潮區 的英文怎麼說

中文拼音 [cháo]
潮區 英文
actic
  • : Ⅰ名詞1 (潮汐; 潮水) tide 2 (比喻大規模的社會變動或運動發展的起伏形勢) (social) upsurge; cur...
  • : 區名詞(姓氏) a surname
  1. Small alluvial fans at mouths of wet weather drainage ways also are commonly intermixed indistinguishably.

    濕氣侯地河道出口處的小沖積扇,其沉積物的混合通常也難以別。
  2. An anticlockwise gyre near the kuroshio north of japan inland is simulated using a high - resolution topography

    在高分辨的地形條件下,日本西海岸外側的黑北部存在一逆時針漩渦,這可能與該域的漏斗型地形誘導有關。
  3. The arabian architectural method is of special interest because in many ways it would be a dangerous failure in a wet, european climate.

    阿拉伯的建築方法令人十分感興趣,因為若將它應用於濕的歐洲氣候地,在很多方面都可能造成危險的事故。
  4. More meaningful comparisons can be made by comparing water loss from the potometer with that from an atmometer ( an apparatus used to measure the rate of evaporation from a porous pot or other nonliving wet surface ), which allows uncontrolled evaporation

    更有意義的是,可以比較蒸騰計的失水與蒸發計(通過有孔小罐或者濕表面來測量蒸發速率的儀器)的失水間的別。
  5. Under the guidance of theories of sedimentology, petroleum geology and sequence stratigraphy, and through the comprehensive analysis of outcropsrock, cores, well logs and testing outcomes of rock gas, this paper studies the depositional systems of neopaleozoic and the character of aeration zone in tabamiao area of ordos basin. the result indicates that the object layers are divided into two depositional systems, the barrier seacoast depositional systems are recognized on upper carboniferous taiyuan phase with tidal flat, lagoon and barrier bar sedimentary deposit

    本文根據沉積學、石油地質學和層序地層學理論,綜合利用地表露頭、鉆井巖芯、測井曲線資料和試氣成果資料,對鄂爾多斯盆地塔巴廟塊晚古生代沉積體系及含氣層特徵進行了研究。結果表明,研究內目的層段可以劃分為2個沉積體系: ( 1 )上石炭統太原期為有障壁海岸沉積體系,發育坪?瀉湖?障壁砂壩沉積。
  6. The main contents include : water environment, marine sediment and the trend monitoring of marine life quality ; at the same time, to consolidate the monitoring of the functional zones, such as seashore bathing places, oceanic reserves, marine aquafarms ; to set up the seashell monitoring and controlling zones in the sea areas of both pingtan and yunxiao at the first time ; to carry out the statistical monitoring of polder, exploiting sea sand, spartin aallerni flora, terrestrial sewages, etc., to carry out monitoring of the total quantity of pollutants into the offshore marine areas in the min river, the jiulong river as well as the municipal sewages of xinlin industry in xiamen and jiaocheng in ningde ; to carry out the red tide monitoring in the offshore marine areas of fujian province ; to implement time - lapse, pointing and continuous red tide monitoring of high frequency and high intensity in the sandu gulf, the min river estuary and offshore marine areas of xiamen

    主要內容包括水環境、海洋沉積物和海洋生物質量的全海域環境趨勢性監測,同時加強了海水浴場、海洋保護、海水增養殖等功能監測;首次在平潭和雲霄海域設置了貝類監控;開展了圍填海、海砂開采、互花米草、陸源排污口統計監測;並在閩江、九龍江、廈門杏林工業排污口、寧德蕉城市政排污口鄰近海域開展污染物入海總量監測;在全省近岸海域開展赤監視監測,對三都灣、閩江口、廈門近岸海域赤監控實施高頻率、高密度的定時定點連續監測。
  7. There are many salt pans, fish farms, brushwood and gullies. when fish farms are drained in winter after yielding, fish surviving at the bottom of ponds and bathos will become the rich food source of water birds, and abandoned fish farms will be like natural swarms and habitats of birds

    多為鹽田、魚瘟、灌木叢、溝,魚瘟冬季收成放乾后,池底殘存的魚類及底棲生物提供水鳥豐富的覓食環境,而廢棄的魚瘟則形成半天然的沼澤則成為鳥類棲息地。
  8. Most tidal areas in sihcao are distributed near the outlet to the sea where the salt content is low and water flows slowly. therefore, they are ideal habitats for animals and plants and nourish a wide variety of bathos, such as fish, shrimps and shells. when low tide comes, we can see flocks of birds and packs of fiddler crabs come seeking food in these areas

    四草地間帶多分佈於出海口,因為此地位於河海交界,鹽分較低、水流緩慢,適合動、植物棲息,孕育豐富的魚蝦貝類等底棲生物,退時經常吸引成群的鳥類及招蟹前來覓食。
  9. The results show that the strong winter monsoon will decrease the gradient of ssh, and change the characteristics of sst, which has influence on the sea current, especially in a shallow and closed sea area such as the south china sea

