冬季季風氣候 的英文怎麼說
中文拼音 [dōngjìjìfēngqìhòu]
冬季季風氣候
英文
winter monsoon climate-
Zhoushan has a northern subtropical monsoon marine climate with clear four seasons ; leading wind directions are southeast wind in summer, northwest wind in winter. with an annual average wind speed of 3. 3m s ; and an average temperature of 15. 6 - 16. 6, and the frost free period reaches 251 - 303 days perannum, annual average sunshine time 1941 - 2257 hours, and the annual preeipitation is 927 - 1620 mm
舟山屬北亞熱帶南緣季風海洋型氣候,四季分明主導風向,夏季為東南風,冬季為西北風,年平均風速3 . 3米秒年平均氣溫15 . 6 . - 16 . 6 ,冬季最低溫為- 1 ,夏季最高溫度為37無霜期251 - 303天,年日照時數1941 - 2257小時年降雨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 、就所選剖面分析來看,本區在全新世早期氣候回返,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;全新世中期氣候溫暖濕潤,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,氣候向乾冷方向轉化,但變化幅度遠小於末次冰期。No heating in winter is design demand for series east - china multi - span plastic greenhouses. the climate characteristic of east - china is : low temperature, raininess, few shine and often heavy snow in winter and spring ; high temperature, high humidity, more typhoon and rainstorm in summer and autumn, it concentrates all the disadvantageous factors for multi - span plastic greenhouses design
系列化華東地區連棟塑料溫室設計要求冬季不加溫,華東地區的氣候特點是:冬春季低溫、多雨、寡照、常有大雪;夏秋季高溫、高濕、多臺風暴雨,集中了連棟塑料溫室設計中各種不利因素。Occasionally, in winter, tropical cyclones traversing the south china sea pass to the south of hong kong just when a monsoon is affecting the coastal areas of south china
在冬季季候風影響著華南沿岸的時候,間中會有熱帶氣旋橫過南海,並於香港以南掠過。( 2 ) there is stage of soil formation from the evolution of pedogenic environment in the weihe valley during holocene. soil formation shows the law of evolving from warm and wet strong soil formation period to cold and dry dust deposition period ( weak soil formation period ) and to warm and wet strong soil formation period again. the loess - soil sequence is a compound soil sectional system of different kinds of soil evolution under different bio - environment and pedogenic processes
( 2 )通過對全新世渭河流域成壤環境演變問題的討論,揭示了全新世渭河流域土壤的發育具有階段性,表現為由溫濕的強成壤期向冷乾的沉積期(弱成壤期)演變、再向溫濕的強成壤期演變的規律;黃土一古土壤序列是不同生物氣候環境下、不同成壤過程發育的不同土壤類型演替而形成的復合型土壤剖面體系;而且由於冬夏季風環流及其環境效應在空間上的差異,使得復合型土壤剖面體系也存在著南北差異。According to main weather types, this paper determines the criterion for choosing typical month of meteorological model used in buildings energy efficiency, and founds the procedures of annual meteorological model in hot summer and warm winter zone
本文以深圳市為例,研究夏熱冬暖地區建築師用建築能耗計算方法。深圳市地處東南沿海,屬亞熱帶季風海洋性氣候,是夏熱冬暖地區的典型。1. meteorology of southeast asia : winter monsoon and cold surge ; summer monsoon, rainfall of china, mei - yu, fog and crachin, tropical cyclones, tropical synoptic systems, climate of hong kong
1 .東南亞氣象:包括冬季季候風與寒潮夏季季候風中國的降雨情況梅雨霧及蒙雨天氣熱帶氣旋熱帶天氣系統和香港的氣候。7. significant weather influencing relief of southeast asia ; large scale circulations in the tropics ; winter monsoon and cold surge ; summer monsoon ; rainfall of china ; mei - yu ; fog and crachin ; tropical cyclones ; tropical synoptic systems ; climate of hong kong
7 .東南亞地形衍生的天氣熱帶地區的大尺度環流冬季季候風與寒潮夏季季候風中國的降雨情況霧與蒙雨天氣熱帶氣旋熱帶天氣系統和香港的氣候。Significant weather influencing relief of southeast asia ; large scale circulations in the tropics ; winter monsoon and cold surge ; summer monsoon ; rainfall of china ; mei - yu ; fog and crachin ; tropical cyclones ; tropical synoptic systems ; climate of hong kong
