summer belt 中文意思是什麼
summer belt
解釋
夏帶-
Officers use the winter and summer service uniforms as parade uniforms by adding a brown leather belt and white gloves
軍官在使用冬常服和夏常服在正式場合要佩戴棕色皮帶和白手套。 -
The above circul ation structure cause that rain belt tend to north in summer in china, rainfall of the yellow river valley and north china become more, but rainfall of south to the yellow river and yangtze river valley become less, meanwhile temperature of northwest and central region become high, but temperature of south department foreland become low
這樣的高低空的環流配置造成我國夏季雨帶位置偏北，多雨區在黃河流域及華北地區，而黃河以南、長江流域降水偏少，同時我國西北和中部地區氣溫偏高，南部沿海地區的氣溫偏低。 -
It was found that the " key regions " from which moisture transports influenced shandong summer rainfall lies in tropical india ocean, south china sea to tropical west pacific, china mainland to japan sea and the upstream area in westerly belt by analysis of svd method on water vapor transport
夏旱年則相反。通過對旱澇年水汽輸送與山東夏季降水的相關分析，山東夏季降水和水汽輸送svd分析，發現：影響山東夏季降水的水汽輸送「關鍵區」主要位於熱帶印度洋、南海-西太平洋、中國大陸-日本海以及山東上游西風帶地區。 -
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。 -
Seasonal variations of water vapor transport over east asia monsoon region are studied, especially that in summer season. the results indicate that there are four vapor inflow corridors to fetch china : southwest corridor, south china sea corridor, southeast corridor and northwest corridor. it shows impact of south asia monsoon, south china sea monsoon, subtropical monsoon and middle latitude westerly belt on summer rainfall anomaly over china, respectively
分析了東亞季風區水汽輸送的季節變化，並著重研究了夏季東亞季風區的水汽輸送特徵，指出夏季東亞季風區水汽輸送有四條通道到達中國大陸：西南通道、南海通道、東南通道和西北通道，分別體現了南亞季風、南海季風、副熱帶季風和中緯度西風帶對中國夏季降水的影響。 -
We classified flood and drought years of summer and autumn, it is pointed out in the paper that there are circulation anomaly in 500mb height field before flood or drought years. we also find out that there are intimated relation between autumn floods and droughts of zhejiang province and the macro - scale rain belt. the meteorological elements emergence abnormal features in summer before flood and drought years. we make out predictor to predicate summer precipation
論文結合三種排序方法劃分了夏秋旱澇年，研究表明，夏季、秋季旱澇年前期冬季和夏季500hpa高度場環流有明顯的異常特徵，夏秋旱澇與我國夏秋大尺度天氣氣候異常有密切的關系，旱澇前期我國氣象要素場有明顯的異常特徵。製作了浙江省夏季旱、澇預報工具。 -
It is mountainous area with peak over peak and there are more than 20 peaks with altitude over looom. the reserve is located in the transitional climatic belt between middle subtropical zone and north subtropical zone, with distinct four seasons, cold whiter and hot summer
湖北后河國家級自然保護區位於湖北省西南部的五峰土家族自治縣境內，地理坐標位於東經110 29 25 110 40 45 ，北緯30 2 45 30 8 40 。該區地處中亞熱帶與北亞熱帶過渡帶，屬亞熱帶季風氣候。
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