暖氣分區 的英文怎麼說

中文拼音 [nuǎnfēn]
暖氣分區 英文
zone heating
  • : 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
  • : Ⅰ名詞1 (氣體) gas 2 (空氣) air 3 (氣息) breath 4 (自然界冷熱陰晴等現象) weather 5 (氣味...
  • : 分Ⅰ名詞1. (成分) component 2. (職責和權利的限度) what is within one's duty or rights Ⅱ同 「份」Ⅲ動詞[書面語] (料想) judge
  • : 區名詞(姓氏) a surname
  • 暖氣 : central heating; heating installation暖氣爐 furnace; 暖氣片 (heading) radiator; tinned radiator...
  1. Firstly, evidence from depositional pattern suggests that the hsl has experienced an expansion - contraction circle since the late glacial epoch. the expansion and movement of the hsl or desert in early stage were clearly marked by the presence of paleo - aeoline sands. the occurrence of paleosoal characterized the stabilization and contraction of the hsl and also indicated the activity of pedogenesis on the paleo - aeilian sands

    通過系列候代用指標的析,首次發現該地粒度、磁化率指標值在兩個大的峰值之間有多個小的峰谷出現,表明了在大的候變化階段次一級的濕?乾冷候波動,值的進一步做年齡的小尺度高解析度研究。
  2. Zhengzhou has a temperate and monsoonal climate with four clearly distinct seasons

    鄭州地溫帶大陸性候,四季
  3. Beijing has a typical temperate and monsoonal climate with four clearly distinct seasons

    北京的候為典型的溫帶季風候,一年四季顯著。
  4. We can use the mm5 model in definite time, definite area weather forecasting. we conclude that : : the moving route of this necw in its developing progress was direct - south along latitude, the cold air is rough, and just this made the rough vertical velocity ; the necw southern moving and conflicting with the west pacification sub - tropical high makes rough jet steam. the plenty south - west warm and wet air made by the jet stream gave the rainstorm demanded vapor ;. the rough vertical velocity by jet stream is a main reason in this rainstorm ; the mm5 model uses four - direction analysis data as its input, this avoids some errors occurred in observe and transfer, thus made the result more useful

    綜合析認為: ( 1 ) 、這次冷渦在其發生發展過程中,其移動路徑是沿經圈直線南壓,攜帶的冷空勢力較強,形成槽后較強的垂直運動; ( 2 ) 、西太平洋副熱帶高壓偏北位置與東北冷渦南壓形成的急流軸,把源源不斷的西南流輸送到遼西地,也就是急流軸的左前方位置,為這次暴雨的產生提供了充足的水汽來源; ( 3 ) 、低空急流不但為暴雨輸送水汽,其造成的較強的垂直環流也是產生強降水的一個主要原因; ( 4 ) 、 mm5模式以四維同化資料作為初始場,最大限度地避免了觀測誤差可能造成的積不穩定,提高了模擬結果的參考價值。
  5. Setenaly according to the analyses from selected profiles, we know that, it is cold and dry in this region during the early holocene when east asian winter monsoon ' s influence is obvious, so, it is a transition period from sand deposit to sandy soil deposit, when the layers become thinner gradually from north to south. during middle holocene, it is warm and humid, influenced evidently by east asian summer monsoon, so, it is an obivious pedogenesis, when there are generally well - developped holecene palaeosol ( so ) from north to south, and the pedogenesis in the south is better than that in the north, the soil is also thicker than that of the north. from late holocene to now, the climate changes to be dry and cold, but its changing scope is smaller than that of last glacial period

    2 、就所選剖面析來看,本在全新世早期候回返,相對較寒冷乾燥,東亞冬季風影響較明顯,此時為沙層堆積向砂質土壤過渡,自北至南堆積的沙粒漸細;全新世中期候溫濕潤,東亞夏季風影響顯著,此時為明顯的成壤期,表現在自北至南普遍可見發育較好的黑壚土層,且南部的成壤作用比北部好,土壤的厚度也要大;全新世晚期至今,候向乾冷方向轉化,但變化幅度遠小於末次冰期。
  6. The vegetation type was classified in the east transect by unsupervised classification using the data ( ikmx 1km ) from noaa meteorology satellite from 1995 - 1996, and the article analyzed the change of ndvi of all kinds of vegetation types, in the same time analyzed the forest dynamics in typical ecotone ( warm temperate zone to semitropical in qinling woods ) using the higher spatial resolution tm data

