summer annual 中文意思是什麼

summer annual 解釋
春播一年生草
  • summer : n 1 夏季。2 壯年時期；最盛期。3 年歲，年齡〈通常附帶數詞而用復數〉。adj 夏季的。 a summer bonnet ...
  • annual : adj. 1. 每年的；年度的；一年（一次）的。2. （植物）一年一生的，一季生的。n. 1. 一年生[一季生]植物。2. 年刊，年報，年鑒。adv. -ly 年年，每年。
  1. Taking loess cave dwelling of yan an area as represen t area ， the annual temperature wave inside the cave dwelling are solved under t he annual temperature wave of outside disturbance in yanan furthermore ， by comparing with that of bungalows ， the characteristics that warm in winter and cool in summer in cave dwelling are illustrated in quantity

    以延安地區黃土窯洞為模型，以當地的室外年溫度波為外擾，用反應系數法求解和分析了窯洞室內的年溫度變化;並與相同空間結構，相同外擾作用下的平房作了分析比較，定量的說明了窯洞與平房相比具有冬暖夏涼的優點。
  2. 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
  3. Score one for neighborliness when volunteer firefighters from winifred and hilger, small towns 23 road miles ( 37 kilometers ) apart, defy summer storm clouds to assemble for their annual softball duel

    當夏季的暴風雨來到溫妮弗萊德和西爾格，兩個相隔23里路程（合37公里）的小城鎮，的自願消防員們年度壘球對抗賽的上空時，他們的堅持比賽為他們的友誼又加上了一分。
  4. 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水減少、氣溫遞增，其中近50年的時間里，氣溫共遞增0 . 185 ，同時降水減少75 . 35mm ，表現為暖干化特點，其暖化的特點表現在冬半年的暖冬尤其是冬季增溫強烈，干化則主要集中在夏季降水的銳減；而秦嶺西部地區則降水減少的同111氣溫下降，近50年來，氣溫共下降0
  5. The resuts showed that the annual average temperature had an increasing trend ; summer, autumn and winter average temperature also had an increasing trend and the amplitude in winter was bigger ; the change of standard deviation and coefficient of variation were acute during winter ; the coefficients was bigger ; the change of standard deviation and coefficient of variation were acute during winter ; the coefficients of skewness were positive value during summer and autumn ; the kurtosis coefficients were bigger during winter

    得出如下結論：和田地區年氣溫有增加的趨勢；夏季、秋季、冬季氣溫也有增加的趨勢且冬季氣溫值增幅較大；標準差及變差系數都是冬季變化較為劇烈；偏度系數在夏季及秋季為正值；峰度系數值在冬季較大。
  6. The precipitation frequencies is analysed according to 1956 ~ 2000 years of rainfall record series in baoding area. the features of distribution of rainfall are detailed evaluated. firstly, the distribution of monthly precipitation is not even. for instance. the annual rainfall amount is about 548mm in whole year, about 80 % of them in summer season. secondly, yearly variation of rainfall is greater. thirdly, the abundant years usually are followed by short years, but the important changes have taken place in the last decades. before 70 ' s the abundant years took the dominant position, from the 70 ' s to the middle of 80 ' s the short years took place more frequently than ever. after the later of 80 ' s, the short years hold the main position. the above knowledge is instructive for guiding the rainwater resources effective utilization

