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climate changes
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  气候变化
     The spectral analysis shows that the thermocline depth oscillated in the centennial-scale cycles of ~175 a,~210 a and ~360 a during the late Holocene,probably indicating the association between the centennial scale climate changes and the solar activities.
     频谱分析显示南海晚全新世温跃层具有~175、~210和~360 a等百年尺度的周期,与太阳活动周期一致,说明百年尺度的短期气候变化可能与太阳活动有关。
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     Geochemical Features of a Profile in Salawusu River Valley and Their Response to Global Climate Changes since 220 ka BP
     220ka BP来萨拉乌苏河流域地质剖面地球化学特征及其对全球气候变化的响应
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     The abrupt climate events happened at about 550 AD and 1000 AD are of very important significance in climate changes of southern Xinjiang during the last 2\^0 ka, which indicated that the climate was ever re-arranged greatly.
     550AD和1000AD前后的具突变性质的气候事件在南疆地区近2 0ka的气候变化中具有重要意义,反映气候状况有过重大调整。
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     They are used in microbiology study mainly in microbial diversity,community structure and dynamics,metabolic activity,and the impact of global climate changes to microorganisms.
     这些技术在环境微生物研究中的应用主要包括对微生物多样性的研究、种群结构和动力学的研究、代谢活性的研究以及在全球气候变化中对微生物影响的研究。
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     A comparison of climate changes between Arctic and China in the last 600 years
     近600年来北极与中国气候变化的对比(英文)
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  气候变迁
     Carbon Isotopic composition of Organic Matter in Lugu Lake′s Sediment and the Recording of Climate Changes
     泸沽湖沉积物有机质碳同位素组成与气候变迁记录
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     The Lacustrine Sediments of the Nam Co Basin in Tibet from 116 ka and Related Environmental Evolution and Climate Changes
     西藏纳木错地区116 ka以来的湖相沉积及其环境演化与气候变迁
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     The climate factor distribution coincide very well with the dust storm occurrence frequency distribution, which suggested that the climate changes induced the dust storm downward trend in whole during these 40 years in China.
     结果发现气候因子分布与沙尘暴的发生频次分布对应性很好,提出气候变迁导致在这40年中国沙尘暴整体上呈现出下降趋势.
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     From the 6th to 10th century,the climate of Kaifeng standed in the Third Warm Period of 5000-year progress of Chinese climate changes.
     6至 10世纪处在中华 5 0 0 0年气候变迁过程中的第三个温暖期 ,开封的温暖气候从隋唐经五代 ,一直持续到北宋初年。
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     CLIMATE CHANGES IN LIANGSHAN MOUNTAIN AREAS SINCE 10000 YEARS BEFORE
     一万年以来凉山地区气候变迁
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  气候冷暖
     The organic carbon content change is incompletely consistent with the organic δ ~(13)C change, its height cannot instruct the climate changes in temperature change completely.
     有机碳与氮含量变化有明显的正相关关系,千年尺度的沉积变化以自然有机物质输入影响为主,有机碳含量变化与有机δ~(13)C变化不完全一致,其高低不能完全指示气候冷暖变化。
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     ③Glacier drift epoch and climate changes method;
     ③冰川冰期与气候冷暖方法;
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     of the ancient oceans. Therefore, the study of marine carbonate rock stable isotope composition is of great significance to understanding the changes of paleocean level, tectonic activity, global climate changes, biological extinction, ancient seawater temperature and salinity.
     因此,研究海相碳酸盐岩稳定同位素组成对于了解古海洋平面变化、构造活动、全球气候冷暖变化、生物灭绝以及古海水温度、盐度等具有十分重要的意义。
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  “climate changes”译为未确定词的双语例句
     2.25~0.80m (5.9-2.lka) the temperature decreases dramatically and the precipitation is also lower, with some abrupt climate changes.
     2.25~0.80m(5.9~2.1ka)气温较低,降水量较小,环境出现剧烈波动。
短句来源
     Risks and Countermeasures of Climate Changes
     气候变暖的风险与对策
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     Atlantic Thermohaline Circulation and Abrupt Climate Changes
     大西洋热盐环流与气候突变
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     The climate changes can be divided into three periods:warm(46-44.6?kaBP),cool and wet(44.6-40.6?kaBP),hot and dry(40.6-40kaBP).
     古气候重建结果显示46~44.6kaBP为温凉期; 44.6~40.6kaBP为持续稳定的冷湿期;
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     Study on the Abnormal Long-term Climate Changes and Developing Tendency over Zhoushan Islands
     舟山群岛异常气候长期变化与发展趋势的研究
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  climate changes
The response of the phytocenotic habitats to possible climate changes is estimated from the changes in net primary production for the considered climatic scenarios.
      
