風向後移 的英文怎麼說

中文拼音 [fēngxiànghòuyí]
風向後移 英文
veer aft
  • 風 : Ⅰ名詞1 （空氣流動） wind 2 （風氣; 風俗） practice; atmosphere; custom 3 （景象） scene; view 4 ...
  • 移 : Ⅰ動詞1. （移動） move; remove; shift 2. （改變; 變動） change; alter Ⅱ名詞（姓氏） a surname
  • 風向 : wind direction
  1. Mackerel sky, not twenty - four hours dry describes the deterioration of weather after the appearance of cirrocumulus clouds. although it may be bright at the beginning, the weather will deteriorate in half a day s time as the cyclone or front approaches. as they pick up more moisture, the cirrocumulus clouds thicken and extend downward to become low - level clouds which bear rain

    魚鱗天，不雨也風顛是形容卷積雲出現後天氣轉壞的狀況，雖然初時天氣明朗，但約半天光景后，天氣會隨氣旋或鋒面的移近而轉壞，風速增強，卷積雲也會隨著水氣增加而逐漸增厚，雲層向下伸延轉為低層雲，產生降雨。
  2. Hagibis then slowed down and turned north. it attained typhoon intensity on 18 may

    其後它減速及轉向北移，於五月十八日達至臺風強度。
  3. Rammasun weakened into a severe tropical storm on 5 july and changed its course to the northeast

    七月五日，威馬遜減弱為一個強烈熱帶風暴，然後改向東北移動。
  4. Our factory increase a set of intensifier with non - grade - adjustable rating speed to form the intensive air drying, the wet material mixed with hot air fully by screw feeder in the intensifier and material surface is crashed into fine granules and moving to the outlet as well as drying, under rapid rotating hitting and pushing. in the long run, the materials get a further even drying in the dryer pulled by the wind force and those wet and weighty granules the wind force can not pull continue to be crashed, dried until they are pulled by the wind force into the dryer

    我廠強化型氣流乾燥是在基本型上增加一套轉速可以無級調節的強化器組成，濕物料通過螺旋加料器進入強化器后和熱氣流充分混合，在飛速旋轉的擊刀擊碎和推進下，物料被破碎成細顆粒，在乾燥同時向出口移動，最後在風力吸引下進入乾燥管，進一步均勻乾燥，風力無法吸引的濕重顆粒繼續被擊碎、乾燥、直至能被風吸起進入乾燥管。
  5. One day later, it turned to the northwest. on 5 november, huko weakened into a severe tropical storm and headed north

    胡高初時向西北偏西移動，一日後轉向西北，於十一月五日減弱為一個強烈熱帶風暴后再轉向北移。
  6. Bavi then headed north - northwest and intensified into a severe tropical storm on 11 october. it turned to the north one day later

    其後它改向西北偏北移動，於十月十一日增強為一個強烈熱帶風暴，一日後再轉向北移。
  7. These disturbances are believed to be generated as a result of deflection of the airflow by the ridges of lantau island, bringing about significant windshear as they moved towards the approach and departure corridors. with the turning of winds at hkia to southerly, the signature of windshear over the airport became more prominent

    此時，雷達探測到大嶼山山脈的下游有細小的擾動出現並移向升降區，相信這些擾動是氣流繞過大嶼山山脊后轉向而產生的，這些擾動為跑道升降區帶來顯著的風切變。其後香港國際機場轉吹偏南風，風切變影響機場的情形更為明顯。
  8. It intensified rapidly into a typhoon on 15 july, and maintained a northwest movement in the next ten days. fengshen was an intense typhoon with maximum winds estimated to be over 200 kmh

    它在往後十天維持向西北方移動。風神是一個強勁的臺風，估計其中心風力為每小時200公里以上。
  9. It attained typhoon strength on 31 august and moved to the west in the next few days. it moved across okinawa on the night of 4 september and then slowed down over the east china sea in the next two days. sinlaku speeded up on 7 september and headed towards zhejiang

    森垃克在八月三十日增強為一個強烈熱帶風暴及改向西北移動，於八月三十一日進一步增強為一個臺風，並在隨后數日以偏西方向移動。森垃克在九月四日晚上橫過沖繩島，其後兩天在東海緩慢移動。
  10. During 1950 ~ 1976 / 1977, the walker circulation over the tropical pacific and the vertical zonal monsoon circulation over the tropical indian ocean coupled at the oceanic continent, the same period when el nino occurs, the anomaly of the west wind over the tropical pacific can correlate with the departure of east wind over the tropical indian ocean through the two coupled vertical zonal circulation. but after 1976 / 1977, the updraft of the walker circulation moved eastward. locating at the north of australia. therefore the two vertical zonal circulation could n ' t coupled, and the anomaly of west wind and the departure of east wind could n ' t geared. in the result. the signal of enso decreased in indian ocean after 1976 / 1977

    1951 1976 1977年，熱帶太平洋的walker環流和熱帶印度洋的緯向季風環流在海洋性大陸附近耦合，當elnino事件發生時，太平洋的西風異常可以通過這兩個緯向的垂直環流與印度洋的東風異常聯系起來，而1976 1977年以後，由於西太平洋walker環流上升支東移到澳大利亞北部，熱帶兩洋的緯向垂直環流無法耦合，熱帶太平洋elnino事件中的西風異常與熱帶印度洋的東風異常聯系減弱，所以1976 1977年以後， enso在熱帶印度洋的信號減弱了。
  11. Chataan moved generally to the northwest in the next few days and attained typhoon strength on 5 july

    查特安在往後數天大致向西北移動，並於七月五日達至臺風強度。
  12. It then turned northwestwards before becoming almost stationary and attaining typhoon strength the following night

    它然後轉向西北移動，跟著差不多停留不動，並在翌日晚上達至臺風強度。
  13. On 23 june 2001, due to subsidence ( descending motion of the air over a rather broad area ) ahead of typhoon chebi, heat showers formed over inland guangdong and moved south to affect hong kong in the evening. these heat showers later developed into a northwest - southeast oriented squall line

    二零零一年六月二十三日，臺風飛燕前端出現下沉現象（較大范圍的空氣下降現象） ，導致廣東內陸地區產生熱驟雨，並在晚上南移影響香港。這些熱驟雨後來更發展成颮線，從西北延向東南。
分享友人
分享到 Line

分享到臉書