    本文利用1956 2000年保定市的長系列降雨資料，對保定市降水量進行了頻率分析、年內變化分析和多年變化分析，明確了保定市降水量年內、年際間的變化情況：保定市降水量年內分配不均，汛期（ 6 - 9月）占年降水量的81 。保定市降水量年際間變化大，豐水年和枯水年交替發生， 70年代以前以豐水年段為主； 70年代到80年代前期降水量豐枯交替頻繁，總的接近於枯水年段； 80年代後期至今以枯水年段為主。這種降水分佈規律對農業生產雨水資源的高效利用具有重要的指導意義。
  7. By using ncep / ncar reanalysis data of height and wind, the inter - monthly lpac map, the climate lapc map, inter - annual anomaly map and mean variance map of monthly wind field of 850 and 500hpa and monthly height field of 850, 500, 150, 30hpa are calculated in a globe - belt area, which situates between 30 s and 75 n, from december 1957 to december 1997, according them we analysis the rule of the season transfer and anomaly of nh mean circulation. the results show that the climate map of lapc can describe the seasonal transfer process of large scale circulation better. the advance process of summer circulation establish is form south to north at the middle and lower level of the troposphere, that is reflected primly in the inter - monthly wind and pressure map of lapc ; at lower lever of stratosphere, the establish process is simulate to that of troposphere, and reflect of process of that the south asia high toward plateau ; at middle stratosphere the summer circulation establish begins at middle and high latitude initially, and then transmits to low latitude gradually, while the seasonal variability in mid - stratosphere is stronger than it in troposphere and low - stratosphere

    利用ncep ncar再分析高度場和風場資料，計算了30 s 75 n球帶區域1957年12月至1997年12月逐月850 、 500hpa風場及850 、 500 、 150 、 30hpa高度場月際局地型相似系數圖、多年平均圖（即氣候lpac圖） 、年際異常圖及均方差圖，在此基礎上，分析了北半球平均環流季節轉換及其異常的規律。分析表明，氣候局地型相似系數圖較好地給出了大尺度環流季節轉換發生的過程：在對流層中、下部，風、壓場月際局地型相似系數圖清楚地反映了夏季型環流建立由南向北的推進過程；低平流層夏季型環流的建立與對流層接近，其中，南亞高壓上高原過程有明顯反映：中平流層，夏季型環流的建立明顯表現為從中、高緯度開始，逐步向低緯傳播的特徵，且變化較對流層和低平流層明顯。
  8. 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。
  9. Annual mean flux in togara strait was about 27. 9sv and the flux in summer was larger than that in spring and winter, as well as smallest in autumn

    吐噶喇海峽水交換量年平均27 . 9sv ，夏季最大，春季、冬季次之，秋季最小。
  10. In a year the change of river flow is drastically and season distributes of runoff in river is mainly centralize in the summer in jia - lu - he, qiu - shui - he and pian - guan - he catchments. for example, the runoff amount from july to august accounts for 41 %, 58 % and 57 % of the annual runoff amount in the above three catchments, respectively

    所選四條流域中，佳蘆河、湫水河和偏關河三條河流徑流量年內變化劇烈，季節分配不均，集中度高， 7 8月份徑流量分別占各流域年徑流量的41 、 58和57 。
  11. In order to study the variation characteristics of heat flux at nansha and xisha islands in the south china sea, the observational data from the ocean stations are calculated to obtain air - sea heat exchanges and the annual circulation of heat budget around the summer monsoon onset in 1998

    摘要為探索西沙和南沙海氣熱通量時間演變特徵，用海洋站觀測資料計算了1998年南海夏季風爆發前後，海氣界面熱量交換值及海面熱收支年循環。
  12. The responses of asian monsoon circulation to the heat source annual anomalies over the bay of bengal and philippines in summer and the annual relationships between the heat sources over the bay of bengal and philippines and the precipitation of china in summer are studied emphatically, with the results as follows : ( 1 ) the coverage and intensity of atmospheric heat source are the largest and strongest in summer and then turn smaller and weaker in autumn and winter, and in turn begin to become larger and stronger in spring again

    著重討論了夏季孟加拉灣和菲律賓熱源年際異常時，亞洲季風環流系統的響應，及其與中國夏季降水的年際關系。結果表明： （ 1 ）夏季大氣熱源的范圍最大，強度最強，以後以秋、冬季依次變小變弱，春季又開始變大變強。夏季亞洲季風區有三個強的大氣熱源中心，其中以孟加拉灣熱源最強，菲律賓熱源和印度半島西部熱源次之。
  13. Using the daily and monthly ncep / ncar reanalysis data from 1951 to 2000 and monthly precipitation of 160 stations in china in summer from 1951 to 2000, the climatic distribution of heat source are computed. the responses of the asian monsoon circulation to the annual anomaly of the heat source over the bay of bengal in summer and the annual relationship between the heat source and the precipitation of china in summer are analyzed

