sea land wind 中文意思是什麼

sea land wind 解釋
海-岸風
  • sea : SEA ＝ Southeast Asia 東南亞。n 1 海；海洋；內海；大（淡水）湖。2 〈pl 或與不定冠詞連用〉海面（狀...
  • land : n 1 陸地，地面。2 土地，田地；農田；〈pl 〉所有地，地產。3 國土，國，國家；領土；地方；（…的）世...
  • wind : n 1 風；大風，暴風；氣流；【機械工程】壓縮空氣。2 【航海】上風；風向；〈古語〉〈pl 〉方向。3 氣息...
  1. But as soon as it grew dusk in the evening, i chang d my course, and steer d directly south and by east, bending my course a little toward the east, that i might keep in with the shoar ; and having a fair fresh gale of wind, and a smooth quiet sea, i made such sail that i believe by the next day at three a clock in the afternoon, when i first made the land, i could not be less than 150 miles south of sallee ; quite beyond the emperor of morocco s dominions, or indeed of any other king thereabouts, for we saw no people

    這時風勢極好，海面也平靜，我就張滿帆讓船疾駛。以當時船行速度來看，我估計第二天下午三點鐘就能靠岸。那時我已經在薩累以南一百五十英里之外了，遠離摩洛哥皇帝的領土，也不在任何國王的領地之內，因為那兒我們根本就看不到人跡。
  2. What little wind there was blew me towards the land ; and thus, having found two or three broken oars belonging to the boat, and besides the tools which were in the chest, i found two saws, an axe, and a hammer, and with this cargo i put to sea ; for a mile, or thereabouts, my raft went very well, only that i found it drive a little distant from the place where i had landed before, by which i perceiv d that there was some indraft of the water, and consequently i hop d to find some creek or river there, which i might make use of as a port to get to land with my cargo

    至今我還不知自己身處何地，在大陸上呢，還是在小島上，有人煙的地方呢，還是沒有人煙的地方，有野獸呢，還是沒有野獸。離我不到一英里的地方，有一座小山，高高聳立於北面的山丘之上，看來那是一道山脈。我拿了一支鳥槍一支手槍和一角筒火藥，向那座山的山頂走去。
  3. Hong kong ' s vehicles and coal - burning power plants also generate a fair share of pollution within the city, which is then exacerbated by local wind patterns and what is known as " land - sea breeze circulation "

    汽車和火力發電廠產生的污染，也在香港的污染中占據了相當比例，而被稱為「陸海風循環」的當地刮風模式更加劇了這種污染。
  4. ( 5 ) the spring greenland sea - ice extent is larger ( smaller ) : then during the following summer the high of the japanese sea is stronger ( weaker ), and the low of the asian land is stronger ( weaker ), which make the pattern of low west and high east easily ( uneasily ) form ; the ascending movement over north china is strengthened ( weakened ) ; the summer monsoon of east asia is stronger ( weaker ), then the southeastern, warm and damp airflow towards the north china is stronger ( weaker ), and the cold airflow of the high level over the north china is also stronger ( weaker ), which make the convergence of the cold and warm air over north china easily ( uneasily ) form ; the sst of the east pacific ocean is lower ( higher ), while the sst of west wind drift is higher ( lower )

    （ 5 ）春季格陵蘭海冰面積偏大（小） ：後期夏季日本海高壓偏強（弱） ，而大陸上低壓也偏強（弱） ，易（不易）形成西低東阻的形勢；華北地區的上升運動增強（減弱） ；東亞夏季風偏強（弱） ，向華北地區輸送的西南暖濕氣流偏強（弱） ，而對應高空華北地區上空冷空氣活動偏強（弱） ，利於（不利於）華北上空冷暖空氣的交匯；夏季赤道東太平洋海溫偏低（高） ，西風漂流區海溫偏高（低） 。在以上的環流背景下，華北夏季降水偏多（少） ，易澇（旱） 。
  5. There was a time when our people covered the land as the waves of a wind - ruffled sea cover its shell paved floor, but that time long since passed away with the greatness of tribes that are now but a mournful memory

    我們的人民曾一度像大風攪亂的大海覆蓋著布滿貝殼的海床一樣覆蓋著這片土地，但是，那時代早已同龐大的部落一道成為過去，而那些部落現在只不過是一樁令人憂傷的回憶。
  6. Monsoons are large - scale wind systems caused by differences in the temperatures of land and sea over the seasons

    隨著季節演變，陸地和海洋出現溫度差距，因而形成的大尺度風系統，就是季候風。
  7. This paper discuss the effect of roughness coefficient on the tropical cyclone landfalling process using a idealized tc model developed from psu / ncar mm5 in the condition of quiescence and f - plane atmosphere. in order to understand the different influences of land and sea surfaces in the tc landfalling process, two kind of experiments had been designed : one for settled tc, the other for movable tc, and each kind consists four tests. the result indicates that the distribution of wind, precipitation, warm core and intensity of tropical cyclone has been changed obviously due to the effect of difference between the land and sea

    本文利用bogus技術在psu / ncarmm5中加入了理想熱帶氣旋初始渦旋，在f -平面和無環境流場的理想情況下，設計了兩組靜態和動態試驗，通過控制試驗和不同粗糙度的登陸試驗，分別從空間和時間上探討了理想熱帶氣旋的登陸規律和分佈特徵，特別研究了邊界層中熱帶氣旋中心區域風場的垂直細致結構，並初步分析了其物理機制。
  8. In this distress, the wind still blowing very hard, one of our men early in the morning, cry d out, land ; and we had no sooner run out of the cabbin to look out in hopes of seeing where abouts in the world we were ; but the ship struck upon a sand, and in a moment her motion being so stopp d, the sea broke over her in such a manner, that we expected we should all have perish d immediately, and we were immediately driven into our close quarters to shelter us the very foam and sprye of the sea

    我們知道，我們的船已支持不了幾分鐘了，隨時都可能被撞成碎片，除非出現奇跡，風勢會突然停息。總之，我們大家坐在一起，面面相覷，時刻等待著死亡的來臨，準備去另一個世界，因為，在這個世界上，我們已無能為力了。這時，船沒有像我們所擔心的那樣被撞得粉碎，同時風勢也漸漸減弱，使我們稍感安慰。
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