    本論文利用1995 - 1996年noaa象衛星的ndvi ( 1km 1km )數據,採用無監督類方法對中國東部樣帶南方部進行植被類型的劃析各植被類型的ndvi變化情況;並利用較高精度的tm數據析典型交錯域(溫帶到亞熱帶的秦嶺林)的森林動態變化情況。
  7. The ncep / ncar globally tropospheric 1 1 reanalysis data have been employed to select six landfall typhoon cases in order to diagnose variations of typhoon warm sectors in atmospheric boundary layer during their whole life periods

    摘要採用ncep / ncar全球對流層1 1再析格點資料,選取6個登陸臺風個例,析了不同發展階段臺風大邊界層變化的特徵及其與強度變化的關系。
  8. The magnitude of these variables increased approximately ten times. it helped the rapid releasing of instability energy. the interaction of high - level and low - level mesoscale system leads to the rainstorm. the vertical cross section analysis of potential temperature tells us that rainstorm take place in the warm - moist and instability area. usually locate in the very stiff moist isentropes and it can lead to the development of vortex

    通過對相當位溫的垂直剖面析,可知兩場暴雨的中低層都為濕不穩定濕不穩定上部冷空明顯擴散,暴雨產生在濕對流不穩定內,通常產生在_ e陡峭和密集中, _ e陡峭和密集有利於渦旋發展。
  9. The main design points of passive design techniques have been dissertates by the numbers, from three aspects of building groups, single buildup and building parts, which include building group layout, orientation space between, wind protection solar heating, thermal mass and nocturnal cooling and natural ventilation etc. the dissertation also explains the whole climate design process is three stage of climate analysis, conceptual design stage and schematic design evaluation and at last, taking a high - rise residential building as an example case study, evaluates its climate adaptation strengths and limits, and then proposes the correctional advises for responsive to climate

    本文著重從建築群體關系、單體設計、局部構造三個層面上論述了各設計技術策略的設計要點,包括布局、朝向、間距、防風、太陽g睬、建築蓄熱降溫、自然通風等。最後本文以西安為例,給出了建築候設計程序為析?方案設計?方案評價三個主要過程,並對一高層住宅建築的候適應性進行了析和評價,提出了方案的修改建議。
  10. The quasi - geostrophic process was diagnosed for a case of severe cold air breakout under the blocking situation during 16 - 18 march of 1998. the attention was focused on the relationship between the surface anticyclone and 500hpa blocking high. the results indicate that the cold outbreak is associated with the adjustment of blocking situation in the ural area, i. e. the collapsing and rebuilding of the ural mountain blocking high. the temperature advections in the lower troposphere shown that the polar cold air invading from the northwest caused the ural blocking high collapsed, and a new ridge developed rapidly was due to the warm advection on the southwestern side which led to the ural blocking high rebuilt. in addition, the distribution of the vertical motion on 700hpa shown that the surface high splitting was related to the considerable upward motion located on the southeastern part of surface high

    對1998年3月中旬一次高空阻塞形勢下強冷空過程進行了診斷析,著重討論強冷空爆發前後地面反旋活動與高空阻塞形勢調整的關系。研究結果表明,強冷空的爆發與烏拉爾地阻塞形勢的調整阻塞高壓的崩潰和重建緊密相關。對流層下部的溫度平流析表明,阻塞形勢的調整是由於阻塞高壓上游西北方有冷空侵入導致了阻塞高壓的崩潰,而上游來自西南方向的強流則導致高壓脊迅速發展,使阻塞高壓重新建立。
  11. It was well known that the main process of precipitation formation was collecting cloud water in the warm area and ice phase particles melting in the cold area. positive vertical velocity existed between 700hpa and 500hpa in the warm area and near surface in the cold area. wind convergence existed at the height of 700hpa, and divergence existed above and below the height of 700hpa