The obtained data allowed us to recognize the zonal phytocenoses most sensitive to climate changes.
      
Only such measurements should provide the basis for the discussion of global climate changes.
      
A transfer function model with climatic indices as the input and the lake level as the output is proposed to describe the response of a lake to climate changes.
      
The model is used to assess the response of the Lake Ladoga level to different climate changes.
      
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In semiarid loess hilly region ground-water table is present at a very deep depth. Thus water requirement for growth of plant can not get supplement from ground water. The water in soils within this region is mostly in status of suspended water. Soil water regime was considered as an automorphic -evaporative type, of which was followed by aridization of soil layer. Background of soil water in loess hilly region exist in four characteristics, they were: (1) obvious difference of water content in soils on differental...

In semiarid loess hilly region ground-water table is present at a very deep depth. Thus water requirement for growth of plant can not get supplement from ground water. The water in soils within this region is mostly in status of suspended water. Soil water regime was considered as an automorphic -evaporative type, of which was followed by aridization of soil layer. Background of soil water in loess hilly region exist in four characteristics, they were: (1) obvious difference of water content in soils on differental landform; (2)very active upward evaporation ability of soil water; (3) low water content under field steady moisture;(4) existence of wa- ter storage difficulty in deep soil layer and weakness of regulation ability of soil water for growth of plant. Therefore under the automorphic -evaporative type of soil water regime as a result of action of man- made vegetation the aridization of soil layer is further intensified, of that formed "complex dry soil layer" or" overlapping dry soil layer". As the dried soil layer due to the absorption by roots of trees and shrubs is formed, its soil moisture is difficultly restituted to field capacity through the short-term or long-term compensation of rain water. Therefore forest planting and grass cultivating are situated under a unfavourable soil water ecological envi- ronment. According to bioclimatic circumstance the northwestern part of loess hilly region is located in the steppe zone; its centre and southern part-the forest steppe zone. Thus the climate changes increasingly arid to the west. The soil conditions for plantation as well changes unfavourably in this direc- tion. In steppe zone shrubs which has best adaptation to arid circumstance should be planted. In the forest steepe zone it may be recommended to use complex porest type to protect against soil erosion and to solve the problem of fuel shortage. For raising efficiency of soil water use in the loess hilly region the wasteland is best changed to man-made grassland. This measure is an optimum method of efficiency useing soil water resources. At the same time it may be to improve fertility of soil and to increase grass yield.

黄土丘陵区的土壤水分状况属蒸发自成型水分状况,伴随有土层的干燥。在人工林草植被作用下,土层将会进一步向干燥化方向发展,从而形成“复合干层”或“重叠干层”。土壤水分的短期或长期补偿,都难以使其土壤湿度恢复到田间持水量状态。草原地带应以建造适应性强的灌木为主,森林草原地带着重建造防护-薪炭互补的防护林体系。改撂荒地为人工草地,是经济利用土壤水分资源、提高土地生产率的优化措施。

The quick-action of depilation chemically and the priciple of regenerating hair are described in this paper. According to the compatibility of medicines, cold-waving lotion and depilating agent are composed ingeniously and the resuting prescription of the quick-acting depilating agent is screened. The climate-change-resisting toxicity and clinical experiments of the product indicate that the rate of depilating hard hair of human body is 3—8 minuts, which is the same as the high-quality product abroad...

The quick-action of depilation chemically and the priciple of regenerating hair are described in this paper. According to the compatibility of medicines, cold-waving lotion and depilating agent are composed ingeniously and the resuting prescription of the quick-acting depilating agent is screened. The climate-change-resisting toxicity and clinical experiments of the product indicate that the rate of depilating hard hair of human body is 3—8 minuts, which is the same as the high-quality product abroad and has not been reported previously in china.

本文从理论上阐述了化学脱毛的速效性和毛发可以重新生长的机理。根据药物配伍规律,将冷烫剂和脱毛剂配方进行巧妙结合,筛选出了速效脱毛灵配方。研制产品经耐候性、毒性和大面积临床试验证明,脱除人体硬长毛,其速度为3~8分钟,脱除生毛速度为3~5分钟,与国外优质脱毛剂相同。大面积用于临床备皮脱毛,国内未见报道。

This paper reviews the trend of change on global surface mean temperature in recent 100 years,analyses the major causes of global climate change,especially the effects of CO2 and other trace gases on climate .The global climate would be more warm with one climax following another in future decades.This paper also demonstrates the effects on environment of the possible warming.

本文论述了近百年来全球地面平均温度的变化趋势,分析了全球气候变化的主要原因,尤其是CO_2及其他痕量气体对气候的影响,指出在今后几十年和21世纪,世界气候可能会在不断波动的情况下趋于变暖,并论述了这种增暖可能造成的环境后果。

 
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