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westerly adj.西(方)的;向西的;從西面來的(風)。adv.在...

western

Seasonal variations of water vapor transport over east asia monsoon region are studied , especially that in summer season . the results indicate that there are four vapor inflow corridors to fetch china : southwest corridor , south china sea corridor , southeast corridor and northwest corridor . it shows impact of south asia monsoon , south china sea monsoon , subtropical monsoon and middle latitude westerly belt on summer rainfall anomaly over china , respectively 分析了東亞季風區水汽輸送的季節變化,并著重研究了夏季東亞季風區的水汽輸送特征,指出夏季東亞季風區水汽輸送有四條通道到達中國大陸:西南通道、南海通道、東南通道和西北通道,分別體現了南亞季風、南海季風、副熱帶季風和中緯度西風帶對中國夏季降水的影響。

During the el nino ( la nina ) events , the negative ( positive ) sst anomaly occurs and the corresponding the olr mjo intensity weakens ( enhances ) in the tropical western pacific ; at the same time , the positive ( negative ) surface westerly anomaly leads to positive ( negative ) mld anomaly , and the corresponding sst mjo intensity weakens ( enhances ) in the equatorial eastern pacific , 4 ) the interdecadal variation of the atmospheric mjo intensity took place distinctly in 1970s in the tropical western , northwest and eastern pacific , with the stronger intensity in the former than the back stage , and the interdacadal variation of sst is its cause Elnino ( lanina )事件中熱帶兩太平洋sst出現負(正)異常, olr季內振蕩強度出現減弱(增強)的變化。 elnino ( lanina )事件中,赤道太平洋出現地面信風西風分量正(負)異常,并引起熱帶東太平洋mld出現正(負)異常,造成熱帶東太平洋sst季內振蕩強度出現減弱(增強)的變化。 4 )熱帶印度洋、熱帶西太平洋和熱帶東太平洋季內振蕩強度在上世紀70年代發生了明顯的年代際變化,均為前弱、后強, sst本身的年代際變化是其原因。

Results show that subtropical high in june 1998 is more intensive and westerly and than normal , leading to the floods in yangtze river valley . vertical diabatic heating has stronger impacts on the variation of intensity and location of western pacific subtropical high 結果表明: 1998年6 - 7月西太平洋副高較常年同期偏強偏西,從而導致了我國長江流域持續暴雨洪澇天氣的發生;副熱帶地區的非絕熱加熱對副高的強度和位置的變化有極其重要影響。

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 由于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。

Diagnostic results show that the westerly wind stress anomaly and convergent meridional wind stress anomaly over the tropical pacific correspond to the every el nino , and the easterly anomaly and divergent meridional wind stress anomaly correspond to the vanishing of el nino 通過研究表明,每次elnino事件在熱帶太平洋都伴隨著西風應力異常以及向赤道輻合的經向風應力異常,東風應力異常及向兩極輻散的經向風應力異常與elnino消亡對應。

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 由于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。

Jet stream is an elongated belt of high speed air , typically found in upper tropospheric westerly flow round the globe . a jet stream may stretch over tens of thousands of kilometres in length from west to east and a few hundred kilometres in width from north to south 高空急流是圍繞地球的一條強而窄的高速氣流帶,集中在對流層上部或平流層中,在中高緯西風帶內或在低緯度地區都可出現。

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 由于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。

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分別于0910utc和1010utc轉吹西風,但是西風只持續了一段短時間,并于12utc左右全部轉回東風。

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分別于0910utc和1010utc轉吹西風,但是西風只持續了一段短時間,并于12utc左右全部轉回東風。

These three brethren told casual acquaintance that they were spending their whitsun holidays in a walking tour through the vale of blackmoor , their course being south - westerly from the town of shaston on the north - east 這兄弟三個告訴他們偶然遇見的人,他們正在過圣靈降臨節,要步行游玩黑荒原谷,他們的路線是從東北的小鎮夏斯頓往西南方向走。

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。

Formed about 910 km south - southwest of wake island on 19 august . moving in a westerly direction towards guam , chaba intensified into a typhoon on 22 august and turned northwestwards the next day 在八月十九日于威克島之西南偏南約910公里處形成。它向西移動,趨向關島。暹芭在八月二十二日增強成為一個臺風,翌日轉向西北推進。

Mr . yeung reckoned that decreasing wind speeds and increasing frequency of westerly winds might have contributed to the marked rise in reduced visibility at the observatory headquarters between the mid - 1980 s and the present day 楊繼興認為這些風速及風向的變化可能是80年代中期至今天文臺總部能見度轉差加劇的部份原因。

This anomalous non - uniform heating resulted in the powerful anticyclone vorticity locating in the south of yangtze river and western pacific , which lead to the intensive and westerly subtropical high 這種異常的非均勻加熱狀況導致我國江南到副熱帶西太平洋地區呈現帶狀的異常反氣旋性渦度制造,使得6一7月副高偏強偏西。

The spatial and temporal distribution character for lightning of the westerly zone systems and tropical systems that influence the south of china is studied and analyzed , and the difference between them is compared 摘要對影響華南的西風帶系統和熱帶系統的各類云系閃電時空分布特徵進行分析研究,比較它們之間的異同。

But venture into tai o , located on the far north - westerly edge of lantau island , and you ll find a small harbour where fishing is still a local trade today 要感受漁村風味,便得前往大嶼山西北部較為偏遠的大澳。當地仍有漁民作業,而搭建于木樁之上的棚屋,更成為大澳今日的熱門景點。

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 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。