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气候转暖
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  climate warming
     Influence of Climate Warming and Human Activity on Relationship between Precipitation and Runoff for Middle-Small River of Northern Xinjiang
     气候转暖及人类活动对北疆中小河流降水-径流关系的影响
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     Finally, the stability and durability of buildings are discussed, and the related strategies are given under climate warming.
     在此基础上,讨论气候转暖后建筑物稳定性的变化及相应的对策。
短句来源
     (4) The relationship between natural precipitation and runoff of Kaiken river located in the north of eastern Tianshan mountains changed and the natural surface runoff decreased under the background of climate warming during 1980s~1990s and influence of human activity.
     ④天山东部北坡的开垦河,在80~90年代气候转暖及人类活动影响的背景下,其自然降水-径流关系发生了变化,产流量减少。
短句来源
  climatic warming
     Mean air temperature warmed by 0.2℃—0.4℃ in the 1980s than in the 1960s in the Qinghai—Xizang plateau, climatic warming results in regional degradation of permafrost along the Qinghai—Xizang highway.
     青藏高原70年代比60年代的平均气温升高0.2~0.4℃,气候转暖导致目前公路沿线浅层多年冻土多呈退化趋势。
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     However, because the current eco-environment situations retroact eco-environment evolution, the climatic characteristics are dry and warm in the early stage of changing of global climatic warming.
     然而,西北地区现实的生态环境又反作用于生态环境的演化,使得该区在全球气候转暖的初期阶段,暖干化现象非常明显。
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  “气候转暖”译为未确定词的双语例句
     Permafrost area of Qinghai-Tibet Platean is 1. 5x106 km2,70 percent of permafrost area in China. On the basis of global warming, there is a degradation tendency for permafrost.
     青藏高原地区冻土分布面积达1.5×10~6 km~2,占我国多年冻土分布面积的70%,在全球气候转暖的背景下,多年冻土有着退化的趋势。
短句来源
     Therefore the δ18O profiles of ice cores mainly reflect the history of palaeomonsoon in China.
     因此,我国季风气候区冰芯的δ~(18)O曲线主要反映古季风的盛衰进退,即冰芯的低δ~(18)O值对应的是夏季风盛行,气候转暖,降水量增加,夏季风前锋北移;
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     The climate of Holocene is warm, especially in the Middle Holocene.
     在第四纪气候中,全新世是气候转暖期,尤其是全新世中期为其最暖期,然而在温暖期中,却普遍发现有短暂的降温时期,世界各地均有存在。
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     Under conditions of global climatic changing warming, it is becoming focus to research evolution trend of Eco-environment in Northwest China now.
     在全球气候转暖的大环境下,西北地区生态环境演化趋势是目前研究的焦点。
短句来源
     Some results are concluded: (1) The climate bef ore 12 ka BP was colder and drier than that in Holocene;
     12~10kaBP气候转暖湿;
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  相似匹配句对
     Some results are concluded: (1) The climate bef ore 12 ka BP was colder and drier than that in Holocene;
     12~10kaBP气候转暖湿;
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     the climate became warm and 9~5 kaB.P.
     以来气候开始转暖 ,9~5kaB .
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     Climate of Uncertainty
     不确定的气候
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     Climates of North America
     《北美的气候
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  climate warming
Morphophysiological monitoring of winter wheat in spring in the context of global climate warming
      
Findings of three relatively large warm-water Pacific species near Point Hope in the Chukchi Sea are probably indicative of the progressive climate warming during the last century.
      
A large part of the fauna is represented by the species of more southern origin, whose expansion to the northern taiga was caused by anthropogenic transformation of landscapes between the 12th and 20th centuries and recent climate warming.
      
Trends of changes in the floristic composition of forest vegetation in the northern Baikal region upon climate warming
      
These changes are explained by climate warming and increasing humidity.
      
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  climatic warming
In the present age, apparent differences of climatic warming have been observed in the Q-T Plateau, indicating that the warming in high-elevation regions is much higher than that in low-elevation regions.
      
Climatic warming would have a positive influence in Northeast China, but high temperature stress may be produced in some regions of central and southern China.
      
Influence of climatic warming in the Southern and Northern Hemisphere on the tropical cyclone over the western North Pacific Oce
      
The results showed that with the climatic warming in both hemispheres, the frequency of the tropical cyclone over the western North Pacific Ocean reduces and its intensity weakens simultaneously.
      
Since 3 kaBP, the aeolian activity and sandstorms have been enhancing due to the combined influences of climatic warming and illogicill exploitation of land and water resources.
      
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On the Qingdao coast, two layers of Quaternary sediments are recognized, the lo- wer part consisting of upper Pleistocene alluvium and alluvium-diluvium and the up- per part Holocene marine facies and sea-land transitional facies deposits. Results of the study on coastal geomorphology, sedimentary strata and inferred paleography suggest that before the late Upper Pleistocene Qingdao was under a ter- restrial environment consisting mainly of mountainous region of medium-low height and denudated hills while the...

