梅向明 的英文怎麼說
中文拼音 [méixiàngmíng]
梅向明
英文
mei xiangming-
" one branch of it, " according to the historian of concord, for i love to quote so good authority, " rises in the south part of hopkinton, and another from a pond and a large cedar - swamp in westborough, " and flowing between hopkinton and southborough, through framingham, and between sudbury and wayland, where it is sometimes called sudbury river, it enters concord at the south part of the town, and after receiving the north or assabeth river, which has its source a little farther to the north and west, goes out at the northeast angle, and flowing between bedford and carlisle, and through billerica, empties into the merrimack at lowell
「它的一條支流」 ，據研究康科德河的歷史學家說（我喜歡引用權威） ， 「發源自霍普金頓的南部，另一條支流來自西區的一個池塘和一大片雪松沼澤， 」它們從霍普金頓和南區的中間流過，途經弗萊明翰，然後穿過薩德伯里和韋蘭（在這一段它有時被稱為薩德伯里河） ，從南部進入康科德鎮，在與發源自較遙遠的北面和西面的阿薩貝斯河交匯后，從東北方向流出，然後從貝德福德與卡萊爾中間穿過，流經比勒瑞卡，最終匯入洛厄爾的梅里馬克河。The results showed that the trophic lenel of lake taihu was in the transition state, from meso - eutrophic to eutrophic, of which the meso - eutrophic made up about 70 % of the total are. the eutrophic and hyper - eutrophic waters accounted for 10 % or so
結果表明，太湖營養水平處于中富向富營養過渡狀態，中富面積約佔全湖面積的70 %以上；夏季富營養及重富營養水域出現在北部湖區的梅梁湖、五里湖和西部沿岸，約佔全湖面積的10 % 。To the large - scale atmosphere, we separate the terms of the horizontal vorticity converting into the vertical vorticity, which considered as the baroclinic terms, from the terms that not including horizontal vorticity by the rules of the p coordinate transforming to the z coordinate in the traditional vorticity equation, and carry out the scale analysis, and then conclude that the baroclinic terms are able to reach the same magnitude grade as the partial derivative of the vertical vorticity to time when it takes place the large scale precipitation in the summer monsoon period in china. by analyzing the game reanalysis data from april to august in 1998 in the region of chinese continent, we found that the baroclinic terms is important to the large - scale cyclone developing above the 600hpa, and the magnitude changing of the baroclinic terms is nearly in - phase as the monsoon movement, so which imply exactly that the magnitude changing of the baroclinic terms is the one of the natural characters of the summer monsoon evolution and equivalent to the movement rule of the subtropical high of the western pacific
在p坐標垂直渦度方程中，利用p坐標向z坐標轉換的公式將水平渦度向垂直渦度轉化的所有項分離出來，這些項具有明顯的斜壓特徵，對其進行尺度分析后，得出在可以忽略潛熱釋放對渦度影響的對流層中、高層，此轉化項是大尺度斜壓渦度發展的重要項。通過對1998年48月的game再分析資料進行實際計算也發現，轉化項在東亞夏季風上升支的600hpa及以上層次對垂直渦度的局地變化貢獻很大，不能忽略。同時發現水平渦度向垂直渦度的轉化在南海季風爆發時和江淮梅雨入梅及發展過程中均有指示性意義，在南海季風爆發以後，在中國東南部地區，轉化項的大小與夏季風的活躍和中斷等活動有著幾乎一致的變化規律，這從側面也指出了，此轉化項的變化是夏季風演變所具有的本質特徵，並且它反映出了西太平洋副高在中國大陸的活動情況。President mei yi - qi and tsinghua university was inseparable, because tsinghua made mei yi - qi famous and mei guided tsinghua to be bright and brilliant
摘要梅貽琦校長和清華大學密不可分，清華培養了梅貽琦，梅校長引導清華走向光明和輝煌。The results show that there are two centers of occurrence of llsw respectively in dong bei and jiang nan ; the regional torrential rain over the yangtze river basin is closely associated with llsw during the major periods of heavy rainfall ; the diurnal variation of the number of occurrence in the middle and low reaches of the yangtze river is the strongest in china there are some significant differences between llj and nallsw in positive season, spatial variation, diurnal variation and field of pressure. by the way, the important effect of inertial stability on heavy rainfall with both low level south - westerly jet and high level northerly strong flow is analyzed theoretically. the results show that the existence of the maximum of inertial stability in the left font of the low level jet is favor of the accumulation of the moist thermal energy, and conditional symmetric instability or convective instability can be expected in this region
另外，慣性穩定性的作用以往不受重視，本文通過對西南低空急流左前方和高空偏北大風軸右後方的慣性穩定性和對稱穩定性的理論分析和實例計算，表明慣性穩定性在伴有高低空急流的暴雨中有重要意義，揭示了梅雨暴雨的一種新的高低空急流耦合機制：低空急流左前方慣性穩定度大值區的存在，有利於低層濕熱能量的積累，使低層傾斜對流的不穩定發展更多期望于條件性對稱不穩定或對流不穩定；高空偏北大風軸（西風急流）的存在，是其右後方（右側）出現對稱不穩定的有利條件，高空相對容易出現干對稱不穩定；慣性穩定性的作用，使低層的傾斜對流更偏向於垂直方向，有利於對流發展，使高層的傾斜對流更偏向於水平方向，有利於高層輻散。Regional difference in lower - level temperature dv and pressure dv are greatly weakened and dv of llj is distinctly faint without the nanling ridge. this result show that nanling ridge acts as a critical role in the establishment of dv of the lower - level temperature and pressure, which give rise to the dv of llj in south china
而當模式中僅僅去掉南嶺和武夷山山脈地形后，低層大氣溫度場日變化的區域性差異明顯變弱，梅雨低壓帶南側原南嶺山脈所在地的溫度日較差明顯減小，使得梅雨低壓槽與華南地區之間的南北向水平溫度梯度和水平氣壓梯度的日較差顯著變小，導致華南低空急流日變化的顯著減弱。What is beyond dispute is that mr krugman is the finest economist to become a media superstar - at least since milton friedman or, earlier, john maynard keynes turned to journalism
毫無疑問，至少從米爾頓-弗里德曼，或者更早一些的約翰-梅納德-凱恩斯轉向新聞業以來，克魯格曼先生媒體超級明星中最出色的經濟學家。4 ) during the meiyu, the precipitation in middle and lower reaches of yangtze river has the relationship with southern hemisphere circulation in early april and may. when the meridional circulation in middle and high latitude of south pacific in april and may is rather obvious and the south pole eddy is rather strong, the precipitation in middle and lower reaches of yangtze river may be bigger than ever
4 ）梅雨期長江中下游降水多寡與前期4 、 5月南半球環流存在聯系，當4 、 5月南太平洋中高緯度地區經向環流較為明顯，南極渦偏強時，長江中下游地區梅雨期降水易偏多；反之，當4 、 5月南太平洋中高緯度地區緯向氣流較為明顯，高緯度西風較弱，南極渦偏弱時，長江中下游地區梅雨期降水易偏少。It was a typical mei - yu front on the middle and upper level of the troposphere which became wider with the height increased. the temperature field of mei - yu front area looked like " sandwich " with the warmer air along the each side of the colder air of mei - yu area
在水平方向，梅雨鋒區的溫度場在對流層中低層呈現「暖-冷-暖」的「三明治」結構，即梅雨鋒區溫度最低，而在其兩側溫度最高。分享友人