風暴的位置 的英文怎麼說

中文拼音 [fēngbàodewèizhì]
風暴的位置 英文
location of storm
  • 風 : Ⅰ名詞1 （空氣流動） wind 2 （風氣; 風俗） practice; atmosphere; custom 3 （景象） scene; view 4 ...
  • 暴 : Ⅰ形容詞1 （突然而且猛烈） sudden and violent 2 （兇狠; 殘酷） harsh and tyrannical; cruel; fierce...
  • 的 : 4次方是 The fourth power of 2 is direction
  • 位 : Ⅰ名詞1 （所在或所佔的地方） place; location 2 （職位; 地位） position; post; status 3 （特指皇帝...
  • 置 : 動詞1. （擱; 放） place; put; lay 2. （設立; 布置） set up; establish; arrange; fix up 3. （購置） buy; purchase
  • 風暴 : storm; windstorm; tempest
  1. In this distress, we had besides the terror of the storm, one of our men dyed of the calenture, and one man and the boy wash d over board ; about the 12th day the weather abating a little, the master made an observation as well as he could, and found that he was in about 11 degrees north latitude, but that he was 22 degrees of longitude difference west from cape st. augustino ; so that he found he was gotten upon the coast of guinea, or the north part of brasil, beyond the river amozones, toward that of the river oronoque, commonly call d the great river, and began to consult with me what course he should take, for the ship leaky and very much disabled, and he was going directly back to the coast of brasil

    在這危急的情況下，風暴已使我們驚恐萬狀，而這時船上一個人又患熱帶病死去，還有一個人和那個小傭人被大浪卷到海里去了。到第二十二天，風浪稍息船長盡其所能進行了觀察，發現我們的船已刮到北緯十一度左右的地方，但在聖奧古斯丁角以西二十二經度。船長發現，我們的船現在所處的位置在巴西北部或蓋亞那海岸我們已經駛過了亞馬孫河的入海口，靠近那條號稱"大河"的俄利諾科河了。
  2. The bay model complements the first by using a very fine grid to resolve those geographic features such as bays and inlets at which storm surge observations are absent and where storm surge information is required as design parameters for coastal structures such as embankments

    而港灣風暴潮模式的覆蓋范圍較小，這模式利用一套非常密集的網格點來計算出例如港灣和河口等地理位置的風暴潮資料以補開闊海岸模式的不足。
  3. Fantasia : what is the position, direction and speed of the tropical storm centre

    幻想曲：該熱帶暴風圈的中心位置、前進方向以及每小時風速為何？
  4. The diagnostic analysis for the sandstorm process on the base of height, temperature, pressure and wind etc output from the model shows that the upper cold trough, low - level wind shear, surface cold anticyclonic ridge, mesoscale cyclone and cold front are the main synoptic systems, surface cold anticyclonic ridge and cold front provide condition of wind force to occurrence of the sandstorm weather, the strong mesoscale cyclone before front makes pressure gradient before and after cold front obviously strengthen, moreover, and it increases obviously the temperature of the controlled area, as a result, the updraft movement caused by convergence before front strengthens

    500hpa強鋒區、 700hpa切變和鋒前中尺度系統的強弱及位置變化是沙塵暴天氣發生發展到減弱的直接原因。地面冷高壓、地面氣旋及冷鋒是造成本次沙塵暴天氣的主要地面天氣系統。地面冷高壓及冷鋒為沙塵暴天氣的發生提供了風力條件，而中尺度氣旋使冷鋒前後氣壓梯度明顯增強外，又使所控制的區域增溫明顯，使鋒前輻合上升運動加強，為沙塵暴天氣的發生提供了熱、動力條件。
  5. The upper part of the cargo fetched away a little when the storm hit

    在風暴襲擊的時候，貨物的上半部分有點兒移動了位置。
  6. The main relative systems of heavy - hard rainfall in northeast plateau are western pacific subtropical high, south asia high, low latitude systems, upper level jet ( ulj ), low level greater wind speed axes, westerly trough and plateau trough, low level vortex, cold frontal, occluded front in qinghai lake, mesoscale low pressure, heat low - pressure in qinghai, shear line and convergence line, mesoscale cloud cluster, etc. the west subsidiary model of south asia high is the main circulation type of heavy - hard rainfall in this area

    3 、西太平洋副高、南亞高壓、低緯系統、高空急流、低空大風速軸；西風槽和高原槽、低渦、冷鋒、青海湖錮囚鋒以及中尺度低壓、青海熱低壓、切變線與輻合線、中尺度雲團等系統是高原東北部地區大到暴雨的主要相關系統。 100hpa上的南亞高壓中心強度加強，位置東西擺動預示高原地區將有降水產生，中心強度減弱，降水過程結束。南亞高壓西部副型是高原東北部地區大到暴雨的主要流型。
  7. The northeast qinghai - xizang plateau is margin area which topographic altitude is precipitate, and which has the high frequent interaction between synoptic system in plateau and westerlies system. the heavy - hard rainfall in this area is strong outburst, lasting short time, which consists the singularity of the plateau being its especial geography position, topography and underlying surface

    青藏高原東北部地區位於高原東北側邊坡地帶，是地形高度陡然下降的地區，也是高原天氣系統與西風帶天氣系統較多發生相互作用的地區，由於特殊的地理位置、地形和下墊面條件，產生的大到暴雨天氣突發性強、時效短，具有獨特的高原特徵。
  8. Six - hourly position and intensity data of severe tropical storm bolaven 0523