    結果表明:強冬季風會減弱海面高度梯度,普遍降低黑潮區海表溫度,對流場有一定的影響,尤其在南海這樣的封閉海
  10. ( 3 ) the previously winter kuroshio ssta relates greatly to the east asian summer monsoon ( easm )

    ( 3 )前期冬季黑潮區域海溫異常與東亞夏季風存在顯著的聯系。
  11. Conclusions are drawn as follows : ( 1 ) there is a closely relationship between the autumn kuroshio ssta and the east asian winter monsoon ( eawm )

    ( 1 )秋季黑潮區域海溫異常與東亞冬季風有明顯的正相關關系。
  12. It also explain that the correlation between ssta of kuroshio and the change of wind field in equaroral mid - pacific is results of air - sea interaction ; however, when time comes into summer, the instance status of ocean is different from the last winter to next early springtime, the sea surface temperature turn into the definitive factor, so the increase of heat flux in may to jun month which is realized by absorbing more heat from the sun radiation results in the decrease of sst in kuroshio in the season of jun - jul. finally, during the aug to dec season of next year, the sst of kuroshio is increasing again

    最後分析了黑海溫與夏季東亞大氣環流及我國降水的時滯關系,發現:當前冬黑潮區域海溫異常偏高時,後期夏季亞洲低壓的強度減弱,西北太平洋副熱帶高壓強度加強,而且位置西伸、偏北,梅雨鋒位置偏南,長江中下游地降水偏多,北太平洋冬季海域的海溫分佈呈+ 、 - 、 +趨勢(順序為赤道中東太平洋、西北太平洋、我國近海) ;反之亦然。
  13. The study of rural - urban transition in the pearl river delta area

    海平面上升對珠江三角洲潮區水利工程和咸的影響分析
  14. ( 2 ) the anomalous eawm predominantly relates to the winter kuroshio ssta. the winter kuroshio ssta becomes positive ( negative ) when there is a strong ( weak ) eawm. the possible links might be the winter latent and sensible heat release in the west - northern pacific ocean

    ( 2 )東亞冬季風異常對冬季黑潮區域海溫異常有密切的聯系,當東亞冬季風偏強時,冬季黑潮區域海溫偏低;反之,冬季黑潮區域海溫偏高。
  15. A 3d baroclinc ocean model is used to model the ocean current around the kuroshio area on the condition of successively anomalous east asia winter monsoon, some significant results are obtained, and the influence of strong ( weak ) winter monsoon on sea surface height ( ssh ), sea surface temperature ( sst ) and sea current around the kuroshio area is analyzed preliminarily

    摘要運用一個三維斜壓海洋模式對冬季風風場持續異常時期的黑潮區海洋進行了模擬,初步分析了冬季風風場持續異常對黑潮區海面高度、海流和海溫的影響。
  16. By using of eof analysis, distribution of sst over the kuroshio area during winter are identified, which show cold or warm anomaly

    本文首先通過eof分析確定了冬季黑潮區sst的主要分佈形勢,發現冬季黑潮區海溫主要表現為冷異常或暖異常。
  17. When the winter kuroshio ssta is high, there is high ( low ) pressure ( compared with mean ) in the asia and weak ( strong ) easterly jet at high level in summer. at the same time, the west - northern pacific high becomes strong ( weak ) and shifts westward ( eastward ) and northward ( southward )

    當冬季黑潮區域海溫異常偏高時,亞洲熱低壓強度減弱,西北太平洋副熱帶高壓位置西伸且偏北,強度明顯偏強,梅雨鋒位置偏南,長江中下游地降水偏多。
  18. From just the entrance, in the southern part of the bay, up to a second slack water area, about midway up the bay, tidal currents are ebbing

    在海灣的南部,從緊靠入口處內側直到第二平潮區,其間距離大約是到海灣的一半,流正在回落。
  19. ( 4 ) based on the ncar ccm3 simulations, the influence of the previously winter kuroshio ssta on the easm is investigated. results from the simulations are highly coincidence with the observations, namely, the winter kuroshio ssta may impacts the subsequent year east china summer rainfall by making influencing on the strength and location of the west - northern pacific high and the easm systems

    ( 4 )利用ncarccm3模式模擬冬季黑潮區域海溫異常對東亞夏季風的影響,模式模擬的結果與統計分析結果是一致的,即前期冬季黑潮區域海溫異常可以通過影響次年夏季的西太平洋副熱帶高壓的強度和位置變化以及東亞夏季風環流的強弱,從而進一步影響我國東部地的降水,尤其是長江中下游地
  20. When the autumn kuroshio ssta is positive, the sea - land sea level pressure differences in the east asian region become large in winter, the east asian trough at 500hpa shifts eastward and is deep in its south and shallow in the northern, along with strong north winds in the above area and weak westerly circulation in the asian region

    當秋季黑潮區域海溫異常偏高,東亞地的海陸氣壓差異進一步加大,東亞大槽北部減弱、南部加深、位置東移,東亞地的偏北風加強,亞洲地西風環流減弱,即東亞冬季風加強;反之亦然。
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