海洋的季節 的英文怎麼說

中文拼音 [hǎiyángdejié]
海洋的季節 英文
the seasonal seas
  • : Ⅰ名詞1 (海洋) ocean 2 (洋錢) silver coin 3 (姓氏) a surname Ⅱ形容詞1 (盛大; 豐富) vast; m...
  • : 4次方是 The fourth power of 2 is direction
  • : 節構詞成分。
  • 海洋 : seas and oceans; ocean; [詩歌用語] blue海洋霸權 maritime hegemony; 海洋保護區 marine preserve; 海...
  1. The apec summit coincided with the high autumn fishing season. to ensure safe communications and under the coordination of the municipal government, we cooperated with marine regulatory and fishery administrative departments in jiangsu, zhejiang and shanghai to wage a cable protection combat that involved 36 boats and round - the - clock watch keeping. fighting furious waves on the unbounded sea in resolute will, our staff expelled 1, 457 fishing rule - violating boats and contributed in a tacit way to the safe communications of the apec summit

    底光纜是通信保障薄弱環, apec會議期間正值秋漁汛高潮,為了確保安全,在市政府協調下,我方聯合了江蘇、浙江、上監管和漁業管理部門,聯合行動,出動了36條護纜船,日夜拼搏,劈風斬浪,戰斗在一望無邊中,驅趕違規漁船1457艘,為apec期間通信安全立下了汗馬功勞。
  2. Transient species such as the yellow croaker and melon seed, typically found off northern china and japan, bolster the resident marine fauna when the monsoonal flow brings in cooler waters

    此外,還有一些基本上在中國北部及日本水域出沒過境品種,諸如黃花魚及瓜核魚,這些魚類隨著較涼性水流來港,令該段時間本港動物數量大增。
  3. Areas that are well protected from the ocean experience a more continental type of climate with warmer summers, colder winters, greater daily and seasonal tempe - rature ranges, and generally lower relative humidity

    種植區域逐漸由性氣候變為大陸性氣候,夏天炎熱,冬寒冷,每日和溫差較大,並且濕度相對較低。
  4. Therefore, in the development process of domestic and international ocean science, thermocline, particularly the seasonal thermocline, is always one of the main subjects

    因此,在國內外科學發展過程中,溫度躍層,尤其是性溫度躍層調查和研究一直是調查研究主要內容之一。
  5. 4 ) air - sea interaction retain its character throughtout the seasonal cycle in the tropical pacific, but it is not the same in the north pacific ; and there are also relationships in the two areas : 1 ) for the interdecadal time scale, there is the same abrupt change both in the north pacific and in the tropical pacific, especially in winter

    4 )熱帶太平區域氣相互作用有較好一致性;而北太平區域氣相互作用差異較大。區域間主要聯系為: 1 )兩個區域主要年代際躍變點出現時間接近,這在冬反映最明顯。
  6. Being now passed the vast ocean, and a sea of troubles before them in expectations, they had now no friends to welcome them, no inns to entertain or refresh them, no houses, or much less towns, to repair unto to seek for succour ; and for the season it was winter, and they that know the winters of the country know them to be sharp and violent, subject to cruel and fierce storms, dangerous to travel to known places, much more to search unknown coasts

    現在越過了浩瀚,一個預期中困難之攔在他們前面,沒有朋友來歡迎他們,沒有可以款待或使他們恢復體力小旅館,沒有房子,或少得多城鎮,讓他們修整後去尋找援助,而且因為是冬天,那些了解這個國家冬天人們知道它是嚴酷和殘暴,遭受殘酷和猛烈暴風雪,到已知地方旅行是危險,探索未知岸更是危險得多。
  7. Longing for the sea, is a seasonal symptom, and can ' t be restrained

    摯念,似乎是一種無可抑止性疾病。
  8. Severe ocean storms happen less often in the southern hemisphere. there the season of greatest activity is between december and march

    一般在南半球劇烈性風暴會少些,最強烈和頻繁大概是在十二月和三月
  9. Game on the fishermen in the marine fish breeding season, the total catch seagulls to the sea. xiaoyuer be allowed to be born t just by the amount of predation

    游戲介紹:漁民們在魚類繁殖,總要出鷗,為是讓剛出生小魚兒可以不被大量捕食。
  10. Compared with water temperature and the monthly alternatives of fish was much significant

    漁獲種類變化比較明顯,與表層水溫變化有關,種類月更替率比較高。
  11. The species composition of fish varied significantly with seasons, particularly high with monthly alternatives, and associated with changes of water temperature

    漁獲種類變化比較明顯,種類月更替率比較高,與表層水溫變化有關。
  12. With the exception of the tropical western pacific of large mld. there is negative correlation relationships between the anomaly of the sst mjo intensity and that of the mld in the other three regions in the seasons of the climatic small mld thus the causes of climatic and anomalous characteristics of atmospheric mjo are related to sst identically, and the corresponding features of sst mjo are related to mld, 3 ) enso is the strongest sign and can lead to the distinct sst and mld anomaly, hence the intensity anomaly of the air - sea system inevitably takes place during the enso

