暖气候

词组短语

warm climate

与暖气候相关的网络例句 [注：此内容来源于网络，仅供参考]

The chondrite normalized distribution patterns of REEs are characterized by light REE enrichment and Eu depletion with terrestrial sedime...

约 1 740年以前，陆相特征明显，气候干燥、寒冷，但是，1 5 5 0年左右有一暖期。1 740年后，出现海侵，巴罗气候变暖，1 82 1年后，变暖较明显，1 890年左右为低谷。1 90 4年持续变暖，1 971年左右，有一变冷阶段

The present project of "deepsea processes and records" targets at the ignored aspects of the theory. Combining the geological records with climatic numerical modeling, we recognized the stepwise process of development of the "Western Pacific Warm Pool" and the East Asian monsoon system, and found that the sea surface warming in the Warm Pool was leading the melting process of the boreal icesheet during the deglaciation.

本项目以"西太平洋暖池"为重点，通过地质资料和气候数值模拟的结合，揭示了"西太平洋暖池"和东亚季风发育的阶段性，发现了暖池海区冰消期表层水升温超前于北半球冰盖的融化。

Three preliminary conclusions could be approached as follows:(1) SST changes were distinctively characteristic of stepwise fluctuations. A warming trend during the last deglaciation was punctuated by a slightly cooling event which corresponded to the Younger Dryas. The Holocene episode could be divided into three phases of warming, continuously high temperature and cooling.(2) Two remarkable cooling records were documented around 4 kaBP and 1.5 kaBP after the megathermal of the Holocene.(3) Comparison between time series of MD05-2904 diatom R SST index and stalagmite δ^18O results from Dongge Cave, Guizhou Province suggested that changes in the East Asian Monsoon climate is synchronous with variations in the SST in the northern SCS since the last deglaciation and they might have a close correlation with each other

结果表明：(1)南海北部15 kaBP以来表层海水温度呈现明显的阶段性波动特点，即末次冰消期气候转暖过程中，12.9~11.5 kaBP前后温度略有下降，与新仙女木事件对应，全新世南海北部气候依次经历了升温期、高温期和降温期3个变化阶段；(2)全新世大暖期鼎盛期结束后，南海北部海水温度阶段下降，两次明显降温分别发生于4 kaBP前后和1.5 kaBP前后；(3) MD05-2904孔硅藻R值时间序列曲线与董哥洞D4石笋δ^18O曲线对比表明，南海北部表层海水温度变化与末次冰消期以来东亚季风强度变化关系较为密切。

The study has shown:(1) With increasing sediment depth and the woody giblets, the total organic carbon, the extraction of benzene , the total humic acids and the unhydrolyte are enhanced, while the hydrolyte is decreasing.(2) According to the GC-MS analysis, n-alkane,n-alkan-2-ones and n-alkanones are composed mainly of long-chains,such a result is thought to be characteristic of a herbaceous input from 2300a.B.P. n-alkanones exist in the samples may be considered as the evidence of microorganisms activity.(3) It is showed that the lipids is more sensitive to the climate change than the floristic. The proxy of the pollen spore of the peat stratum is different from the normal environment proxy. It is one of the main reasons that the sensitivity difference of the bog vegetation reacting to the climate isn't accordant with the log of the fat molecule fossil and biology fossil.(4) The transformation of the peat organic carbon is under the influence of temperature,acidity,organic material constituting, etc, and it showed the up-trend with the depth. In the short-term scale, the conversion of the peat organic carbon is effected by seasonal water,regional climate and vegetations; while in the long-term scale, it is controlled mainly by the climate.(5) According to the comparing the orderliness of organic compound,vegetation giblets with the depth to the characteristics of the peat molecule fossil with the section, in the development of this peatmire, 1500a B.P（210cm）is regard as the borderline of the late Holocene, the keynote of the front period is warm with several cold fluctuations, and the trend of the back period is dry and cold although there were several fluctuations.

研究表明：（1）随深度的增高及植物残体中木本残体的增多，总有机碳、苯萃取物、总腐植酸、不被水解物含量逐渐增高，而易水解物含量减少；（2）GC- MS分析显示，正构烷烃，直链烷基2-酮和正烷醇均以长链组分为主，揭示了该泥炭柱剖面2347a.B.P的母源输入以草本植物为主；甲基酮类和短链正烷醇的存在是微生物活性很大的生物证据；（3）通过有机分子标志物与孢粉、植物残体等指标的对比研究表明：脂类化合物对气候变化的反映要比植物种灵敏得多，不同沼泽植物对气候变化的敏感性的差异是脂类分子化石记录与生物大化石结果很难一致的主要原因之一；（4）泥炭有机碳的转化受到温度、酸度、有机物质组成等很多因素的影响，短时间尺度，泥炭有机碳的转化受季节性降水、地方气候和植被等因素的影响；长时间尺度，泥炭地有机碳的转化，受气候条件控制；（5）总结泥炭分子化石特征、泥炭有机质各组分含量及植物残体组成随深度的变异规律，分析结果显示该泥炭地层形成过程中，1500a B.P（210cm）可作为划分前后晚全新世的界线，前期的基调是气候偏暖，但又有几次偏干冷气候的反复，后期气候以干冷为主，其间虽有几次上升波动，但整体趋势不变。

Except the climate in winter and fresh air that are god-given as well as some delicious fruits like pawpaw, plantain and pineapple that are cheap in season, I cannot see any advantages of the city.

这座城市除了天赐的冬暖气候和清新的空气之外，当然还有天赐气候下的一些物美价廉的水果，例如木瓜，芭蕉和菠萝，其它方面一无是处。

The planet is experiencing a global climate changing, global warming affects distribution, penology and breeding of wildlife. Metrological records indicate that the Qinghai Lake drainage area is also experiencing such a climate change.

