深海溫度 的英文怎麼說
中文拼音 [shēnhǎiwēndù]
深海溫度
英文
abyssal temperature- 深 : Ⅰ形容詞1 (從上到下或從外到里的距離大) deep 2 (深奧) difficult; profound 3 (深刻; 深入) thor...
- 溫 : Ⅰ形容詞(不冷不熱) warm; lukewarm; hot; gentle; mild Ⅱ名詞1 (溫度) temperature 2 (瘟) acute ...
- 度 : 度動詞[書面語] (推測; 估計) surmise; estimate
- 深海 : abysmal sea; abyssal sea; deep sea深海捕撈 deep sea fishing; 深海捕魚 deep sea fishing; 深海采礦 ...
- 溫度 : [物理學] temperature
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In this paper, features of decadal variability and the possible mechanism of sea - air system in the pacific are investigated by using upper - ocean temperature, heat storage and wind stress data, the main results are as follows : the most pronounce decadal sign exists at about 160 meter in depth in the western pacific. there are significant decadal abrupt changes in temperature from surface to deep in the subsurface at about 1980. with different depth in the subsurface, there exist 4 types of abrupt change modes, their generation is closely related to the decadal sign which originates from the east of north pacific and propagates along the south - west subduct ion route
研究表明,太平洋次表層海溫最強的年代際信號在熱帶西太平洋約160m深處,此信號在1980年前後從上至下,先後經歷了一次顯著的年代際突變過程,而且隨深度的不同存在著四種不同的空間突變模態,這四種模態的形成與北太平洋海溫異常的西南潛沉路徑有著密切的聯系。Use low - density aluminum alloy oxide to the first, with the introduction into superior performance ; neiqiang use special vocabulary design let s hear first from the surface temperature is equipped with colour sets, enabling patients to feel comfortable ; pipeline grey colour black red light green light blue pink sea blue purple yellow note : 220 - tone models of the length of 52cm diameter listen first bamboo : 48mm film - based 30mm bell type
採用低密度的鋁合金氧化聽頭,具有優越的導音性能;內腔採用特殊的圓弧設計,且聽頭表面都配有彩色的隔溫套,能使病人使用時感到舒適;管道顏色黑色灰色紅色深藍粉紅淺藍深綠淺綠海藍紫色黃色注:型號220導音管長度52cm聽頭外圓直徑: 48mm膜型30mm鐘型As a result, we find that in winter when the kuroshio is cooler than the normal, at following summer, the continental cyclone deepen and the east asia monsoon strengthen, that the mid - latitude blocking high weaken and zonal circulation develop, the east asia teleconnection of " - + - " is stired up, so that subtropical high weaken and diminish, and tend to east north, tropical monsoon trough strengthen and mei - yu front weaken, and tend to north, meanwhile south asia high weaken and diminish, and tend to eastvnorth, is easy to form eastern region type
結果發現當黑潮海溫冷異常時,後期夏季大陸熱低壓加深,東亞夏季風偏強。中緯度阻塞高壓減弱,東亞地區緯向環流發展,在東亞-西太平洋地區激發「 - + - 」的東亞遙相關型,從而西太平洋副高強度偏弱,面積偏小,位置偏東、偏北,東亞梅雨鋒也偏弱,季風槽則變強,位置偏北。同時南亞高壓偏弱,位置偏北、偏東,易形成東部型。The shallow thermocline distributes in the areas of guangdong, guangxi, fujian and vietnam continental shelf, with obviously seasonal variabilily, and at the same time, in the south and middle areas of nanhai, even in winter when there is no thermocline in the coastal area, there also exists the shallow thermocline
後者廣東、廣西、福建沿海陸架區則與黃、東海相同,表現為季節性溫躍層,有成長、強盛、消衰、無躍層的年周期變化過程。南海深溫度躍層基本屬於水團疊置型,躍層分佈范圍及躍層強度、上界深度、厚度與氣候關系不大。Salinity temperature depth recorder
海水鹽度溫度深度記錄器For example, some of the large sedentary organisms associated with vents are also found at ordinary deep - sea temperatures many meters from the nearest hydrothermal sources
比如,人們在離最近的熱液源幾米開外、處於一般深海溫度的地方也發現了一些與噴口有關系的大型附著生物。In the ocean, the velocity of sound varies with the temperature, salinity, and depth of the water.
在海洋中,音速隨著水的溫度、鹽分和深度而變化。It is evident that their abundance change and preservation are associated closely with these environmental control factors, and high surface nutrient and productivity controlled by the variations of large scale seasonal climate and input of terrestrial detritus
它們與壞境控制因素關系的分析表明,矽藻、放射蟲和海綿骨針豐度的高低及其保存程度與深度、溫度、鹽度和受大規模季節性氣候變化控制的表層海水的高營養和高生產力,以及陸源物質輸入的變化密切相關。If you open an encyclopedia, you can see a variety of bright and beautiful plants. even in the polar regions, icy regions, beaches, deserts, deep oceans, and tropical forests, with temperatures and humidity that most animals and human beings cannot bear there are many bright and beautiful flowers to embellish the world and comfort explorers
翻開百科全書,看到多彩多姿鮮艷美麗的植物,即使在極地冰原海灘沙漠深海熱帶叢林,任何連人類和多數生物都難以生存的溫度和濕度,都有鮮美的花朵探頭來美化世界景觀,撫慰探險旅人的心。The most obvious sea temperature difference appears between 500m and 600m and the variable amplitude in southern hemisphere is larger than that in northern hemisphere
模擬的海溫,海溫溫差最明顯的地方出現在500 ? 600米之間。南半球的變化幅度要大於北半球,到海洋深層,海溫溫差變化不是很明顯。Another difficulty is that similarly dense populations of large deep - sea animals have been found in the proximity of “ smokers ” ? vents where water emerges at temperatures up to 350
另一個難點是人們在水溫高達350的「冒煙噴口」附近發現了同樣高密度的大型深海動物群。As the results suggested, the climatological shift was primarily induced by variability of the air temperature and the decrease of temperature adjacent to the changjiang river estuary was influenced by the run - off of the changjiang river
2 )黑潮:對夏季表層溫度的影響在31on以南,對深層溫度和鹽度幾乎可影響到整個海域,其影響自60年代以來一直呈增強趨勢。Furthermore, many invertebrates that live in the depths of the ocean never experience change in the depths of the ocean never experience change in the chill of the deep water, and their body temperatures remain constant
此外,很多住在深海的無脊椎動物(變溫動物)在寒冷的深水中從未經歷過溫度變化,因為海洋深處的冰冷海水的溫度從沒變化過,所以他們的體溫也是恆溫的。They lowered nets, dredges, bathythermographs, still cameras, water bottles, coring pipes, and current meters
他們沉降下去網、挖掘機、深海溫度測量器、靜態照相機、水瓶、以及取心鉆管和測流計。" the measurement is simple - it only takes about five minutes ", said mr. w. t. chow, senior divisional officer of fsd at chek lap kok. " all we need to do is to use a special bucket to collect some sea water 1 metre down, and take its temperature.
