westerlies 中文意思是什麼
westerlies
解釋
偏午-
At this stage sea - level westerlies are strong and zonal in character and they lie poleward of their normal position
在這一階段海平面上西風氣流很強且屬緯向性的，它較正常位置偏向極地（北半球上偏北或南半球偏南） 。 -
The belts of prevailing westerlies in general have moderate average temperature.
一般來說，盛行西風帶的氣溫比較適中。 -
The complexities of the northern belt of westerlies are well illustrated in climates in the united states.
美國的氣候相當有力地說明了西風帶北緣的復雜性。 -
The results show that the heavy storm was caused by the interaction between a tropical cyclone trough that landed in guangdong province and a weak cool front in the westerlies
結果表明，本次大暴雨是由在廣東登陸的熱帶氣旋倒槽北伸與西風帶弱冷空氣相結合的產物。 -
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。 -
In winter ( january ), there are four nearly latitudinal moisture transport belts ( channel ) over asian - australian monsoon region. they are closely related with the easterlies and westerlies over southern hemisphere and northern hemisphere. in boreal winter, asian monsoon region is moisture source ; the cross equatorial moisture transport channels transport the moisture to australian monsoon and south indian ocean from asian monsoon region
主要結論如下： （ 1 ）冬季（ 1月）的水汽輸送形勢與南北半球東、西風帶緊密聯系，主要有四條近似緯向分佈的垂直積分的強水汽輸送帶，越赤道輸送將水汽從亞洲季風區輸送到南半球澳大利亞季風區和南印度洋季風區，亞洲季風區為水汽源區。 -
As 22 january 1999 was a fine day, the signal returns captured by the terminal doppler weather radar tdwr were too weak and the westerlies were too shallow for any windshear event to be detected using tdwr data
由於一九九九年一月二十二日天氣晴朗，機場多普勒天氣雷達tdwr收集到的回波訊號相當微弱，而且西風也太淺薄，以致未能根據tdwr數據探測到風切變現象。 -
As 22 january 1999 was a fine day, the signal returns captured by the terminal doppler weather radar tdwr were too weak and the westerlies were too shallow for any windshear event to be detected using tdwr data. a windshear alert had been issued following receipt of aircraft report
由於一九九九年一月二十二日天氣晴朗，機場多普勒天氣雷達（ tdwr ）收集到的回波訊號相當微弱，而且西風也太淺薄，以致未能根據tdwr數據探測到風切變現象。 -
As 22 january 1999 was a fine day, the signal returns captured by the terminal doppler weather radar ( tdwr ) were too weak and the westerlies were too shallow for any windshear event to be detected using tdwr data. a windshear alert had been issued following receipt of aircraft report
由於一九九九年一月二十二日天氣晴朗，機場多普勒天氣雷達（ tdwr ）收集到的回波訊號相當微弱，而且西風也太淺薄，以致未能根據tdwr數據探測到風切變現象。 -
From 500 - hpa geopotential height maps, one can depict important weather systems on the large scale, e. g. subtropical ridge or long - wave troughs in the westerlies
從500百帕斯卡的位勢高度圖，可清楚檢視大尺度的重要天氣系統，例如西風長波槽或副熱帶高壓脊等等。 -
The events in table 1 could be grouped into 2 separate episodes, the first around 07utc when the westerlies were advancing across the airport and the second around 13utc when the westerlies were retreating
表一所載事項可歸納為兩次不同的事件。第一次發生在大約07utc西風吹越機場的時候，而第二次則發生在大約13utc西風減弱的時候。 -
The sea breezes slowly advanced across chek lap kok and winds at r1c and r1e veered to westerlies at 0910utc and 1010utc respectively. however, the westerlies were short - lived and winds all backed to easterlies by around 12utc
海風緩慢地吹越赤角，而r1c和r1e分別於0910utc和1010utc轉吹西風，但是西風只持續了一段短時間，並於12utc左右全部轉回東風。
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