    通過對降水雲系的綜合研究,建立了河南省春季層狀雲降水概念模型:降水主要通過雲水碰並形成,冷降水機制以冰粒子融化等冷雲過程為主;700一50ohpa通常有上升流,冷上升佈在近地面附近: 700沖a存在風場的輻合,其上下則主要是輻散;水汽主要集中在7o0hpa高度上,水汽來自南、東南方向,冷水汽以西南輸送為主;位勢不穩定佈在o 。
  12. Temperature increased in most parts of the study area, with the most rapid increase occurred in the qinghai - xizang plateau

    大部秋、冬季節溫上升比春、夏季明顯,全國性的冬趨勢明顯。
  13. During the little ice age precipitation is little. due to different resolution, every record has difference in detail and also reflects area character

    結合孢粉資料析,在冷候變化中本植被類型變化不大,以落葉闊葉木本植被為主,草本植被為輔。
  14. On base of results above, composite model of ssta in pacific and circulation anomaly are constructed for analysis their evolution. during mature phase of el nino usually in winter, positive ssta dominates in tropical eastern ocean and negative ssta dominates in west wind drift district in mid - latitude ocean, correspondingly the pna index of 500 hpa geopotential height is positive which means the aleutian low gets strong, and the situation is somewhat inversely during la nina phase of ssta

    合成位相反映了太平洋ssta演變特徵,以及相對應的大環流異常特徵:當西風漂流處于態而熱帶中東太平洋海溫偏低時,合成大模型當中阿留申低壓減弱, 500hpapna指數為負異常;當西風漂流處于冷態,熱帶中東太平洋處于態( elnino峰值?成熟期ssta典型佈) ,合成大模型中阿留申低壓加強, 500hpapna指數為正異常。
  15. 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

    中尺度結構析表明,本次暴雨具有明顯的中尺度特徵,是由三支流共同作用的結果,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 )東路冷空主要是通過中低層侵入陜南地的,並與地面冷式錮囚鋒的形成密不可; ( 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,另一個是降水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 )本次暴雨的水汽主要靠偏南風急流將孟加拉灣和中國南海的水汽輸送至西北地東部,為暴雨的發生提供了必要熱力條件。
  16. Compared with the common situation, the result of numerical simulation shows that the cold air will result in an uncomfortable area indoors by using either of the method mentioned above

    對三種供方式在不同換次數條件下的溫度場和pmv佈模擬結果顯示,大換量將造成室內一部域的不舒適性。
  17. Across much of the storm ' s path, wind gusts have knocked down ice - coated power lines leaving hundreds of thousands of people without electricity, and, in many cases, without heat for their homes

    暴風雪侵襲的大部,被冰覆蓋的電線都被風吹倒了,導致成千上百的人沒有電,在很多地方房子都沒有供應。
  18. But warmer regions, such as southern europe, the us south and parts of asia, will suffer lower agricultural yields, droughts and the spread of human, animal and plant diseases, the scientists are expected to conclude

    但是,預計科學家們將得出結論稱,在候較為溫的地,如南歐、美國南部和亞洲部,將出現農作物減產、乾旱以及人類和動植物疾病蔓延等後果。
  19. New studies project that the arctic ocean could be mostly open water in summer by 2040 ? several decades earlier than previously expected ? partly as a result of global warming caused by emissions of greenhouse gases

    新的研究顯示,到2040年夏天的時候,北冰洋的大部域將為廣闊的水域-比之前預計會達到這種情況的時間要早了幾十年-一部是由於排放體溫室效應全球變而引起的
  20. Beijing has a semi - humid climate with clearly cut seasons. spring and autumn are short while winter and summer are long

    北京屬溫帶半濕潤,四季明,春秋短促,冬夏較長。
分享友人