northwest by west 中文意思是什麼
northwest by west
解釋
北西偏西-
The prairie, across which the sledge was moving in a straight line, was as flat as a sea. it seemed like a vast frozen lake. the railroad which ran through this section ascended from the south - west to the northwest by great island, columbus, an important nebraska town, schuyler and fremont, to omaha
平原象是一個遼闊無邊的結冰池塘，在這個地區這一條由西南向西北延伸的鐵路，經過大島和內布拉斯加州的重鎮哥侖布斯，再經過休列爾弗列蒙，最後到達奧馬哈。 -
( 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。 -
Free trade zone is 31 km away from, in the south, tsimshatsui, kowloon of hong kong, 30 km from kuiyong dock, in the east 10 km from luohu railway station, shenzhen, 30 km from yantian port : in the west 25 km from mawan. shekou port. tn ttie northwest it is 3o km away fom huangtian airport, shenzhen, and there is a special path by guang - shen highway connecting with it
保稅區南至香港九尖沙咀31公里，葵涌貨櫃碼頭30公里，東至深圳羅湖火車站10公里，至鹽田港30公里，西至媽灣蛇口港公里，西北至深圳黃田機場30公里，並經廣深高速公路設有專用通道與之相連，保稅區建有封閉的一號專用通道與香港直接相連。 -
A few other watercourses have had their monitoring interrupted at various points in their history. the kt1 monitoring station on the kam tin river was suspended temporarily in 1997 and 1998 while river training work was being carried out in the vicinity, resuming in 1999 once the station again became accessible. the tsang kok stream in the northwest was also affected by the west new territories landfill development, being suspended in 1999 but resuming from 2000
此外，有些時期河溪的監測活動亦曾經中斷過，例如1997年及1998年間，設于錦田河的kt1站位的監測因為附近進行河道改善工程而暫時停止，直至1999年才恢復運作新界西北部的曾角溪亦於1999年受新界西堆填區發展工程影響，水質監測暫停至2000年才重新恢復運作。 -
It proposed two development stratagem by swot matrix analysis : implement market penetration strategy, expanding the market share of west china, exploiting the market in the northwest and north of china to realize the new increasing target for corporation ’ s economic benefit
根據西南電力設計院的經營思想和經營目標，依據swot矩陣匹配分析提出了二個主要市場發展戰略: （ 1 ）實施市場滲透戰略，利用區位優勢迅速而且極大地擴大「西電東送」項目中的市場份額，以保持和擴大經濟效益。 -
In this paper, decadal variability of tropic and north pacific ' s ssta and of precipitation in china, correlations between them and the possible mechanisms of the ssta decadal change compacting on the precipitation decadal change are analyzed by using ncep globe temperature, wind and height data ( 1948 - 2001 ), coads ssta data ( 1900 - 2001 ) and 147 stations " precipitation data in china. results show that : ( 1 ) mid - high latitude north pacific and tropic west pacific ssta have obvious decadal change, the prior ' s decadal change has great variance and the latter ' s has great contribution in total variance, the main eigenvectors " distribution are stable in eof of tropic and north pacific ssta ' s decadal variability, the key area of the first eigenvector allots in two sides of tropic pacific ; the second one ' s allots in mid - high latitude northwest pacific and low latitude mid - east pacific which vary contrary ; the third one ' s allots in middle north pacific
本文利用ncep資料（ 1948 - 2001年）中的全球表面溫度場、風場、高度場資料， coads （ 1900 - 2001年）海表面溫度距平資料及中國147個站點1951 - 2001年共51年的降水資料，探討了熱帶及北太平洋ssta 、中國降水的年代際變化特徵，夏季熱帶及北太平洋ssta年代際變化與中國夏季降水年代際變化的耦合相互關系以及夏季熱帶及北太平洋ssta年代際變化影響中國夏季降水年代際變化的可能機制，結果表明： （ 1 ）北太平洋中高緯與熱帶西太平洋均有明顯的年代際變化，北太平洋中高緯年代際變化方差顯著，而熱帶西太平洋年代際變化方差貢獻顯著。 -
Tainan city is 10 kilometers northwest of the district and kueijen township office is about 5 kilometers to the north of the district. surrounding the hsr tainan station, the north border of the special district is about 200 meters from the guanmiao expressway and the east border is 760 meters from the farms of taisugar company. the district is bordered on the south by no. 15 cemetery of kueijen township and the west border is 100 meters to the west of county highway no. 149
本特定區以高鐵臺南車站為中心，計畫范圍界線北以臺南關廟線東西向快速道路南緣約200公尺為界，東至高鐵臺南車站中心點東側約760公尺處之現有臺糖農地為界，南至歸仁鄉第十五公墓附近為界，西至南149號縣道西側約100公尺為界，計畫面積299公頃。 -
The positive load take absolutely advantage in the first spatial pattern of year and seasons. especially that the precipitation field load of winter is all positive. not in the southwest of china because of southwest monsoon etc. system ; the characteristics of the second spatial pattern are that most of the area is taken up by positive load in year and four seasons, the west of talimu basin is the center of negative load of the year, spring and autumn vector fields ; east of zhungeer basin is the center of positive load of the third spatial pattern of year, spring, summer and winter, the center of negative load is often in east of chaidamu basin, but the distribution center of autumn is in east of zhungeer basin ; the distribution of the fourth spatial pattern is difficult to describe and forms several centers of positive and negative load ; several centers of positive and negative load also appear, the distribution of load fields of the fifth spatial pattern of year, spring and winter represents the situation of " +, -, + " from southeast to northwest ; the complexity of the sixth spatial pattern is more stonger than that of the fourth and the fifth spatial pattern, several centers of load fields of year and each season often appears inverse situation of the positive and the negative load. but the centers are still most in zhungeer basin, chaidamu basin and talimu basin
第一空間型中，年和四季都是正荷載占據絕對優勢，特別是冬季降水場皆為正值，只是西南地區由於受西南季風等系統的影響，表現為與其它地區的不同；第二空間型的特點如下：年和四季分佈皆為正荷載占據大部分區域，負荷載中心年、春季和秋季分佈中都是位於塔里木盆地西部地區；第三空間型正荷載高值中心除秋季外都是處在準格爾盆地以東地區，負荷載中心多在柴達木盆地以東地區，秋季卻處于準格爾盆地以東地區；第四空間型分佈就較復雜無章法可言，形成多處正負荷載中心；第五空間型特徵是這樣的，同樣是多個荷載中心出現，年、春季和冬季中的荷載場分佈從東南到西北大體呈現「 + 、 - 、 + 」的特點；第六空間型分佈的復雜程度較之第四、第五空間型更大，年和各季分佈比較中多個荷載中心常出現正負相反的情況，但中心仍以柴達木盆地、準格爾盆地和塔里木盆地為主。 -
It is concluded that : the enrichment of main ore - forming elements in northwest and west tianshan mountains represents the character of gold mineralization ; east tianshan mountain represents the mineral pattern of au, cu, ( ni ), and ag ; the north tianshan mountain is dominated by the ore - forming character of gold
得出西南天山、西天山元素富集特徵反映了以金為主的礦化特徵；東天山反映以金、銅（鎳） 、銀多金屬為主的礦產格架，北山是以金為主礦化特徵。
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