随着全球气候变暖，野生动物的分布区、物候期，繁殖等都不同程度受到了气候变暖的影响。

On the basis of pollen analysis of surface sample in North China, polynomial function analysis method was applied to establish pollen climate response surface of Pinus, Betula, Quercus, Artemisia, Chenopodiaceae, Compositae, Picea, Ephedra, Gramineae in North China, therefore an easy and applicable method for reconstructing palaeoclimate and palaeoenvironment with data of fossil pollen was founded; Multi-analysis method was applied to analyse the principal elements of surface sample pollen in central Inner Mongolia Steppe, the assemblages of surface sample pollen in steppe area and its relationship with vegetation type were discussed with helps from spore-pollen analysis of a peat section in Chasuqi, Inner Mongolia and 〓C chronometer, fossil pollen data were obtained with high resolution on the peat section in Chasuqi. Vegetation succession and environmental changes since Holocene at resolution of 70 years were primarily reconstructed in south Mount Daqingshan and Plain Tumete. The changes in the area were copmared with those in the neighbouring areas during the same period. It was found that Holocene environmental change had undergone the following stages: cold-arid, temperate-wet, warm-wet, temperate-arid and cold-arid, and the climatical optimum period occurred in 5000-4100 aB.

本文在对中国北方表土花粉研究的基础上，采用多项式函数回归方法建造了中国北方松属、桦属、栎属、蒿属、藜科、菊科、云杉属、麻黄属、禾本科等的花粉——气候趋势面，从而为利用化石花粉资料直接恢复古气候、古环境提供了一种方便易行的方法；采用多元分析方法对内蒙古中部草原区表土花粉进行了主成分分析，探讨了草原区表土花粉组合的规律及与植被类型的关系；本文还应用孢粉分析方法，结合〓C测年技术，通过内蒙古中部察素齐泥炭剖面高分辨率的化石花粉数据，初步恢复了大青山山地南部及土默特平原地区分辨率为70年的全新世以来植被演替和环境变迁的状况，并与邻近地区的全新世古气候、古环境进行了对比研究，研究发现，本区域全新世古环境的变迁序列基本上可以与周围地区及华北地区进行对比，其环境变迁经历了凉干～温湿～暖湿～温干～凉干的变化，且气候最适宜期出现在5000～4100aB.P。

First of all, retreat of glaciers and shrink of perennial snowbank induced by climate warming provide parent materials and spatial room for soil formation and development in the maritime Antarctica. Meanwhile, melt water originating from glaciers and snow-ice covers enhances temporal and spatial availability of free water, which plays all-important roles both in periglacial processes and the processes within soil profiles, thus influencing soil genesis and evolution to a great degree.

首先，南极海洋性气候区日益加速的气候变暖现象导致冰川消退、地表积雪融化，为土壤形成与分布提供了母质与空间基础；同时，气候变暖导致自由水活动在时间和空间上的加强促进了以自由水为基础的土壤过程和冰缘地貌过程，对南极海洋性气候区土壤发生、发育产生深刻影响。

Everything was contestable, whether it was the cause of climate change or the fact of climate change, the size of the deficit or the culprits to blame for the deficit.

一切都能产生分歧，从气候变暖的原因到气候变暖的事实；从赤字的规模到产生赤字的罪魁祸首。

There were three abrupt warmings,i.e.1910s,1930s and the early of 1980s,of the which the first two occurred in daytime,only the last mainly in nighttime.

近百年上海气候变暖主要表现为三次突然增暖，其中10年代的增暖仅限于白天，30年代则以白天增暖较多，80年代以来则主要发生于夜间。

与暖气候相关的网络解释 [注：此内容来源于网络，仅供参考]

warm braw：暖布劳风

warm anticyclone 暖反气旋 | warm braw 暖布劳风 | warm climate with dry summer 夏乾温暖气候

warm temperate continental climate：暖温带大陆[性]气候

warm temperate climate 暖温带气候 | warm temperate continental climate 暖温带大陆[性]气候 | warm temperate maritime climate 暖温带海洋[性]气候

warm temperate continental climate：暖温带大陆气候

warm temperate climate暖温带气候 | warm temperate continental climate暖温带大陆气候 | warm temperate maritime climate暖温带海洋气候

global warming：全球气候变暖

气候变化(climate change)主要表现为三方面:全球气候变暖(Global Warming)、酸雨(Acid Depostion)、臭氧层破坏(Ozone Depletion),其中全球气候变暖是人类目前最迫切的问题,关乎到人类的未来!

paleoclimatology：古气候学

一代代的科学家们在数据不足的情况下,构拟出了一万年内的气候变化图,并表明自冰河时代结束后的暖期以来,全球气候变化很小. 但近年来,研究古代气候的古气候学(Paleoclimatology)所发生的变革(参见专栏1-1),改变了我们对全新世的认识.

climate warming：气候变暖; 气温升高

climate variation 气候变化 | climate warming 气候变暖; 气温升高 | climate watch 气候监视

climate warming：气候温暖化 気候温暖化

■ cliff 崖 崖 | ■ climate warming 气候温暖化 気候温暖化 | ■ climatic fluctuation 气候波动 気候変動

climate warming：气候变暖

气候变暖:Global Warming | 气候变暖:climate warming | 预警模型:early warming model

warm climate with dry summer：夏干温暖气候

warm braw 暖布劳风 | warm climate with dry summer 夏乾温暖气候 | warm climate with dry winter 冬乾温暖气候

warm climate with dry winter：冬乾溫暖氣候

warm climate with dry summer 夏乾温暖气候 | warm climate with dry winter 冬乾温暖气候 | warm cloud 暖云