the ability to work in pineline from casting, forging machining step to polishing and plating step

    廣州市番禺榮祥器材有限公司創建於一九九八年,廠區位於廣州市番禺區石基鎮,佔地15000平方米,主要以生產陶瓷閥芯和器材配件為主,現有員工八百多名,擁有鑄造車間(分為引鑄和砂鑄) 、鍛壓車間、沖壓車間、數控車間、鉗工車間、焊接車間、拋光車間、彎管車間、模具車間、新產品試制車間、電鍍車間、試驗車間、檢測車間、裝配車間等十八個專業車間,具備了從鑄造、鍛沖壓、機加工到外層拋光電鍍一條龍的生產能力。
  14. While modest warming has taken place, there is no conclusive evidence human beings are responsible, no conclusive evidence earth ' s temperature is rising dangerously or will reach intolerable levels and no conclusive evidence that warming will do more harm than good

    氣候是出現了適度的化,但並不沒有結論性的證據明和人類有關,也沒有結論性證據說明地球的(大氣)溫度升高得非常危險,或者說到了一種難于忍受的平,更沒有結論性證據說明氣候化弊多於利(危害多於受益) 。
  15. Genetic analysis shows that it may be caused by the difference of the response of each area to winter monsoon ' s abnormal, the kuroshio and our offshore is influenced mostly by heat flux between the sea and atmosphere, but in the other areas, the abnormal current incited by abnormal wind has decisive effect on the change of the sea temperature, at the same time, air pressure also has some impact on the sea temperature

    其區域性形成的原因主要可能是因為各海區對冬季風異常的響應方式不同,強冬季風使得黑潮與我國近海海洋過多散熱,海溫降低;在西北太平洋池北部,強冬季風引起西風異常,從而引發異常氣旋性環流,海輻合下沉加熱其層以下海,同時異常環流使得更多東側異常向西加熱其;在黑潮與親潮交匯處的升溫也主要是由於強冬季風導致的流場異常,海輻合下沉升溫。
  16. 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由北向南輸送至赤道附近直接導致nino3區海溫度增加。
  17. There is a minimum of vertical mixing because the warm water can not displace the dense, colder deep water

    在海洋中,因為不能代替深部較高密度的冷體,所以海的垂直混合作用很小。
  18. 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、沿msta在北平球熱帶海洋中形成一個冷、相交替的環路,而在赤道上就現為elni (
  19. 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」 ,發現如果以池次層為起點,則一般來說,或冷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,並在池的經度范圍內再作經向運動傳到地,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。
  20. Whole system include available for user intellectual heating form and collector of design realized to design make up already, a machine gets user ' s heat of using within some time through measuring the instantaneous flow and temperature of the hot water in real time ; the measurement can reach the pc of the administrative center of the property far through the collector, finish data processing, expenses close, report form person who type multiple tasks in unison by administrative center

    整個系統包括已經設計實現的供用戶使用的智能和設計中的通訊模塊以及採集器組成,戶機通過按時測量熱的流量及溫度,得到用戶在一段時間內的用熱量;測量數據通過採集器可以遠傳至物業管理中心的pc機,由管理中心統一完成數據處理、費用結算、報列印等多項任務。
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