    強烈熱帶風暴布拉萬0523的每六小時位置及強度
  9. Information on the nearest approach together with an estimate of the minimum central pressure of each tropical cyclone during its closest approach, the maximum winds at king s park and chek lap kok and waglan island, the minimum mean sea - level pressure recorded at the hong kong observatory and the maximum storm surge ( the excess of the actual water level over that predicted in the tide tables ) recorded at various tide stations in hong kong are included

    資料包括熱帶氣旋最接近香港時的位置及時間和當時估計熱帶氣旋中心附近的最低氣壓、京士柏及赤?角及橫瀾島錄得的最高風速、香港天文臺錄得的最低平均海平面氣壓以及香港各潮汐測量站錄得的最大風暴潮（即實際水位高出潮汐表中預計的部分） 。
  10. Information on the nearest approach together with an estimate of the minimum central pressure of each tropical cyclone during its closest approach, the maximum winds at king s park and waglan island, the minimum mean sea - level pressure recorded at the hong kong observatory and the maximum storm surge the excess, in metres, of the actual water level over that predicted in the tide tables recorded at various tide stations in hong kong are included

    資料包括熱帶氣旋最接近香港時的位置及時間和當時估計熱帶氣旋中心附近的最低氣壓京士柏及橫瀾島錄得的最高風速香港天文臺錄得的最低平均海平面氣壓以及香港各潮汐測量站錄得的最大風暴潮即實際水位高出潮汐表中預計的部分，單位為米。
  11. " it was the legislative equivalent of a perfect storm, " larocco said, " and we should thank those at the helm for their calm heads and steady hands.

    「這相當于司法領域的一場風暴。 」拉盧科說， 「我們應當感謝那些處于舵手位置上的人們所表現出來的冷靜的思維和穩健的處理手法。 」
  12. When the baroclinicity of southwest vortex had not been built and where cold front existed, the rain belt may lie in anywhere of the left of southwest low level jet

    在西南渦斜壓性未建立之前以及冷鋒附近，暴雨區可位於低層西南風急流左側的任何位置。
  13. Pilots not familiar with this alerting principle may be caught by surprise when on approaching the airport they first experience a gain event windshear of 15 kt instead of a loss event microburst of - 30 kt at the first encounter 3 mile final location only to encounter a loss of - 30 kt a couple of seconds later at 1 mile final

    他們在三海里處首次相遇位置所遇到的，並不是風速減少的情況- 30海里/小時的微下擊暴流，而是風速增加的情形+ 15海里/小時的風切變。而於數秒後到達最後進場1海里處卻遇到- 30海里/小時的風速減少情況。
  14. The idea is that the microburst or windshear alerts passed by the air traffic controllers to the pilots should include the location i. e. runway or 1, 2 or 3 nautical miles from runway threshold of the first encounter of the microburst or windshear event i. e. first encounter and the maximum value of the computed wind speed difference i. e. maximum intensity

    這準則的構思是，所有經航空交通管制員傳遞給飛機師們的微下擊暴流預警或風切變預警，均包含首次相遇微下擊暴流或風切變事件的位置即跑道或離跑道入口兩端1海里2海里或3海里的地方以及計算風速差別的最大數值即最大強度。
  15. The idea is that the microburst or windshear alerts passed by the air traffic controllers to the pilots should include the location ( i. e. runway or 1, 2 or 3 nautical miles ( nm ) from runway threshold ) of the first encounter of the microburst or windshear event ( i. e. first encounter ) and the maximum value of the computed wind speed difference ( i. e. maximum intensity )

    這準則的構思是，所有經航空交通管制員傳遞給飛機師們的微下擊暴流預警或風切變預警，均包含首次相遇微下擊暴流或風切變事件的位置即跑道或離跑道入口兩端1海里、 2海里或3海里的地方以及計算風速差別的最大數值即最大強度。
  16. Six - hourly position and intensity data of tropical storm washi 0508

    熱帶風暴天鷹0508的每六小時位置及強度
  17. Six - hourly position and intensity data of tropical storm vicente 0516

    熱帶風暴韋森特0516的每六小時位置及強度
  18. Contrasting with the results of the 3 - d numerical model output shows that the general trends of the retrieved wind stream field are completely coincided with the simulated ones. the central position of the storm is about on the same altitude and the upward as well as the downward stream are almost the same

    與數值模式輸出的結果進行對比表明不論在風暴的發展階段還是在強盛階段，反演得到的流場和模擬的流場總體趨勢完全一致，風暴的中心位置吻合的很好，兩者上升氣流和下沉氣流的分佈也很接近。
  19. The disadvantage is that small variations in coastlines such as bays and inlets cannot be resolved. the bay model complements the first by using a very fine grid to resolve those geographic features such as bays and inlets at which storm surge observations are absent and where storm surge information is required as design parameters for coastal structures such as embankments

    而港灣風暴潮模式的覆蓋范圍較小，這模式利用一套非常密集的網格點來計算出例如港灣和河口等地理位置的風暴潮資料以補開闊海岸模式的不足。當建設沿岸工程如堤壩等需要參考港灣和河口的風暴潮資料而又沒有這些紀錄時，這套模式便派上用場。
  20. As an example, under the windshear conditions depicted in the figure below where there is a windshear event of 15kt at 3 mile final and a microburst event of 30kt at 1 mile final, the consolidated windshear alert based on the first encounter, maximum intensity principle will be

    下圖例子顯示跑道進場3海里處出現了15海里小時風切變的事件，於1海里處同時出現- 30海里小時的微下擊暴流。根據"首次相遇位置最大強度"的準則，風切變預警應為：
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