氣壓脊 的英文怎麼說
中文拼音 [qìyājǐ]
氣壓脊
英文
pressure ridge-
( 2 ) sxsp anomaly is closely related to the abnormity of 500hpa geopotential height field over the east of ural and yakutsk area, western ridge point and area of subtropical high, the cold air abnormity from north of china and the position of upper level westerly jet over east asia
( 2 )三峽庫區夏季降水異常與大氣環流異常密切相關:與500hpa烏拉爾山以東高度場異常、雅庫茨克以東高度場異常、副熱帶高壓面積及西伸脊點、北方冷空氣異常、 200hpa東亞高空西風急流位置異常偏南(偏北)密切相關。The summer rainfall anomaly of north china is closely related to indian low, west pacific subtropical high, westerly troughs and ridges in mid - latitude, south asia high, subtropical monsoon circulation and cold air activity on the corresponding period, and similar circulation pattern also appears in the preceding spring
結果表明: ( 1 )華北夏季降水異常與同期印度低壓、西太平洋副高、中緯度西風槽脊、南亞高壓、副熱帶季風環流和冷空氣活動的異常都密切相關。華北夏季降水異常年春季的環流特徵與夏季類似。The quasi - geostrophic process was diagnosed for a case of severe cold air breakout under the blocking situation during 16 - 18 march of 1998. the attention was focused on the relationship between the surface anticyclone and 500hpa blocking high. the results indicate that the cold outbreak is associated with the adjustment of blocking situation in the ural area, i. e. the collapsing and rebuilding of the ural mountain blocking high. the temperature advections in the lower troposphere shown that the polar cold air invading from the northwest caused the ural blocking high collapsed, and a new ridge developed rapidly was due to the warm advection on the southwestern side which led to the ural blocking high rebuilt. in addition, the distribution of the vertical motion on 700hpa shown that the surface high splitting was related to the considerable upward motion located on the southeastern part of surface high
對1998年3月中旬一次高空阻塞形勢下強冷空氣過程進行了診斷分析,著重討論強冷空氣爆發前後地面反氣旋活動與高空阻塞形勢調整的關系。研究結果表明,強冷空氣的爆發與烏拉爾地區阻塞形勢的調整阻塞高壓的崩潰和重建緊密相關。對流層下部的溫度平流分析表明,阻塞形勢的調整是由於阻塞高壓上游西北方有冷空氣侵入導致了阻塞高壓的崩潰,而上游來自西南方向的強暖流則導致高壓脊迅速發展,使阻塞高壓重新建立。A ridge of high pressure is an elongated area of high pressure
當高氣壓呈延長狀,稱為高壓脊。A ridge of high pressure is approaching from the atlantic and will bring sunny wheather
來自大西洋的高壓脊正在逼近,將會帶來陽光充足的天氣。E. weatherwise, a ridge of high pressure covered that area, bringing fine weather and light winds, hence the calm sea
在天氣方面,一道高壓脊正覆蓋著該區,為該區帶來晴空及微風,造就了平靜的海面。With a ridge of high pressure extending westwards from the western pacific, the weather over the south china coastal region improved in late june
六月下旬,西太平洋的高壓脊向西伸展,令華南沿岸地區天氣逐漸好轉。With a strong ridge of high pressure dominating over southern china, fine weather has persisted in hong kong and neighbouring areas for over two weeks
由於華南地區受到一道高壓脊的影響,香港的晴朗天氣已持續了兩個多星期。The weather pattern that day see the weather chart was characterized by a ridge of high pressure ahead of a cold front over south china
當日華南地區正受一道冷鋒前緣的高壓脊所支配見天氣圖,地面吹偏東風,而大嶼山山頂則吹南風。The weather pattern that day ( see the weather chart ) was characterized by a ridge of high pressure ahead of a cold front over south china
當日華南地區正受一道冷鋒前緣的高壓脊所支配(見天氣圖) ,地面吹偏東風,而大嶼山山頂則吹南風。The ncep / ncar reanalysis data, china 740 stations precipitation data, and the tbb data from meteorological institute research of japan are employed to study the structure and variation law of subtropical high ( sh ) in the period of double ridges. by combining together case diagnosis and statistic analysis, some new findings of the sh double ridges are obtained
