海洋資料站 的英文怎麼說

中文拼音 [hǎiyángliàozhàn]
海洋資料站 英文
ocean data station
  • : 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...
  • : Ⅰ名詞1 (錢財; 費用) money; wealth; expenses 2 (資質) intelligence; endowment 3 (資格) quali...
  • : 名詞1 (材料; 原料) material; stuff 2 (喂牲口用的穀物) feed; fodder 3 (料器) glassware 4 (...
  • : Ⅰ動詞1 (站立) stand; be on one s feet 2 (停下來; 停留) stop; halt; pause Ⅱ名詞1 (停車點) st...
  • 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...
  • 資料 : 1. (生產或生活的必需品) means 2. (依據的材料) data; material
  1. " our major concerns on the eia report include inadequate information regarding the future gas supply, the conflicts between the objectives of marine parks and an lng terminal, a lack of real commitment in protecting chinese white dolphin and other marine species and down playing of the black point option " said clarus chu, marine conservation officer, wwf hong kong

    本會環境保護主任朱炳盛表示:我們對環評報告特別關注的部份包括:有關未來天然氣供應的不足岸公園與天然氣接收並存的可能性,中電對保護中華白豚和其他生物欠缺真正的承擔,以及對鼓灘選址欠缺公平的比較。
  2. Abstract : monthly rainfall data from 1951 to 1995 for june, july and august in 13 meteorological stations of the north china were used for accounting z index and discussing serious flood and drought featureas in these months. serious flood mainly happened in july and august, and sevious drought mainly happened in august. there were more flood in 1950 ' s to 1960 ' s and more drought since 1970 ' s in the north china. meanwhile, the deeper trough which covered the regions from the ural mts. to the balkhash lake play an important role in serious rainstom in rainy season in the north china. there often happened serious flood ( drought ) when the northwester pacific subtropical high was by west and north ( east and south ), and the sea surface temperature in the equatorial central and eastern pacific was mainly in dropping ( raising ) stage

    文摘:利用華北平原地區的13個點, 45年( 1951 1995 )的降水,對夏季4個時段( 6月、 7月、 8月、 6 8月)進行了z指數計算,確定了該地區各個時段的嚴重澇年和嚴重旱年.發現華北地區雨季的嚴重洪澇主要集中在7 , 8月,嚴重乾旱則主要發生在8月,並可明顯看出由50 60年代的多水期向70年代中期以後的少水期的轉變,另外,烏拉爾山到巴爾喀什湖附近的低壓槽加深和西北太平副熱帶高壓的北抬,對華北地區雨季持續性暴雨的產生起著決定性的作用.嚴重洪澇年的夏季( 6 8月) ,西北太平副熱帶高壓偏西、偏北,赤道東太平溫多處于下降階段;嚴重乾旱年西北太平副高偏東、偏南,赤道東太平溫則處于上升階段
  3. Based on the thermohaline data in august of 1958 and 2000, january of 2001, january and august in the marine atlas of bohai sea, yellow sea, east china sea ( hydrology, 1992 ), the normal annual wind field data in bohai sea, and the near forty years sss data observed in the four measurement stations beihuangcheng, tanggu, qinhuangdao, huludao of bohai sea : the thermohaline field ' s variance characteristics are analysed

    基於1958年8月、 2000年8月、 2001年1月、 《渤、黃、東圖集( 1992 ) 》中的1月和8月份溫鹽、渤多年平均風場以及渤北隍城、塘沽、秦皇島和葫蘆島4個水文測近40年的sss觀測,分析了渤溫鹽場的變異特徵。
  4. Data used in this work are north pacific ssta, 160 stations precipitation of china, and ncep reanalysis data. main results are as follow : ( 1 ) it is found that a apparent transition of north pacific ssta in later 1970 ' s : eastern and middle - equatorial pacific ssta turns from cold to warm with area extending, and mid - latitude pacific ( west wind drift zone ) turns from warm to cold. during this transition of ssta, different characters also appear in el nino and la nina : before 1976, la nina happens more frequently, and its duration is longer, el nino zone develops from negative ssta in the early stage ; after 1976, el nino happens a little bit frequent and longer with more intensity than before, el nino zone develops from positive ssta in the early stage ; the course of ssta variation has an enso cycle of 2 - 6 years, annual oscillation of 8 - 9 years, and decadal variation of about 22 years

