winter in july 中文意思是什麼
winter in july
解釋
七月里的冬天-
Centropages tenuiremis is a mainly dominant species in xiamen waters during winter - spring. there is a noticeable character in its life history, that in may and june, when the population of this species begin to reduce gradually, the females could produce diapause eggs with long spines on their surface to over summer - autumn ( from july to november )
瘦尾胸刺水蚤（ centropagestenuiremisthompsen & seott ， 1903 ）是廈門海區冬春季節的主要優勢種，其生活史中一個顯著的特點就是在種群數量逐漸減少的5 6月間，雌體會產出表面遍布長刺的滯育卵，以滯育形式度過不利其生長繁殖的夏秋季（ 7 11月） 。 -
Furthermore, weather phenomena uncommon in hong kong had occurred which included hailstorms in the urban areas in april, a waterspout at tathong channel in july, and regression of seawater at tsim bei tsui and sheung wan due to storm surge during typhoon utor also in july. last winter is the third warmest one on record
此外，有些在香港不常見的天氣現象都在2001年發生了：包括4月在市區發生的雹暴； 7月在藍塘海峽出現的水龍卷；及臺風尤特襲港時因風暴潮影響而在尖鼻嘴及上環出現的海水倒灌等。 -
Since the suggested method makes a significant improvement in wind speed, it is more suitable for wind field estimation over complex terrain than other methods which only concerns the effect of distance. then we calculate the wind change with evaluation, last we can conclude the wind abase the hilly terrain, we find the wind in westward and center plain is much smaller than other area. while the wind in northward hilly area is much bigger with the hilly arising. the wind of chongqing is the biggest period in spring ( april ), the smallest period in winter ( january ), the wind in summer ( july ) is bigger than its in autumn ( october )
本文利用重慶及其周邊地區的常規氣象站的1951 ? 1980年30年的風速平均資料，針對復雜地形風速診斷，以地理信息系統為數據處理平臺，根據重慶1 ： 25萬dem數據，來獲得重慶市實際復雜地形的高程，提出了一種適合於起伏地形的權重內插方法，通過引入一個表示地形起伏變化程度的因子，構造了一種新的權重函數，來處理復雜地形上的風速，通過與只考慮距因素同反平內插方法比較發現，本方法更適合在起伏地形條件下使用；然後根據經驗公式在地形上進行計算，得出重慶地區起伏地形下的風速分佈；得出重慶市的西部、中部平原地帶風速較小，而北部山區隨海拔高度升高風速也較大；重慶市風速最大時期為四月份，冬季一月份最小，夏季（七月份）大於秋季（十月份） 。 -
Through having done field surveys in the campus of chongqing university, this paper tested classroom indoor and outdoor climate parameters in june, july and september of 2005, it used questionnaire to acquire subjects ’ thermal sense, draft sense and humidity sense in classroom each month, and programmed composition to compute predicted mean vote and compared pmv with the field testing results of mean thermal sensation vote. it is discovered that pmv is overvalued the college student ’ thermal sensation in chongqing. it finds that people in chongqing adapt to the typical summer hot and winter cold sweltering weather
對重慶地區高校教室的現場調查，測試了重慶大學2005年六月、七月和九月教室室內外熱環境參數，通過採用問卷主要掌握了受測對象教室里的冷熱感、氣流感和潮濕感，通過編製程序求得預測平均熱感覺評價pmv的值，比較pmv和問卷調查得到的平均熱感覺mtsv ，發現pmv預測值高估了重慶地區高校學生的熱感覺，這里的人群對重慶這種夏熱冬冷地區比較典型的悶熱氣候具有一定的熱適應性，對現場問卷調查的結果進行分析，得出了室內空氣溫度、氣流速度、相對濕度與人體主觀感覺之間的回歸曲線，發現重慶地區高校學生熱中性時的空氣溫度為25 . 5 ， fanger根據歐美人群調查得到的公式計算出的預測熱感覺為中性時的空氣溫度為25 . 0 ，兩者相差0 . 5 。 -
Terence mckenna and peter meyer ' s timewave zero software that graphs time as a fractal demonstrates by graph the accuracy of the winter solstice of 2012 as the correct end - date of the mayan calendar with graph anomalies appearing in the months of july
