雨期氣候 的英文怎麼說

中文拼音 [yǔqīqìhòu]
雨期氣候 英文
pluvial climate
  • 雨 : 雨名詞（從雲層中降向地面的水） rain
  • 期 : 期名詞[書面語]1. （一周年） a full year; anniversary 2. （一整月） a full month
  • 氣 : 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...
  • 氣候 : 1. （氣象情況） climate; weather 2. （局勢） climate; situation 3. （結果; 成就） successful development
  1. The result indicates that key stages include the growth stage of late autumn treetop 、 bud differentiation stage and anthesis stage, and that key climate factors are temperature, precipitation, rainfall days and sunlight time

    結果表明：氣候條件影響廣西地區龍眼產量的關鍵時期為晚秋梢生長期、花芽分化期和開花座果期，關鍵氣候因子分別為氣溫、雨量、雨日和日照時數。
  2. Fuhong class a inorganic dampproof fireproof board adopt natural minerals, featuring good performance in water, sunshine, acid rain, and frosted condition, its lifespan can last as long as more than 20 years, it keeps room warmer in winter and cooler in summer, damp - resistant, wet - resistant, it is applicable to island climate, and wont generate halogenation like ordinary fireproof board

    福宏a級無機防潮防火板：為天然礦物研製而成，具備了礦物應有的特性，長期水浸日曬酸雨寒凍也不脫層變質或腐蝕，使用壽命更可達20年以上且冬暖夏涼，又能抗濕抗潮，更能適合海島型氣候，絕不會有一般防火板材的反鹵現象。
  3. 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
  4. The modified zndx in comparison with others is well indicative of the severity and extent of flood / drought event and of more objective classification of them, which is therefore quite applicable to a extended area. ( 3 ) the main anomaly structures of grades of drought / food in summer over northwest china present pluvial pattern and dry pattern in all the areas, and spatial changes are opposite pattern from the noth to the south and the west to the east. the first four rotated loading vector fields represent four principal precipitation anomaly areas : the weishui river basin, east of the qinghai - xizang plateau

    但修訂過的zndx指數根據氣溫、土壤濕度及前期氣候濕潤度等因子能夠客觀的反映出西北地區的旱澇特徵。 （ 3 ）西北地區季與年區域旱澇等級表明：西北地區的乾旱雨澇有顯著的階段性和年際變化特徵。 1980 』 s到1990 』 s中期，氣候較濕潤，土壤濕度增墑較明顯； 1990 』 s中期以後是40年乾旱最異常的時段； 1960 』 s旱澇交替發生，旱澇趨勢接近常年； 1970 』 s氣候雖乾旱，但沒有1990 』 s中後期顯著。
  5. Yueyang is a wettish area of confienental subtropical monsoon with mild climate, plenty of rainfall and four distinct seasons. annually, the average temperature is about 17, the average precipitation is 1387. 93. mm, the average sunlight time is 1680 hours, and the frost - free period lasts 270 days

    岳陽市屬亞熱帶季風濕潤氣候區、氣候溫和、雨量充沛、四季分明，年平均氣溫17左右，多年平均降雨量1387 . 93毫米，年平均日照1680小時，無霜期270天。
  6. Moreover, milking wheat should be irrigated since the weather is very drought and short of rainfall from maize interplanting to jointing stage

    另外，灌漿小麥應當灌水，因為玉米套種至拔節期氣候乾燥少雨。
  7. Result shows that summer precipitation in north china has gone through four major dry - damp phases, richer periods from 1900 to 1915 and from 1946 to 1978, less periods from 1916 to 1945 and from 1979 to 2001, and has obvious inter - decadal variations, and has about 60a, 20 - 30a, 10a major periods and has twice abrupt changes in 1953 and 1979

    結果表明：華北夏季降水經歷了四個主要干濕階段，即1900 1915年和1946 1978年為多雨期， 1916 1945年和1979 2001年為少雨期，具有明顯的年代際變化，主要有約60年、 20 30年和10年左右的周期，並在1953年和1979年發生了兩次氣候突變。
  8. The location of quangan city is at subtropics moist monsoon climatic region with plenty heat, plenty rain

    廣安市地處中亞熱帶濕潤季風氣候區，氣候溫暖，熱量充足，雨量豐沛，空氣濕度大，日照少，霜期短，風力小。
  9. The whether during the chung yeung festival period will be very hot, while both the cemetery and the bus stop it is anticipated that the weather during chung yeung festival period will be very hot, and as there is little shade available, grave sweepers are advised to make preparations to the extreme weather. grave sweepers are also reminded to remain clam during queuing, and follow instructions given by the police security personnel on ground

    由於天氣可能會非常酷熱，而巴士站及墳場地內只有極少遮陰位置，參加人士應作好預備，如帶備足夠的飲用水、雨傘和太陽帽；掃墓人士在輪候期間請耐心等侯，切勿推撞，並請依照在場維持秩序的警務人員和保安員的指示，以免發生危險。
  10. Baced on the general circulation background, synoptic - climatological cause and external forcing predictor of rainfall of yunnan in may, the composite model of the long - term weather process of yunnan in may for rainfall and the optimum subset regression model of rank statistics applied for dryness and wetness forecasting are presented