    Sst內振蕩強度與mld異常局地同時性相關結果是,熱帶西太平無顯著相關(氣候mld較大) ,其餘三關鍵區氣候mld小均存在sst內振蕩強度與mld異常負相關聯系。因此大氣內振蕩氣候及異常特徵直接成因一致地與sst 、有關;內振蕩相應特徵則直接與mld有關。 3 ) enso是氣系統中最強異常信號,在中它引起了sst 、 mld明顯異常,因此,伴隨enso必然發生氣系統內振蕩強度異常。
  13. Concentrations of total suspended matter ( ctsm ) is unanimous with observational data and other scholars " researching results. the distribution of ctsm is higher along coast than other areas there is a tongue - like zone with high ctsm from north to southeast. the transport simulation result reveals that sm can spread to the okinawa trough for enough sea water mixing in winter. but in summer. sm can not traverse the big water barrier of kushino for different circulation character. this difference is probably related to the shifting n - s monsoon

    懸浮體輸送表明,在冬,懸浮體除了在陸架上發生擴散外,由於強烈混合作用和環流性變化,部分中、底層懸浮體可擴散至沖繩槽甚至西太平;在夏,由於水層化及夏環流特徵,懸浮體基本不能穿越黑潮這一水障,這一差異可能是由於風和不同環流特徵所引起
  14. In equatorial region, the mean air - sea humidity difference is much smaller, so the variations of air - sea humidity difference under large mean wind speed dominate the variations of latent heat flux. the ocean release the most heat during the period from march to may, when sst is highest in the whole year because sst dominates the variation of air - sea humidity difference

    在赤道冷舌區,平均背景氣濕度差比較小,所以平均風速背景下氣濕度差熱帶大西表潛熱和感熱通量和年際變化研究變化主導該區潛熱通量變化。
  15. Based on the observation data such as coads and soda, the main climatological features of the tropical indian ocean and relationships of sea surface temperature ( sst ), heat budget with ocean dynamics and thermodynamics processes are analyzed ; the seasonal and interannual variability of the tropical indian ocean are well simulated using a ocean general circulation model ; based on the thermal equation and model output data, the variation mechanism of sst and heat budget are investigated in the tropical indian ocean ; besides, the effect of seasonal variation of wind stress, ekman pumping and horizontal diffusivity on the ocean current and heat budget are studied, using both ideal model and complex model

    本文根據coads 、 soda等實際觀測資料,較全面分析了熱帶印度主要氣候特點,並研究了表面溫度( sst ) 、熱收支與動力、熱力過程聯系;利用全球環流模式較好地模擬出熱帶印度和年際變化;基於熱力學方程和環流模式輸出結果,探討了熱帶印度sst和北印度熱量收支和年際變化機制,進一步揭示了動力過程在北印度熱平衡中重要作用;在此基礎上,利用理想化數值試驗與數值模擬結果相結合方式,證實了風應力變化和ekman抽吸,以及水平熱量擴散系數對北印度環流和熱收支影響。
  16. All these results confirm the important of wind in meridional circulation and heat transport. based on mom2 model, a rectangular basin model with ideal w ind stress and other ideal conditions is designed to study the main processes and dynamical mechanism in setting the depth of cross - equator flow. the effects of horizontal diffusivity, seasonal variations of

    我們還通過全球環流模式,進一步證實了風應力變化在北印度熱收支、 sst以及環流變化中作用:即包含風應力變化將使長期平均sst降低,面凈熱通量增加。
  17. Based on the importance of heat flux variability to the earth ' s climate change and the dependence of the study about heat flux variability on the accuracy of heat flux data, this study will focus on the quality evaluation of heat flux datasets available and seasonal and interannual variability of latent and sensible heat fluxes in the tropical atlantic ocean

    基於表潛熱和感熱通量時空變化在全球變化中重要性和表潛熱和感熱通量研究對熱通量資料產品精度依賴性,本文重點就現有熱通量資料產品質量和熱帶大西表潛熱和感熱通量和年際變化開展較深入研究。
  18. It can be found that a great quantity of vapor is transported to atmosphere from arctic ocean open sea in summer, which is very important to concerns on season change of heat budget on arctic ocean

    由此可見,在北冰,無冰面有大量水汽向大氣輸送,這對研究北冰地區大氣邊界層變化過程是至關重要
  19. The seasonal cycle and interannual variation of sea surface height from topex / poseidon and ers - 1 / 2 are analyzed in tropical pacific and indian oceans in this study, and they are compared with those from a coupled climate model fgcmo in order to assess the ability of the model to simulate seasonal cycle and interannual variation in sea level height

    本文利用衛星面高度計資料,分析了赤道太平和印度面高度變化和年際變化特徵,並與一個耦合氣候系統模式fgcmo模擬面高度進行比較,評估模式模擬面高度和年際變化能力。
  20. The tropical indian ocean, especially for the region north of 7, is strongly influenced by asia monsoon. in response to the seasonal reversal of wind, ocean currents also show obvious seasonal reversal with somali current most prominent

    熱帶印度,尤其是7 s以北印度,受亞洲顯著影響,與風對應,環流也有很明顯變化,最明顯是索馬里轉向。
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