本文以副熱帶高壓結構和活動規律為線索,圍繞副高雙脊線這一新主題,利用ncep / ncar再分析資料、中國臺站降水資料以及日本氣象廳提供的tbb資料,通過個例分析和統計分析,發現了若干新事實,揭示了與副高雙脊線有關的一系列特徵和規律。The results show that a warm high ridge at the middle level and transformed surface cold high over the plain provide a good background condition ; a cooling process produced by net surface radiation fluxes is the trigger and strengthening mechanism for the fog event ; the subsidence flow at the middle and low tropospheric levels is favorable for the setting - up and maintenance of stable stratification at the boundary layer and weak wind condition at the ground layer over the fog region ; the transportation of weak warm advection at lower levels and weak lift motion at the boundary layer play a very important role to the long maintenance of the fog event ; the intrusion of north wind accompanied by cold advection is a main dynamic factor of the fog dissipation
結果表明:在中高層暖性高壓脊及地面變性冷高壓穩定維持的大尺度背景條件下,地表凈輻射引起的近地層冷卻是大霧過程的觸發和加強機制;中低空下沉氣流的存在有助於近地層的弱風條件和穩定層結的建立;低層暖平流的輸入和邊界層的淺層抬升是大霧長時間持續的原因;伴隨冷空氣南下的偏北大風是驅使大霧消散的動力因子。When the spatial pattern is of the north - south asymmetry, in the warm north - cold south years, there is a anticyclone circulation existing over the warm pool at 850hpa, easterly at 15 n and westerly in the tropical region have been greatly strengthened, while the center of anticyclone circulation moves to the east asia at 200hpa, and the hadley circulation has been affected evidently, so the summer rainfall may be above normal in the middle and lower reaches of the yangtze river, vice versa. there are different relations to east asia atmospheric circulation and summer rainfall in china
當ssta為南北半球反對稱分佈時,與ssta北暖南冷分佈相對應, 850hpa暖池區上空為一反氣旋偏差環流, 15 n附近東風氣流和赤道附近西風氣流增強,長江中下游地區盛行偏南風氣流; 200hpa反氣旋偏差環流中心移到東亞大陸上空;副熱帶高壓強度、西伸脊點都明顯變強、西伸; hadley環流得到發展,長江中下游(華北)地區為上升(下沉)氣流,降水明顯增多(減少) ,北冷南暖年則相反。However, in july 2002, the subtropical ridge did not extend to southern china and the steering flow over the northwest pacific had a more northerly direction than usual. as a result, the tropical cyclones in the region were carried northwards and did not enter the south china sea (
但今年同期副熱帶高壓脊並沒有西伸至華南,使西北太平洋上引導氣流的方向比正常偏北,在該區的熱帶氣旋因此偏向北移,而不向西進入南海(The pressure there is higher than that at neighbouring points on either side of the ridge line
脊軸線上的氣壓會較其兩旁氣壓為高。Usually, the subtropical ridge over the pacific extends westwards to southern china in july, steering the tropical cyclones over the northwest pacific to move westwards and enter the south china sea (
太平洋上的副熱帶高壓脊通常會在七月份向西伸延至華南,這有利西北太平洋上的熱帶氣旋向西移動進入南海(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。3 by delineating the various features of the weather maps and putting them into layers i. e., pressure cells, troughs, ridges etc, users can overcome visual information overloads by selecting appropriate layers of interest and animating them over time
將描述天氣地圖的不同特徵如氣壓單元,低壓槽和高壓脊並將其放入不同的層中,用戶可以選擇感興趣的圖層以避免可視信息過量,並使之以動畫形式表示。In the atmosphere, geopotential varies with altitudes and across latitudes. on an isobaric surface, higher geopotential implies higher potential energy and vice versa. just like streams flow according to the layout of terrain, air will flow from high to low geopotential regions
在等壓面天氣圖上,位勢高的地方位能較高,位勢低的地方位能較低,高空的氣流會由前者流向後者,情況有點像河川根據山脊高低的分佈而流動一樣。分享友人