特倫斯麥肯納和彼得梅耶的零點時間波軟體顯示的時間圖表是不規則碎片型，通過圖表上七月出現的不規則性來論證了2012年冬至日確實是瑪雅歷法的終結日。 -
Compared with annual variation averaged over china, rainfall in region 1 is more in winter and spring but less in july and autumn ; region ii a and ii b have more rainfall in september and october ; rainfall in region iii is less from november to march of the next year while more in july and autumn ; region iv has less rainfall in may and june ; precipitation in region vis significantly more from middle - dekad in june to first - dekad in july, which manifests the feature of meiyu in middle - lower reaches of the yangtze river ; region via and vib have more rainfall in november. the characteristic periods of time are defined which indicate the typical characteristics of rainfall in each region
與全國平均年變程相比，區域冬、春季降水偏多， 7 - 8月份降水相對偏少；區域a和b在9 、 10月份降水顯著偏多；區域11月至次年3月降水明顯偏少， 7 、 8月份降水相對偏多；區域5 - 6月份降水偏少；區域6月中旬到7月上旬降水顯著偏多，體現了長江中下游的梅雨特徵；區域a和b在11月份的降水相對偏多。 -
Moreover, seasonal cycle also has apparent decadal - scale variety from 1909 to 2002 : monthly mean temperature in winter time from 1983 to 2002 is obviously warmer than that from 1909 to 1931 ( 3. 7 warmer in february ), while colder in summer ( 0. 2 colder in july and august ) and annual range of temperature is lower 2. 5
季節循環也有明顯的年代際變化： 1909 1931年， 1932 1982年和1983 2002年三個時段，第二時段接近平均狀態，第一和第三時段冬、夏季對比有明顯差異，第三個時段的冬季明顯高於第一時段（ 2月份高3 . 7 ） ，夏季低於第一時段（ 7 、 8月份低0 . 2 ） ，年較差減小了2 . 5 。 -
The vertical diffusivity coefficients kv in january, april, july, october, 1997 are studied respectively. the result is same as the fact that the vertical diffusivity coefficient is large near the coastline and the vertical diffusivity coefficient is small in the interior. the vertical diffusivity coefficient assimilated in january is larger and the possible reason is that the vertical mixing of the south china sea is stronger in winter and there is a cool eddy in winter in the south china sea
我們分別做了1997年1 、 4 、 7 、 10月份的k _ v ，結果與垂直混合系數在岸邊附近較大，在海洋內部較小這一事實相一致， 1月份同化的垂直混合系數值偏大分析原因是冬季南中國海垂直混合較強，可能也與在南中國海內部冬季有一個冷渦有關系。 -
With composition analyzing and significance test of simultaneous & previous general circulation and surface temperature of extreme warm or cold january & july in heilongjiang province, distinct difference can be concluded in terms of statistics between previous general circulation or surface temperature and the tempreture of heilongjiang province, which gives some evidence for predicting extreme warm or cold temperature of heilongjiang province ' s winter and summer
通過對黑龍江異常暖與冷7月和1月的同期和前期環流場和下墊面溫度距平的合成分析和差值顯著性檢驗，歸納出了前期環流場和下墊面溫度統計上顯著的差異，所得的結果可以為預報黑龍江夏、冬季異常暖、冷提供依據。 -
Because in july the sun ' s radiation is lower in scs than east china sea and the air temperature difference of winter and summer is smaller, the thermocline intensity is weaker in scs than in huanghai and east china sea
由於夏季日輻射相對低、冬夏季溫差小等原因，夏季南海溫躍層強度較黃、東海弱。本研究工作在溫躍層統計方法的確定、結果驗證上作了大量工作，並有所創新。
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