summer wind 中文意思是什麼
summer wind
解釋
夏風-
Such results are gotten : due to the unique topography the wind of beijing area during the day time is southern anabatic wind and in the night is northern katabatic wind in summer
研究結果表明: 1北京區域夏季邊界層風場受西北特殊地形的影響，夜間低層大氣流場常表現為由北向南的下坡風，白天逐漸轉為由南往北的上坡風。 -
In fuggy summer, the wind from the worn proof brings a bit of cool here
悶熱的夏日，來自房頂的自然風為這里帶來清涼。 -
From the numerical modeling results, it can be found that there is a clockwise gyre in the middle part of bohai sea, whether in wintertime or in summertime. in summer, the clockwise gyre corresponding to the high - temperature and low - density center in the middle bohai sea is mainly dominated by the density circulation. and in winter, it is mainly dominated by the wind stress curl
通過數值模擬結果發現，在渤海中部，無論冬季還是夏季，都存在一個順時針的渦旋運動，夏季，對應于渤海中部的高溫低密中心，其流場主體部分呈順時渤海冬夏季環流特徵及變異的初步研究針向旋轉，這主要是密度環流占優的結果，而冬季的順時針向的旋轉，主要是海面風應力旋度影響的結果。 -
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 -
When the light summer wind stirred amidst the trees of the garden, there came through the open door the heavy scent of the lilac.
當夏日的輕風在花園里樹叢間吹拂的時候，從開著的門里就傳來濃烈的紫丁香香味。 -
Unadorned and kind hotan people work hard day and night, wearing big hats which can stop wind and sand, shade sunshine in summer, keep warm and resist against wind and snow in winter
樸實善良的和田人民頭頂大帽日夜操勞，夏日擋風沙、遮太陽；冬天保暖又抵擋風雪的侵襲。 -
If the fed becomes overzealous in the pursuit of a stronger dollar … then we cold wind up with another uptick in short - term interest rate like we had late last summer, and it would pull the rug out from under us again
如果聯邦儲備局過度熱衷尋求強勢美元… …那麼我們可能導致像去年夏末一樣再一次短期利率升高，那將使我們再度失敗。 -
It also explain that the correlation between ssta of kuroshio and the change of wind field in equaroral mid - pacific is results of air - sea interaction ; however, when time comes into summer, the instance status of ocean is different from the last winter to next early springtime, the sea surface temperature turn into the definitive factor, so the increase of heat flux in may to jun month which is realized by absorbing more heat from the sun radiation results in the decrease of sst in kuroshio in the season of jun - jul. finally, during the aug to dec season of next year, the sst of kuroshio is increasing again
最後分析了黑潮海溫與夏季東亞大氣環流及我國降水的時滯關系，發現：當前冬黑潮區域海溫異常偏高時，後期夏季亞洲低壓的強度減弱，西北太平洋副熱帶高壓強度加強，而且位置西伸、偏北，梅雨鋒位置偏南，長江中下游地區降水偏多，北太平洋冬季海域的海溫分佈呈+ 、 - 、 +趨勢（順序為赤道中東太平洋、西北太平洋、我國近海） ；反之亦然。 -
On base of the data analysis, three - dimensional tide - induced residual currents, the wind - driven and thermohaline currents in the bohai sea are diagnostically computed with an orthogonal curvilinear grid system, by means of a three - dimensional ecomsed model. the winter and summer thermohaline structure and circulation characteristics in bohai sea are analysed, and the circulation variance is discussed preliminarily. the tides and tidal currents in bohai sea are well reproduced
在資料分析的基礎上，應用三維斜壓ecomsed模式對渤海的潮致余流、風生環流和密度環流進行了診斷計算，分析了渤海冬夏季的溫鹽場結構和對應環流的特徵，並對渤海上述幾個不同時期的環流變異進行了初步的分析和探討。 -
The updated model with complete forcing has excellent ability of simulation and forecast. to study yellow and east china circulation in winter and summer, based on long - term ocean observation data of january and august, the fine structure of yellow and east china seas circulation is diagnostically calculated with complete forcing ( including surface wind stress, boundary transportation, baroclinic effect, tide, changjiang river runoff ) in winter. the influences of factors on main circulation patterns are discussed respectively
對于冬季和夏季海洋環流的情況，在多年觀測的溫鹽資料基礎上，分別以1月份和8月份代表黃東海冬季和夏季的情況，以月平均大氣風應力、邊界流輸送、溫鹽斜壓效應、潮汐、長江口徑流等作為強迫條件，對黃東海環流的細微結構作了高分辨的三維數值模擬，探討了各因子對冬、夏季主要流系的動力學作用。 -
The reverse distributions pattern of ssta over the east pacific region and west wind drift region not only occurs in the summer of severe drought and flood years of north china, but also in the preceding spring
（ 3 ）赤道東太平洋和西風漂流區相反的海溫距平場配置不僅出現在華北夏季嚴重旱澇年同期，在前期春季也表現得十分清晰。 -
In summer wheat waved in the wind, producing the song of a golden ocean
夏天麥子在風中搖曳，像是在金色的海洋中唱歌。 -
Her laugh was as grateful to him as a summer wind.