    摘要根據影響雲南5月旱澇的大氣環流背景、天氣氣候成因以及外界強迫因子，提出了雲南5月雨量的長期天氣過程的物理概念模式和用於旱澇預測的秩序統計量最佳子集回歸模式。
  11. It is easy to become epidemic in the period of bloom to pod of broad bean plants, especially in conditions of lower temperature and rainy days

    發病盛期為開花結夾期，低溫多雨的氣候發病重，發病程度與溫度、田間濕度及土壤肥力密切相關。
  12. Annual precipitation series about 50 years is stable and no period ; further, the climate drying and desertification are n ' t caused directly by the decrease of precipitation during the period of the research according to the relational analysis among precipitation temporal - spatial change, runoff, evaporation, potential evapotranspiration and soil water ; longyangxia reservoir which was built in 1986 does n ' t have influence on precipitation up to now ; but annual temperature series in gonghe is unstable, having a linear upward trend, and it increases about 0. 0247, 0. 0422 and 0. 0272c per year, and temperature rise must be having an influence on desertification, but there is a very little temperature change, so that the effect is very small ; annual potential evapotranspiration series is stable too, so climate change has little influence on plant water consumption. 2

    在青海共和盆地，近50年的年降雨量序列是平穩的、無周期，其時空變化與徑流、蒸發、潛在蒸散和土壤水分的關系表明，氣候乾燥和嚴重的荒漠化不是由於降雨量減少直接引起，龍羊峽水庫對共和盆地年降雨量變化沒有影響；但是年氣溫序列是非平穩的，茶卡、恰卜恰和貴南的年氣溫平均每年升高0 . 0247 、 0 . 0422和0 . 0272 ，且氣溫升高2 ，年潛在蒸散增加57mm ，盆地內氣候逐漸變乾燥，但影響比較小；由於歷年潛在蒸散序列是平穩的，因此氣候變化對盆地的作物潛在蒸散的影響在研究期內是較小的。
  13. Using the daily rainfall data of 740 stations over china and ncep daily up - ai data from 1971 to 2000, we analyzed the average mei - yu climate field. based on the climate field and mei - yu intensity index, we confirm that the year of 1999 is a typical mei - yu. besides, the intensity of mei - yu rainfall in 1999 is the highest since we had record, so the analysis of mei - yu in 1999 can present the common characteristics of mei - yu

    本文利用1971 - 2000年中國740站的日平均降水資料和ncep的日平均高空資料分析了梅雨氣候場，利用梅雨的氣候場及中國氣象局氣候診斷預測室的梅雨強度綜合指數，確定了1999年是一個非常典型的梅雨年，並且1999年梅雨期間的降水強度是歷史以來的最高值，因此我們對1999年梅雨進行的分析有很大的代表性。
  14. 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。
  15. Climate : located in the temperate zone of east asia, binzhou has a sub - humid continental monsoon climate featuring four distinct seasons

    氣候特點：屬東亞暖溫帶亞濕潤大陸性季風氣候，冬冷夏熱，雨熱同期，四季分明。
  16. Based on case study and climate analysis, this work arrives at the central cause of dv of the meiyu rainfall, which lies in the regional difference in dv of the lower - level temperature field of east asia, and the cause relates essentially to 1 ) distinct topography in this region and 2 ) a particular cloud pattern during the wet season

    本文通過實例分析、氣候比較和數值模擬認為：梅雨降水日變化的根本原因是東亞低層大氣溫度場日變化的區域性差異，造成這種差異的基本原因又包括兩個方面，一是東亞特殊的地形構造，二是梅雨期內特殊的雲區分佈。
  17. So far, only a handful of cores have been drilled that go back to the last ice age and none of them provide enough information to prove how the amazon rainforest reacts to climate change

    參考譯文）迄今為止，只鉆探出來少量上次冰川期的核心物質，這些物質無法提供足夠的信息證明亞馬遜雨林如何對氣候變化作出反應。
  18. The change of meiyu periods is closely related with the frequently postponed phenomena of their ending dates and the later onsets of high summers in the mid - lower yangtze

    此兩時段梅雨由弱轉強和出梅入夏期由偏早轉為延遲呈密切聯系，這在相當程度上反映中國東部夏季氣候水資源分佈的突變。
  19. Fluorine carbon coating has outstanding anti corrosive properties and weathering resistance, resisting acid rain, salt fog and various air contaminants, having good performance of thermal and cold endurance, resisting strongultraviolet irradiation, keeping no fading and chalking for a long period, and having long service life

    氟碳塗層具有卓越的抗腐蝕性和耐候性，能抗酸雨鹽霧和各種空氣污染物，耐冷熱性能極好，能抵禦強烈紫外線的照射，能長期保持不褪色不粉化，使用壽命長。
  20. The summer climate of north china is wetter with more frequent flood from the 1950s to the 1960s and drier with more frequent drought from the 1980s to the 1990s

    夏季華北地區五十年代到六十年代中期氣候偏濕，以雨澇多見；八十年代到九十年代初期氣候偏干，以乾旱多見。
分享友人
分享到 Line

分享到臉書