    本文採用1950 - 1999年北太平表溫度( sst ) 、中國160夏季降水和ncep再分析的歐亞500hpa高度場等,利用eof 、 svd 、小波分析、合成分析和相關分析等方法,在分析北太平溫時空分佈特徵的基礎上,著重探討了溫異常及其年代際變化對我國東部降水的影響,並對降水、高度場和溫三者之間的關系進行了分析,以試圖尋找三者異常之間可能的聯系,主要結論如下: ( 1 ) 1976年前後,北太平溫經歷了一次明顯的轉變,赤道中、東太平厄爾尼諾區由冷轉暖,暖水范圍增大,中緯度西風漂流區溫由暖轉冷;在這樣的年代際背景下,厄爾尼諾、拉尼娜事件在不同的時期也有不同的特徵:在76年前,拉尼娜事件發生頻率高,持續時間長,事件起始於負溫距平;而76年後,則是厄爾尼諾事件發生頻率略高,持續時間長,強度增大,事件起始於正溫距平。
  5. From the situ - observation data of shallow and deep water regions at the coastal zone, it is shown statistically that the occurrency of the coupled ocean waves is more than those of the wind - induced waves and swell. the ratio of the coupled ocean waves at the yangtse river estuary ( especially at shallow sea region ) is nearby 70 % of all the ocean waves, for instance at the observation station dajishan

    近岸(淺水)波浪測和深水的波浪觀測統計表明,混合浪的出現均大於純風浪和純涌浪,特別在淺水區域,例如大戟山,混和浪所佔的比率接近70 。
  6. Using monthly temperature and rainfall data of 160 stations in china and global sea surface temperature and heat content data, diagnostic analysis is performed by means of harmonic analysis, correlation analysis, svd and corresponding statistical significance test methods

    利用全球溫、熱含量、中國160月平均氣溫和降水,通過周期分析、相關分析和奇異值分解( svd )以及相應的統計學顯著性檢驗方法,分析比較了全球熱狀況與氣候異常的相關聯系。
  7. In order to study the variation characteristics of heat flux at nansha and xisha islands in the south china sea, the observational data from the ocean stations are calculated to obtain air - sea heat exchanges and the annual circulation of heat budget around the summer monsoon onset in 1998

    摘要為探索西沙和南沙氣熱通量時間演變特徵,用觀測計算了1998年南夏季風爆發前後,氣界面熱量交換值及面熱收支年循環。
  8. On receipt of this and similar information from other seismograph stations in different countries, ptwc would determine the location, depth and magnitude of the earthquake and assess the likelihood of a tsunami. it would send a message to participating countries and territories on details of any tsunami forecast including the expected arrival time and amplitude of the tsunami at different locations around the pacific

    太平嘯警報中心收到各國地震的地震后,會計算地震震中位置、深度和地震強度並且評估發生嘯的可能性,並向參與的國家及地區發送詳細嘯預測,包括預期嘯到達太平沿岸各地區的時間及嘯高度等。
  9. Using ncep / ncar 40 - year reanalysis, gisst2. 3b data - set, cru south oscillation index along with in situ the 160 station data of surface air temperature / rainfall records in china, the inter - decadal variations in the relationship between equatorial western and eastern pacific variabilities are examined. the possible relations to the surface air temperature / rainfall in china are also investigated