她的笑聲對於他好象夏天的風一樣令人愉快。 -
Further, correlation analysis is used to the summer rainfall and four seasonal north pacific ssta, the results suggest north pacific ssta which notability cause the summer rainfall anomaly over eastern china are prophase winter ssta of kuroshio region of northwestern pacific, prophase spring ssta of middle and eastern equatorial pacific and summer ssta of west wind drift region
進一步對上述東部夏季降水異常區夏季降水與春夏秋冬太平洋海溫異常作相關分析，表明對中國東部夏季降水有顯著影響是：西北太平洋黑潮海區前期冬季海溫異常、赤道中東太平洋前期春季海溫異常、中高緯太平洋西風漂流區同期夏季海溫異常。 -
In the scorching summer, whenever going hiking among forests on mogan mountain, you will soon feel cooling down. and soft wind breezing brings you a kind of unutterable comfort. mogan moutain, what a cool and refreshing world
盛夏炎日，一走進浙江莫干山的林間小道就汗止心涼，加上輕風拂煦，渾身有說不出的舒坦，忍不住要贊嘆一聲：莫干山，好一個清涼世界！ -
Hongzhushan hotel is located at the foot of mt. emei that is one of one of the four buddhist mountains in china, covering 440, 000m2, which is a shining pearl on mt. emei that is on the heritage list of the world nature and culture. there is only a strip of water between hongzhushan hotel and baoguo temple. if one goes to hongzhushan in spring, everything is green and still, if in summer, a good cool, if in autumn, its wind will give you a jolly cool, if in winter, just enjoy the silver world
紅珠山賓館座落在中國四大佛教聖地之一的峨眉山麓報國寺旁，可聞晨鐘暮鼓，盡沾仙山之靈氣，地理位置得天獨厚。賓館佔地面積44萬平方米，其中紅珠湖1萬平方米，森林覆蓋率98 % ，館內古木蔽日綠水環繞鳥語花香，幢幢別墅如林海珍貝，鑲嵌于峨眉山林海碧波之中，自然環境無與倫比，素有「森林酒店」之美譽。 -
The sound of wind in the pines, like waves, birdsong, and insects, inspires enlightenment. summer brook, autumn valley, spring flower, and winter snow are manifestations of truth
松濤拍岸，鳥叫蟲鳴，無非是悟道的契機；夏澗秋谷，春花冬雪，無非是真理的示現。 -
It is about 20kilometers apart for people to stay. looking into the distance from the upper part of the building, you can see the river with green water weeping willow branches saway gentily in the dyed white snow. the ever - changing jilin frost - branch is a marvelous willow branches swaying gently in the wind. it is an excellent summer ressort
居高眺望，可俯視松花江兩岸風光，夏見碧水長流綠波蕩漾，垂柳搖曳清風送爽，是極好的避署之處冬觀銀裝素裹，千姿百態，聞名遐邇的吉林霧淞，大自然的鬼斧神功，令人嘆為觀止。 -
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。 -
I sit at the open window to enjoy them ; and hear only the voice of the summer wind
我坐在敞開的窗前欣賞著這夜色，耳邊只聽見那夏天的風聲。
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