northeast by east 中文意思是什麼
northeast by east
解釋
東北偏東方向-
( 4 ) in summer, tropic west pacific ssta decadal change infect precipitation decadal change in south and north of changjiang river maybe by : positive ssta in tropic west pacific weaken the summer monsoon circulation, lead more precipitation in south of changjiang river and less precipitation in north of it, vice versa ; middle north pacific ssta decadal change infect precipitation decadal change in mid - down valley of changjiang river maybe by : when ssta is negative in middle north pacific, the height field in tropic rises obviously, the subtropical high strengthens and extends westward, the northern limit retreats southward, leads upper trough retreats northward and move eastward, meiyu front moves northward, then leads more precipitation in mid - down valley of changjiang river, vice versa ; middle northwest pacific - low latitude mid - east pacific infects precipitation in north china possibly by change the activity of northeast china cyclone
（ 4 ）熱帶西太平洋ssta年代際變化影響夏季中國長江南北降水年代際變化的可能機制是熱帶西太平洋海表溫度正（負）異常減弱（加強）東亞夏季風環流，從而使江南降水增加（減少） ，江北降水減少（增加） ；夏季中部北太平洋ssta年代際變化影響中國長江中下游地區夏季降水年代際變化的可能機制是中部北太平洋海表溫度負異常，將導致熱帶地區高度場普遍增高，副高加強西伸，副高北界南退，致使高空槽北縮東移，梅雨鋒西移北進，中國長江游中游、中卜游降水增多，反之亦反；夏季中高緯西北太平洋一低緯中東太平洋反向距平分佈結構影響中國東北降水的可能機制是低緯中東太平洋海表溫為負異常。 -
The direction of migration was in east and northeast. ( 3 ) this paper introduced the balanced section into the early reservoir description in the sidaogou structure for the first time, and gave a new viewpoint that the sidaogou structure was a fault - bend fold formed by two step thrust fault. the structural stress direction came from the northeast of the hami depression
首次將平衡剖面技術引入了四道溝構造早期油藏描述的構造研究之中，並首次提出四道溝構造是?至少由兩個階梯狀斷層組成的后傾雙重構造疊加的斷層轉折褶皺，構造應力方向應大致源於北東方向。 -
Detailed diagnoses is made on a heavy - hard rain in the northeast qinghai - xizang plateau using ncep data of 1 x 1 with 6h intervals, more complete and integrated conventional observational data and the data set of automatic meteorological stations in plateau and new generation doppler radar data and satellite images and etc. the following conclusions can be drawn : 1. the distribution of heavy - hard rain, which is characteristics of valley topography in northeast qinghai - xizang plateau is obviously effected by topography. the distribution of yearly mean precipitation and the frequencies of heavy - hard rain in this area are descending from east to west
本文首先利用ncep時間間隔為6小時的1 1的格點資料、更全面、更為完整的常規探測資料和高原地區布設的自動氣象站資料、新一代多卜勒天氣雷達資料、衛星雲圖資料等對高原東北部地區大到暴雨的天氣、氣候特徵及大尺度環流背景進行分析，形成對高原暴雨的整體認識，並為以後的數值模擬提供大尺度環流背景及依據，分析中發現： 1 、高原東北部地區大到暴雨的分佈明顯受到地形影響，年降水量和大到暴雨次數自東向西呈階梯性遞減趨勢，分別在高原東北部的外流河谷地區和四川北部地區存在大值中心。 -
Six sound mountainous region area is located within the boundaries of the hebei province qinhuangdao lulong shimen town, is located northeast our country huabei pingyuan the beijing and tianjin tang qin economy to move in a circle the area, east is near bohai sea, west depends on luanhe river, north the pillow mt. yanshan - odd arteries, south depend on 205 federal highways and the jingshan railroad parallel transportation skeleton line ; by a series of lianshan, the rivers, the village are composed, about area approximately 8 square kilometers
六音山地區位於河北省秦皇島市盧龍縣石門鎮境內，位於我國華北平原東北部京津唐秦經濟環行地區，東臨渤海，西依灤河，北枕燕山余脈，南靠205國道與京山鐵路并行交通干線；由一系列連山、河流、村落組成，面積約8平方公里左右！ -
The district is bounded by wo yi hop road and texaco road to the east. its western end extends to tsing lung tau, while the northern part covers the hilly areas of tai mo shan. its coastline provides a natural boundary to the south, but ma wan island and northeast lantau are also part of the tsuen wan district
荃灣東面以和宜合道及德士古道為界，西端伸展至青龍頭，北部則包括大帽山的山嶺，南面以海岸線為界，而馬灣和大嶼山東北部也屬荃灣區的范圍。 -
Particularly, it focuses on the differentiation of two geographical terms ? the northeast asia region and the east sea ( japan sea ) rim region, the illustration of the necessity of the economic cooperation among local regions within the east sea ( japan sea ) rim region, and several patterns of the economic cooperation proposed by chinese, japan and south korean scholars and experts. in the second part, the thesis makes a systematic and thorough analysis on the background, current situation and characteristics of the economic communication and cooperation in the east sea ( japan sea ) rim region, and also comments on the present progresses and existing problems
同時，介紹了環東海（日本海）地區的經濟合作模式，另外，還分析了環東海（日本海）地區經濟合作的現狀、特點及產生的效果等相關問題，並以環東海（日本海）地區的中國吉林省、俄羅斯濱海邊疆區、韓國江原道為重點提出了一些合作設想，主張在這三個地區間率先建立起經濟合作共同體，以此進一步帶動整個東北亞地區的經濟合作。 -
Paper is divided into nine chapters by each chapter mainly as follows : chapter is about regional economic development and government management in the era of the planned economy. this chapter from the perspective of history, introduced economic development of the north - east region from dynasty to former nation - building, and systematically elaborated on the central government, local governments and governmental agencies for the northeast region and history in the era of the planned economy
中篇，從比較的角度，分析了上個世紀80年代以來以英國為首的西方國家進行政府管理新變革的經驗、世界幾個發達國家在老工業基地改造中政府的管理經驗和我國部分地區進行政府管理創新的經驗，從中為東北老工業基地政府管理創新提供有益的啟示。 -
By using multi - channel observations of olr, hirs - tb12, erb, vis, ssmr and ssm i on the us satellites, it is analyzed that the global general atmospheric circulation features related to the anomaly of cold vortex over northeast china and it s premonitors are also revealed. it is found that there is an effected chain, which consists of sea ice over northern hemisphere, sea surface temperature in the mid - east equatorial pacific, asia monsoon and local budget of earth radiation in northeast china, on the anomaly of northeast cold vortex. the impacts of each factor in the chain are discussed. the results indicate that the applications of multi - channel satellite observations on research of climate change are of significance
利用美國氣象衛星olr ， hirs - tb12 ， erb ， vis ， ssmr和ssm i多通道的觀測資料，分析了東北冷渦異常年的全球大氣環流特徵及其關鍵地區的先兆特徵對于東北冷渦異常，發現了有一個由北半球的海冰，赤道東太平洋的海溫，亞洲的季風以及東北地區地氣系統輻射收支組成的影響鏈存在。由此討論了影響鏈上的各因子對東北冷渦異常的作用。結果表明多通道衛星觀測資料的綜合應用在氣候變化的研究和預測中有著重要的意義。
分享友人