駐守赤角機場的高級消防區長周榮德先生說:量度工作頗為簡單,需時約5分鐘,同事只須利用一個特製提桶,在海水約1米深位置收集樣本,然後讀取它的溫度便可。The climate of this period is almost as warm and wet as the stage 5e of the last interglacial. the mean temperature is 2 - 4 c higher and the precipitation is much larger than that of the today, the holocene which we live in. while in the climatic records of deep ocean, antarctic and greenland ice - core, marine isotope stage ( mis ) 3 is a weakly warm period, though a little warmer than marine isotope stage ( mis ) 2 and marine isotope stage ( mis ) 4, evidently colder than the last interglacial and holocene favorable period
末次冰期中期,即深海氧同位素第3階段的氣候在我國,尤其是青藏高原地區表現出明顯不同於深海沉積物和極地冰芯記錄的特徵:青藏高原古里雅冰芯的~ ( 18 ) o曲線表明3階段存在特強夏季風事件,其氣溫和降水接近於末次間冰期5e階段,超過全新世,其暖濕程度已經達到間冰期的程度;而深海氧同位素3階段在深海、南極、格陵蘭冰芯的氧同位素記錄中均為弱暖期,雖較2階段、 4階段溫暖,但顯著低於全新世大暖期和末次間冰期。Based on the analyses, it was found that if the subsurface warm pool is regarded as the beginning point, the warm or cold signal propagates initially eastward and upward along the equatorial surface of msta to the eastern pacific and stays there several months and then turns north, usually moves westward near 10 to western pacific and finally propagates southward to return to warm pool to form an off - equator closed circuit. it takes about 2 to 4 years for the temperat ure anomaly to move around the cycle. if the smta of warm ( cold ) water is strong enough, there will be two successive el nino ( la nina ) events during the period of 2 to 4 years
) a事件下/負海溫距平信號的分佈和傳播「軌跡」 ,發現如果以暖池次表層為起點,則一般來說,暖水或冷水先是沿赤道的極值深度面向東、向上「傳播」或運動,到達赤道東太平海盆邊界附近后,分別轉向向北和向南運動,然後在南、北緯10左右再折向西運動,並在暖池的經度范圍內再作經向運動傳到暖地,即在南、北半球以赤道為一邊, 「傳播」或運動路徑形成扁的閉合環路,溫度距平運動一圈需時2 - 4年。The eggs were put in an incubator filled with sand collected from their birthplace and kept at 28 to 30 degrees celsius. after two months of incubation, 85 of the 121 eggs collected hatched out baby turtles, giving a hatching rate of over 70 per cent. " the new - born turtles were about 23 grams in weight and five centimetres in carapace length
漁護署護理員將該窩為數一百二十一隻的海龜蛋放置在數個籃內,鋪上從深灣取來的沙,再放進人工孵化箱中,孵化箱的溫度須保持在攝氏二十八度至三十度,兩個月後,成功孵出八十五隻小海龜,孵化率超過七成。Because of the existence of meiyu precipitating cloud band the temperature dv is faint inside the meiyu trough and on account of large - scale prominent terrain available, significant temperature dv occurs on both sides of the trough, leading to the reinforcement of the subtropical high and middle latitude transformed high, and the deepening and narrowing of the trough in the night with the result that the relative intensity and precipitating function of the meiyu frontal rainfall system are changed at day and night, resulting in precipitation dv
由於梅雨雲帶的存在,梅雨鋒低壓槽內溫度日變化很微弱;由於梅雨系統四圍高大地形的存在,梅雨鋒低壓槽南北兩側溫度日變化非常明顯,使南海副高和中緯度變性高壓在夜間增強,梅雨鋒低壓槽也在夜間變深、變窄,改變了早、晚時刻梅雨系統的相對強度和降水功能,導致降水日變化。4. the study on the frozen soil feature and its influence on the runfall of the catchment in qilian mountains. the results indicated that the soil begins to freeze around october 20, and finishes melting around august 20 of next year. altitude slope side, vegetation condition of the land and temperature are the factors influencing the depth and the time of soil
4對祁連山區凍土特徵及其對流域徑流的影響研究表明,祁連山林區土壤每年的10月20日左右開始凍結,較低海拔的到第二年的8月20日左右消融結束;海拔、坡向、植被、下墊面狀況、溫度是影響凍土深度、早晚的制約因素;凍土厚度與徑流量成反比關系。分享友人