On the Qingdao coast, two layers of Quaternary sediments are recognized, the lo- wer part consisting of upper Pleistocene alluvium and alluvium-diluvium and the up- per part Holocene marine facies and sea-land transitional facies deposits. Results of the study on coastal geomorphology, sedimentary strata and inferred paleography suggest that before the late Upper Pleistocene Qingdao was under a ter- restrial environment consisting mainly of mountainous region of medium-low height and denudated hills while the Jiaozhou Bay and the Dingzi Bay etc. were inland ero- sional basins. In the early Holocene about 8000--12,000 years ago the Huanghai Sea transgressed into this area leading to the formation of the present shallow shelf sea and gulf. At the beginning of the middle Holocene some 8000 years ago, transgres- sion reached to the present coastal zone and extended along low and flat river valleys and intruded about 5--20 km to inland area which caused the formation of the estu- ary of Dingzi Bay and the ancient Mawan Bay etc. At the time of the highest sea le- vel, sea water intruded onto coastal land less than 5 m in height, where the paleoco- astline was generally 5 m high during the Holocene transgression. The 5 m high iso- pleth indicates the ancient coastline. At about 3000--4000 years ago, as a result of the lowering of sea level and of the deposition of terrigenous silt into the sea, sea wa- ter was forced to retreat to a location near the present coastline. Results of sporo-pollen content of Quaternary sediments indicate that there are 4 sporo-pollen assemblages connected to different environments. From top to bottom, they are as follows: Zone I, Chenopodiaceae-Artemisia-Compositae-Polypodiaceae; Zo- ne Ⅱ. Chenopodiaceae-Artemisia-Quercus-Pinus Zone Ⅲ, Quercus-Chenopodiaceae-Pinus- Pleistocene (Zone Ⅰ) vegetation consisted ofe-Pinus-Quercus-Sparganiaceae. From the characteristics of sporo-pollen assemblages shown in the Late Upper Pleistocene (Zone Ⅰ)vegetation consisted of saline meadow, sparse trees and herbal plants, and the climate was dry and cold, but turned warm and damp during the Ho- locene (Zone Ⅱ, Ⅲ and Ⅳ), vegetation was luxuriant than ever, upland-hill zones were covered with forest of deciduous, broad and coniferous leaves, plain and river valley zones with trees and grasses. The three different Holocene sporo-pollen assem- blage zones are characteristic of warm-cold and rather dry in the early Holocene, warm and damp in the middle Holocene and warm and cold and rather damp in the late Holocene.

本文通过微体古生物和孢粉分析,岩相古地理研究和海岸地貌调查资料,探讨了青岛沿海地区20,000年以来的海陆变迁和古植被古气候的演变规律。在距今12,000—11,000年前,由于气候转暖,全新世陆架海侵使晚更新世末期的平原和盆地变成浅海和海湾。8000—5000年前出现高海面,5m等高线构成全新世海侵最大范围的古海岸线。自3500年以来,气温降低,海面逐渐下降至现代海岸线附近。

The fossil diatom in the Yellow Sea since the Late Pleistocene can be divided into five diatom zones in ascendant order.

黄海更新世晚期以来的硅藻化石,自下而上可划分为五个硅藻带。在Ⅰ带的上下层位,各含一个淡水藻类化石带,显示黄海在大理冰期时,由于气候变冷,海面下降,黄海陆架三次出露成陆。亚间冰期时,气候转暖,海面回升,复为海水淹没,海域中生长着Ⅰ带的各种海生硅藻。随着全新世气候转暖,沉积物中发现Ⅱ—Ⅴ带海生硅藻带,其中Ⅲ带硅藻外洋种比例较大,含亚热带暖海种多,表明此时水温较大,海域扩大,相当于大西洋期,其他各带与全新世各期相当。

Concerning the understanding of the "Yunmeng Swamp", there are various versions in history but all of them indicate that there used to be a large "Yunmeng Swamp", which basically coincides with the results gained by geoscience analysis that a wide-area limnal land actually existed in palaeogeography. The writer pays attention to the fact that the historical geography recorded in history conforms with palaeogeography while studying relationship between palaeogeography and"Yunmeng Swamp" in Jianghan plain. This...

Concerning the understanding of the "Yunmeng Swamp", there are various versions in history but all of them indicate that there used to be a large "Yunmeng Swamp", which basically coincides with the results gained by geoscience analysis that a wide-area limnal land actually existed in palaeogeography. The writer pays attention to the fact that the historical geography recorded in history conforms with palaeogeography while studying relationship between palaeogeography and"Yunmeng Swamp" in Jianghan plain. This will provide experience for studying history and geography by means of geoscience analysis. In te light of geoscience analysis the gluviolake vicissitudes is that because of the cold climate, there did not exist a "~/unmeng Swamp" ten thousand years BP. Later, because of the climate warming up and the rainfall increasing, "Yunmeng Swamp" began to form and develop and itts area ranged more than twelve thousand km2 during 3--4thousand years BP. With the enlargement of the lake area and the decrease of flow-velocity of the fluvial water, the sand and mud silted up continuously, thus causing the reduction of the lake area gradually. By Tang dynasty and Song dynasty the "Yunmeng Swamp" had disintegrated. During recent decades, the lakes are almost on the brink of disappear. The Yangzi River was not originally located at present site but cutting the plain hinterland and running eastward into the sea. With the action of neotectonic movements it migrated gradually southward to the present site in about ten thousand years. In Qin dynasty and Han dynasty, its main branches were Yang, Xia and Yong streams, which were probably the palaeocurrents left by southward migration of the Yangzi River.

本文根据地学分析,一万年前,气候偏冷,“云梦泽”并不存在。后气候转暖,降雨增多,“云梦泽”逐渐形成并发展。在距今3000—4000年前,范围可达12000平方公里。以后,流入其中的江河水流速减缓,泥沙不断淤积。其范围逐渐缩小,至唐宋时期“云梦泽”解体。

 
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