    利用ncep / ncar再分析、全球冰gisst2 . 3b、英國cru提供的南方濤動指數以及中國160降水和氣溫,分析了熱帶太平地區氣系統內部聯系的年代際變化特徵及其與中國降水/氣溫異常的聯系。
  10. Monthly rainfall data from 1951 to 1995 for june, july and august in 13 meteorological stations of the north china were used for accounting z index and discussing serious flood and drought featureas in these months. serious flood mainly happened in july and august, and sevious drought mainly happened in august. there were more flood in 1950 ' s to 1960 ' s and more drought since 1970 ' s in the north china. meanwhile, the deeper trough which covered the regions from the ural mts. to the balkhash lake play an important role in serious rainstom in rainy season in the north china. there often happened serious flood ( drought ) when the northwester pacific subtropical high was by west and north ( east and south ), and the sea surface temperature in the equatorial central and eastern pacific was mainly in dropping ( raising ) stage

    利用華北平原地區的13個點, 45年( 1951 1995 )的降水,對夏季4個時段( 6月、 7月、 8月、 6 8月)進行了z指數計算,確定了該地區各個時段的嚴重澇年和嚴重旱年.發現華北地區雨季的嚴重洪澇主要集中在7 , 8月,嚴重乾旱則主要發生在8月,並可明顯看出由50 60年代的多水期向70年代中期以後的少水期的轉變,另外,烏拉爾山到巴爾喀什湖附近的低壓槽加深和西北太平副熱帶高壓的北抬,對華北地區雨季持續性暴雨的產生起著決定性的作用.嚴重洪澇年的夏季( 6 8月) ,西北太平副熱帶高壓偏西、偏北,赤道東太平溫多處于下降階段;嚴重乾旱年西北太平副高偏東、偏南,赤道東太平溫則處于上升階段
  11. In this paper, decadal variability of tropic and north pacific ' s ssta and of precipitation in china, correlations between them and the possible mechanisms of the ssta decadal change compacting on the precipitation decadal change are analyzed by using ncep globe temperature, wind and height data ( 1948 - 2001 ), coads ssta data ( 1900 - 2001 ) and 147 stations " precipitation data in china. results show that : ( 1 ) mid - high latitude north pacific and tropic west pacific ssta have obvious decadal change, the prior ' s decadal change has great variance and the latter ' s has great contribution in total variance, the main eigenvectors " distribution are stable in eof of tropic and north pacific ssta ' s decadal variability, the key area of the first eigenvector allots in two sides of tropic pacific ; the second one ' s allots in mid - high latitude northwest pacific and low latitude mid - east pacific which vary contrary ; the third one ' s allots in middle north pacific

    本文利用ncep( 1948 - 2001年)中的全球表面溫度場、風場、高度場, coads ( 1900 - 2001年)表面溫度距平及中國147個點1951 - 2001年共51年的降水,探討了熱帶及北太平ssta 、中國降水的年代際變化特徵,夏季熱帶及北太平ssta年代際變化與中國夏季降水年代際變化的耦合相互關系以及夏季熱帶及北太平ssta年代際變化影響中國夏季降水年代際變化的可能機制,結果表明: ( 1 )北太平中高緯與熱帶西太平均有明顯的年代際變化,北太平中高緯年代際變化方差顯著,而熱帶西太平年代際變化方差貢獻顯著。
  12. This paper is concerned with the time - spatial characteristics of summer extreme precipitation over eastern china and with the teleconnection between summer extreme precipitation and sst of the north pacific and soi, based on the daily rainfall data of 59 stations from 1951 to 2000

    本文利用我國東部( 105e ~ 0以東) 59個測1951 - 2000年的夏季逐日降水對我國東部夏季降水極值的時空特徵及其與北太平溫和南方濤動指數( soi )的遙相關進行研究。
  13. In this website, each of the lively ocean s 10 will narrate its own unique story about the biology, fun facts, threats and conservation status

    在新設的網內,十寶將以生動有趣的方式介紹自己的生態趣味小檔案,面對的威脅和保育狀況。
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