東南亞地形衍生的天氣、熱帶地區的大尺度環流、冬季季候風與寒潮、夏季季候風、中國的降雨情況、霧與蒙雨天氣、熱帶氣旋、熱帶天氣系統和香港的氣候。Topographically, chongqing features hills and low mountains. it has a humid subtropical monsoon climate, characterized by warm winter, hot summer, little frost and snow, heavy fog and less - than normal sunshine
在地形上,重慶以小山和低山為主要特色。它以潮濕的亞熱帶季風氣候為主,其獨特的天氣特色是冬暖,夏熱,少霜雪,濃霧和低於常規的日照。Kunming belongs to the low latitude plateau mountainous country monsoon climate, because of locating in the western region of yungui plateau, the degree of latitude is low, the elevation is high, there are the wumeng mountains to be as the natural screen in the north, separating the cold air to go down south, the whole area is subjected to influence that come from southwest and warm moisture of indian ocean s flow more, adding there are the plateau lakes to regulate degree of humidity, becoming the four seasons of " summer have no intense heat, winter have no strict and cold ", such as pleasant weather of the spring
昆明屬低緯高原山地季風氣候,由於地處雲貴高原西部,緯度低,海拔高,北部有烏蒙山等群山作為天然屏障,阻隔南下的冷空氣,全區多受來自印度洋西南暖濕氣流的影響,加之有高原湖泊滇池陽宗海調節溫濕度,形成「夏無酷暑,冬無嚴寒」四季如春的宜人氣候。年平均氣溫為14 . 5 ,最熱月平均氣溫19 . 7 ,最冷月平均氣溫7 . 5 ,年平均日照時數為2400多小時。Overcast and rainy weather will accompany the winter monsoon to affect hong kong. under such wintry and windy conditions, the feeling of coldness will be particular strong
天陰有雨的天氣將伴隨冬季季候風到來,加上風勢頗大,市民會特別覺得寒冷。Climate : this zone mostly belongs to the subtropical monsoon climate, where four seasons are distinguishable, mild climate, winter is not too cold, summer is not too hot, rain fall is abundant
氣候:大多屬于中亞熱帶季風濕潤氣候,四季分明,氣候溫和,冬無嚴寒,夏無酷暑,雨量充沛。For instance, predictions for a severe winter didn ' t pan out the last time around, nor did projections for a brutal 2006 hurricane season
例如上次有關冬季氣候酷寒的預測並未實現,另外所謂2006年颶風季威力驚人的預測也一樣落空。O in the century. annual rainfall in hong kong was found to be inversely related to the strength of the monsoon in the preceding winter ( figure 3 ), e. g., following the weak monsoon in december 1994 - february 1995 ( preceding winter of 1995 ), 2754 mm of rainfall were recorded in 1995, 540 mm more than the normal rainfall of 2214 mm. figure 2
假若冬季季候風偏弱,隨后一年雨量偏多的機會亦會較高(見圖三) ,例如1994年12月至1995年2月期間的冬季(即1995年的前期冬季)季候風偏弱, 1995年錄得的年雨量達到2754毫米,比氣候平均的2214毫米多了540毫米。From time to time, under the influence of upper air disturbances, cold air from this anticyclone plunges southward through china and brings outbursts of cold air to the south china coastal areas
有時,在高空擾動氣流影響下,冷空氣會南下橫過中國。這些冬季季候風寒潮,最後為華南沿岸帶來一陣陣的冷空氣。Pressure is rising over central china. replenishments of the winter monsoon will progressively bring cold weather to southern china next week
預料一股強烈的冬季季候風會在周末及下周初為華南帶來寒冷的天氣。Under the influence of an intense winter monsoon, the cold air piled up over southern china advanced southwards and brought very cold conditions to the coastal areas of guangdong
受到強烈的冬季季候風影響,屯積在華南的冷空氣向南推進,引致廣東沿岸地區天氣嚴寒。Synoptic weather patterns leading to the arrival of cold surges of the winter monsoon in hong kong are examined and typical patterns are identified for the reference of forecasters
詳細分析過一些冬季季候風寒潮抵達香港之天氣圖形勢后,天文臺鑒定了典型的模式供預報員參考。Products from these global models are generally adequate for forecasting large - scale weather systems such as surges of the winter monsoon. however, limited by the coarse resolution of the data received, the grid point information is inadequate for resolving smaller scale features associated with inclement weather
在預報冬季季候風寒潮這類大尺度天氣系統時,上述資料一般來說是足夠的,但是對于中小尺度的惡劣天氣系統而言,資料的分解度就不夠精細了。分享友人