    摘要利用1951 - 2000年ncep / ncar再分析逐日及月平均資料和我國160個測站1951 - 2000年月降水量資料，計算了夏季大氣熱源氣候分佈，分析了夏季孟加拉灣地區熱源年際異常及亞洲季風環流系統的響應，以及夏季孟加拉灣地區熱源與中國夏季降水的年際關系。
  14. Crystal socha shows her american paint horse, summer, during the 11th annual e - quifest of kansas in kansas

    近日，在美國堪薩斯州第11屆馬術節上，克里斯托?索卡向人們展示她的美國花馬「夏天」 。
  15. C or below will decrease. " by the decade 2090 - 2099, the annual number of very hot days in summer will have risen from the 1961 - 1990 average of 11 days to 24 days. the annual number of hot nights in summer will see an even greater increase, from 8 nights to 30 nights

    楊繼興說：到二九至二九九年，每年夏季酷熱日數可能會由一九六一年至一九九年的平均值11日變為24日，每年夏季熱夜數目的增幅更大，會由八晚變為30晚。
  16. " by the decade 2090 - 2099, the annual number of very hot days in summer will have risen from the 1961 - 1990 average of 11 days to 24 days. the annual number of hot nights in summer will see an even greater increase, from 8 nights to 30 nights. the annual number of cold days in winter will have dropped from 21 days to less than a day

    楊繼興說：到二九至二九九年，每年夏季酷熱日數可能會由一九六一年至一九九年的平均值11日變為24日，每年夏季熱夜數目的增幅更大，會由八晚變為30晚。
  17. In july, although the moisture transport from tropical indian ocean reaches its annual maximum to shandong, its contribution to summer rainfall over shandong during july and august is undistinguished. on the other hand, the contribution from sub - tropical west pacific is evident

    7月雖然來自熱帶印度洋季風區的水汽輸送通量達到最大值，但7 8月它們對山東夏季降水異常的貢獻並不顯著，相反來自南海-西太平洋、中國大陸-日本海的水汽輸送以及西風帶天氣系統對山東夏季降水異常的貢獻較顯著。
  18. The main results are as follows : ( 1 ) in the most of places of naqu, the annual sunshine duration are more than 2550 hours and average wind velocity are higher than 4m ? s ^ ( - 1 ). ( 2 ) the sunshine duration in spring, summer, autumn, winter, growing season ( from may to september ) and a year all decreased in recent 40 years. ( 3 ) the wind velocity in winter decreased and the wind velocity in other 5 periods all increased. ( 4 ) the sunshine duration and wind velocity in 1990 ' s were smaller than that in 1980 ' s for all 6 periods. ( 5 ) the sunshine duration and wind velocity from 2000 to 2005 could continue to decrease

    主要結果是：那曲大部分地區，年總日照時數大於2550小時，年平均風速大於4m ? s ^ （ - 1 ） ；近40年那曲地區春季、夏季、秋季、冬季、生長季（ 5 - 9月）和年6個時段的日照時數均呈減少趨勢；風速冬季呈減少趨勢，其它時段呈增加趨勢； 6個時段的90年代日照和風速都小於80年代； 2000 - 2005年日照時數和風速繼續減小的可能性比較大。
  19. The annual precipitation has a fluctuation change trend, the precipitation increases obviously in winter, the summer precipitation and the annual precipitation increase slowly, in each age the maximum precipitation in winter, summer, autumn and the maximum annual precipitation all appear at the beginning of 21st century in which the air temperature is warmer, the climate has a change trend from dry and warm to wet and warm

    年降水呈波動式變化趨勢，冬季降水增加明顯，夏季和年降水增加緩慢，各年代中冬季、夏季、秋季和年最多降水均出現在氣溫偏暖的21世紀初，氣候有從暖干向暖濕轉變的趨勢。
  20. The wind in summer dominates other seasons with annual mean westerly on the equator

    夏季的風應力在一年中佔有優勢，在赤道上出現了西風。
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