清半夏 的英文怎麼說
中文拼音 [qīngbànxià]
清半夏
英文
qingbanxia pinellia tuber rhizoma pinelliae-
Supreme master ching hai arrived at 7 : 30 p. m., wearing a simple, yet elegant white evening gown enhanced with a white shawl. as she walked down the red carpet to the vip entrance, mr. shadyac stopped his conversation with his son, director producer tom shadyac patch adams, liar liar, the nutty professor to greet master and escort her into the vip room. he proudly introduced her to many of his important friends such as former television talk show host, phil donahue ; actress and wife of phil donahue, marlo thomas ; st. jude s regional director, shoshana grammer ; mike driebe, the st. jude representative who received the contribution from supreme master ching hai at the " one world.
清海無上師於七點半抵達，她穿著一襲簡單優雅的白色禮服，披著白披肩，當她走在通往貴賓室的紅地毯時，理查薩迪雅克先生立即暫停和他的兒子湯姆導演及製作人，其作品有帕赤亞當大話王和瘋教授的談話，前來迎接師父，陪她走進貴賓室，並將她介紹給他的一些朋友，例如：前電視脫口秀主持人費爾唐那赫影星瑪蘿湯瑪斯費爾唐那赫的夫人導演及製作人湯姆薩迪雅克聖裘迪醫院分院長蕭夏娜葛拉梅和馬克得立比這兩位代表該院在和平之音-四海一心音樂會中接受清海無上師捐款的人士，以及其他人。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。
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