正南偏東 的英文怎麼說

中文拼音 [zhēngnánpiāndōng]
正南偏東 英文
south by east
  • 正 : 正名詞（正月） the first month of the lunar year; the first moon
  • 偏 : Ⅰ形容詞1 （不正; 歪斜） inclined to one side; slanting; leaning 2 （只側重一面） partial; prejudi...
  • 正南 : herman
  1. The island lies south by east from here

    那個島位於此地的正南偏東方向。
  2. The doppler radial winds from the terminal doppler weather radar tdwr 0. 6 - degree elevation scan over the hkia and its western approach were generally away from the radar positive radial velocity - warm colours, consistent with the low - level east - southeasterly flow figure 12

    機場多普勒天氣雷達對香港國際機場及西面著陸區的0 . 6度仰角掃描顯示，多普勒徑向風大致離開雷達正徑向風速暖色，與低空東南偏東氣流吻合圖12 。
  3. Mountain wave cloud also known as lenticular cloud, i. e. lens shaped was observed on the hilltop of lantau on 12 august 2003. the picture was taken at around 2 : 20 p. m. that afternoon at the hong kong international airport looking south - southeast towards lantau with a setting of 1 160s, f8. 0 and iso - 100 speed. at the time winds were light to moderate southerly, with showers just passing over lantau an hour earlier

    相片顯示大嶼山的山頂正蓋著一層波狀雲也稱為莢狀雲，因其形狀如豆莢照片是在二零零三年八月十二日下午二時二十分左右拍攝，地點在香港國際機場朝著東南偏東的方向，用度菲林快門為1 160秒和光圈f8 . 0 。
  4. North by east

    正南偏東
  5. Analysis shows that when summer precipitation in north china is richer ( less ), tropical east pacific ssta is colder ( warmer ) phase, and slp and 500hpa geo - potential height are negative ( positive ) anomaly over the asia, west pacific sub - high is northerner ( southerner ), and block high in mid - highs latitude happens less ( more ) than normal, east monsoon is stronger ( weaker )

    分析表明華北夏季多（少）雨期，赤道中東太平洋ssta處于冷（暖）位相，在非洲大陸上slp利500hpa位勢高度均為負（正）異常，西北太平洋副高位置偏北（南） ，中緯度阻塞高壓發生頻率較低（高） ，東亞夏季風偏強（弱） 。
  6. The weather pattern that day see the weather chart was characterized by a ridge of high pressure ahead of a cold front over south china

    當日華南地區正受一道冷鋒前緣的高壓脊所支配見天氣圖，地面吹偏東風，而大嶼山山頂則吹南風。
  7. The weather pattern that day ( see the weather chart ) was characterized by a ridge of high pressure ahead of a cold front over south china

    當日華南地區正受一道冷鋒前緣的高壓脊所支配（見天氣圖） ，地面吹偏東風，而大嶼山山頂則吹南風。
  8. The body pointed straight in the direction of the island, and the compass read duly e. s. e

    屍體正指向骷髏島那一邊，羅盤標明的方位正是東南東偏東。
  9. 2. the precipitation character of the north part of viet nam and its relation to the atmospheric circle. there is a clear relation between summer rainfall in north part of vietnam and pre - spring 100hpa gee - potential height field, the key region is north part of the north pacific ; there is also an obvious relation between summer rainfall and pre - spring 500hpa geo - potential height field, the key regions is north part of the north pacific, greenland and south part of the south pacific

    另外越南北部夏季降水與同期500百帕位勢高度場關系不明顯，表現為：只有南太平洋南部可以認為是與越南夏季降水關系密切的地區，另外在東西伯利亞地區也可認為與越南同期降水有明顯關系的地區，即： 500百帕高度場上的上述兩個區域位勢高度正異常，同期越南北部夏季降水可能偏多，反之亦然。
  10. The comparison showed that the difference between two data is less 0. 5cm in chinese main land area, and the same time we found that modis atmospheric precipitable water vapor is greater than the ncep data in the area of northwest and north of china and less it in the area of southeast of china. if we multiply modis atmospheric precipitable water vapor data with 0. 933983 and 1. 07686 respectively on above area the difference will below to 0. 2cm

    結果發現：在中國大陸地區， modis與ncep的大氣可降水量之差在絕大部分地區在0 . 5cm以內，但是在中國西北、華北地區普遍偏大一些，在東南地區則普遍偏小一些，如果給上述地區的modis大氣可降水量分別乘以0 . 933983和1 . 07686進行修正，則兩者之差在0 . 2cm以內。
  11. There was no wind stirring to help me, and all i could do with my paddlers signify d nothing, and now i began to give my self over for lost ; for as the current was on both sides the island, i knew in a few leagues distance they must joyn again, and then i was irrecoverably gone ; nor did i see any possibility of avoiding it ; so that i had no prospect before me but of perishing ; not by the sea, for that was calm enough, but of starving for hunger

    我在這兒把船停了兩天，因為那兩天一直刮東南風，風向偏東，而且風也不校風向正好與我上面提到的那股急流的方向相反，因而在岬角附近的海面波濤洶涌。在這種情況下，如果我靠近海岸航行，就會碰到大浪，如果我遠離海岸航行，又會碰到急流，所以怎麼走都不安全。
  12. The precipitation character of the middle part of viet nam and its relation to the atmospheric circle. the autumn precipitation of the middle part of viet nam has obvious variations in inter - annual and inter - decade scale with clearly quasi 6a, 10a, 15a period ; in heavy rainfall years, there are a positive anomaly over the north - west pacific and a negative anomaly over japan ; while in deficient rainfall years, the anomaly distribution is on the contrary ; 4. the precipitation character of the south part of viet nam and its relation to the atmospheric circle. the research finds that the rainfall of the south part of vietnam usually concentrates in the autumn every year and a clear difference of atmosphere condition exists between that of flood and drought years

    越南中部降水變化特徵及其與大氣環流和海溫的關系越南中部秋季降水具有明顯的年際、年代際變化特徵，具有明顯的準6a 、 10a 、 15a左右的周期；越南中部多雨年， 500hpa高度距平場在熱帶西北太平洋為正距平，日本附近上空為負距平；而少雨年則相反；越南中部多雨年，熱帶中東太平洋海溫異常偏高，西太平洋海溫異常偏低；少雨年則相反；越南中部多雨年，登陸越南的臺風頻數偏多；而少雨年則相反。
  13. The doppler radial winds from the terminal doppler weather radar ( tdwr ) 0. 6 - degree elevation scan over the hkia and its western approach were generally away from the radar ( positive radial velocity - - warm colours ), consistent with the low - level east - southeasterly flow ( figure 12 )

    機場多普勒天氣雷達對香港國際機場及西面著陸區的0 . 6度仰角掃描顯示，多普勒徑向風大致離開雷達（正徑向風速暖色） ，與低空東南偏東氣流吻合（圖12 ） 。
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