海洋升溫 的英文怎麼說

中文拼音 [hǎiyángshēngwēn]
海洋升溫 英文
oceanic warming
  • 洋 : 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...
  • 升 : Ⅰ動詞1 （由低往高移動） rise; hoist; go up; ascend 2 （等級提高） promote Ⅱ量詞1 （容量單位） lit...
  • 溫 : Ⅰ形容詞（不冷不熱） warm; lukewarm; hot; gentle; mild Ⅱ名詞1 （溫度） temperature 2 （瘟） acute ...
  • 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 report warns that a temperature rise if up to 5. 8, with the warming of the oceans and melting of polar icecaps, will force sea levels to rise by as much as 3ft, making tens of millions of people in bangladesh and egypt homeless

    報道警告說，若地球氣溫升高5 8攝氏度，隨著海洋變暖和極地冰帽融化，海平面將升高3英尺，幾千萬孟加拉人和埃及人將無家可歸。
  2. The report warns that a temperature rise of up to 5. 8c, with the warming of the oceans and melting of polar icecaps, will force sea levels to rise by as much as ft, making tens of millions of people in bangladesh and egypt homeless. parts of lowland britain are also at risk

    報道警告說，若地球氣溫升高5 . 8攝氏度，隨著海洋變暖和極地冰帽的溶化，將導致海平面升高3英尺，幾千萬的孟加拉人和埃及人將無家可歸，部分英國低地也面臨著同樣的危險。
  3. 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個站點， 45年（ 1951 1995 ）的降水資料，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洋副熱帶高壓的北抬，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） ，西北太平洋副熱帶高壓偏西、偏北，赤道東太平洋海溫多處于下降階段;嚴重乾旱年西北太平洋副高偏東、偏南，赤道東太平洋海溫則處于上升階段
  4. They say other evidence of warming, such as increases in ocean temperatures, shrinking mountain glaciers and the decreasing polar ice cover are consistent with this trend

    他們稱其他證據諸如海洋升溫，山頂冰層收縮，極地冰層減少也與全球變暖大勢所趨一致。
  5. As a result, a hotter ocean leads to fiercer typhoons and hurricanes

    因此，海洋溫度升高，導致更加劇烈的臺風和颶風。
  6. However, experts say that the biggest threat from climate warming caused ocean temperatures

    不過專家說，最大的威脅來自於氣候暖化引發海洋溫度上升。
  7. ( 5 ) the spring greenland sea - ice extent is larger ( smaller ) : then during the following summer the high of the japanese sea is stronger ( weaker ), and the low of the asian land is stronger ( weaker ), which make the pattern of low west and high east easily ( uneasily ) form ; the ascending movement over north china is strengthened ( weakened ) ; the summer monsoon of east asia is stronger ( weaker ), then the southeastern, warm and damp airflow towards the north china is stronger ( weaker ), and the cold airflow of the high level over the north china is also stronger ( weaker ), which make the convergence of the cold and warm air over north china easily ( uneasily ) form ; the sst of the east pacific ocean is lower ( higher ), while the sst of west wind drift is higher ( lower )

    （ 5 ）春季格陵蘭海冰面積偏大（小） ：後期夏季日本海高壓偏強（弱） ，而大陸上低壓也偏強（弱） ，易（不易）形成西低東阻的形勢；華北地區的上升運動增強（減弱） ；東亞夏季風偏強（弱） ，向華北地區輸送的西南暖濕氣流偏強（弱） ，而對應高空華北地區上空冷空氣活動偏強（弱） ，利於（不利於）華北上空冷暖空氣的交匯；夏季赤道東太平洋海溫偏低（高） ，西風漂流區海溫偏高（低） 。在以上的環流背景下，華北夏季降水偏多（少） ，易澇（旱） 。
  8. Genetic analysis shows that it may be caused by the difference of the response of each area to winter monsoon ' s abnormal, the kuroshio and our offshore is influenced mostly by heat flux between the sea and atmosphere, but in the other areas, the abnormal current incited by abnormal wind has decisive effect on the change of the sea temperature, at the same time, air pressure also has some impact on the sea temperature

    其區域性形成的原因主要可能是因為各海區對冬季風異常的響應方式不同，強冬季風使得黑潮與我國近海海洋過多散熱，海溫降低；在西北太平洋暖池北部，強冬季風引起西風異常，從而引發異常氣旋性環流，海水輻合下沉加熱其表層以下海水，同時異常環流使得更多東側異常暖水向西加熱其表層水；在黑潮與親潮交匯處的升溫也主要是由於強冬季風導致的流場異常，海水輻合下沉升溫。
  9. At cheung chau, no significant temperature rise is found since the 1970s, indicating that changes in temperatures over the seas around hong kong is small

    至於長洲的氣溫，自七十年代至今無顯著上升，顯示香港周圍海洋上的氣溫變化甚微。
  10. The computer models combine information on ocean warming, sea surface temperatures, wind and rainfall levels

    計算機模型結合海洋升溫信息，海平面溫度信息，風和降雨量信息。
  11. " we ' ve long suspected climate change is driving disease outbreaks. our results suggest that warmer temperatures are increasing the severity of disease in the ocean.

    我們很久之前便推測氣候變遷是疾病爆發的主因，我們的報告指出，溫度上升造成海洋中的珊瑚病情加重。
  12. The fifth is the observation in reality of a predicted link between increased sea - surface temperatures and the frequency of the most intense categories of hurricane, typhoon and tropical storm

    第五，觀察資料顯示：海洋表面溫度的持續上升和最高級別颶風、臺風以及熱帶風暴的發生頻率之間存在著可預測關系。
  13. The assessment in a draft international report by the un intergovernmental panel on climate change ( ipcc ) warned coral bleaching would become more common on the reef as the ocean became warmer and more acidic

    聯合國跨政府氣候變遷小組在一份國際性的報告草案中警告，當海洋溫度上升、酸度增加，珊瑚的白化會更普遍。
  14. 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個站點， 45年（ 1951 1995 ）的降水資料，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洋副熱帶高壓的北抬，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） ，西北太平洋副熱帶高壓偏西、偏北，赤道東太平洋海溫多處于下降階段;嚴重乾旱年西北太平洋副高偏東、偏南，赤道東太平洋海溫則處于上升階段
  15. When the indian ocean sst is positive ( negative ) anomaly, the rainfall increases ( decreases ) inspring, march and may ; when tropic middle - east pacific sst is positive ( negative ) anomaly, the rainfall increases ( decreases ) in spring and may

    當赤道印度洋海溫異常升高（降低）時，華北春季及3 、 5月降水偏多（少） ；當熱帶中東太平洋海溫異常升高（降低）時，華北春季、 5月降水偏多（少） 。
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