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The project will make full use of Cretaceous marine, terrestrial strata and paleontological records.

项目将充分利用中国大陆发育完好的白垩纪海相、陆相地层及古生物记录,通过松辽盆地白垩系科学钻探全岩芯取样和多学科综合研究的途径,着眼于厘定反映地质事件和气候变化的层位及标志和时间格架,解决高分辨率海、陆相沉积事件的精确对比,分析地层记录中气候标志和古生物类群的地理分布,集中研究陆地和海洋环境对同一事件的响应机制,重溯白垩纪地球表层系统重大地质事件过程及成因,探究陆相烃源岩大规模形成、陆地生物群更替与温室气候变化和碳循环之间的正/负反馈关系和机制等科学问题,为预测全球长时间尺度上的气候变化趋势提供科学依据。

The results show that the jump is the most important characteristic for climate change and the periodicity is secondary.

结果表明:突变性是气候变化最重要的特征,周期性是第二位的;突变在气候变化的高层次上有显著反映,低层次对突变具有反馈作用,正反馈作用突出气候变化的突变性;并且在气候诊断分析中,这是一种有特色的方法

After decreasing wavelet transformation s boundary effect, the prediction law and assessment standard are put up based on the theory of climatic hierarchy and wavelet analysis.

论述了子波气候诊断中的边界效应和非周期性对趋势预报的影响,在消除子波变换边界效应基础上,将气候层次理论和子波诊断技术相结合,提出了气候多层次趋势预报法则和评判标准,最后利用若干气候资料进行了多层次趋势预报。

He also extended quasi-geostrophic non-acceleration theorem to primitive equation non-acceleration theorem.

他在国际上首创湿倾斜涡度发展理论和全型垂直涡度方程,成功地揭示青藏高原西南涡和夏季江淮流域的暴雨发展机理,揭示副热带高压形态变异的成因;证明创新的原始方程中的无加速定理以及大气运动的动力强迫和热力强迫的调配率;开展创新性气候动力研究,揭示中高纬和热带海气相互作用差异的机理及厄尔尼诺影响台风频率的机制,继承和发展了我国学者关于青藏高原对大气环流和天气气候影响的研究;在国际上首次把亚洲季风爆发分为三个阶段,证明由于中高纬度的强地转性和斜压性使其海气相互作用的特征与热带显著不同;首次用数值模式提出厄尔尼诺影响台风的机制,得到国际上的高度评价。

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。

Based on the two proxies of climate change - tree-ring and stalagmite, combining them with the historical documents, the author discusses the history and effects of climate change about 200 years in Kunming, In this dissertation, the author infers the possibility of climate change for the next five years, ten years, and fifty years; Then get a Synthetic result of historical climate change.

在对树轮和石笋这两类气候变化自然代用资料研究的基础上,结合历史文献资料,分析了近200年昆明地区气候变化的历史和影响,并对昆明地区未来5年、10年和50年气候变化的可能性进行推测,形成了这三类资料支持之下,对历史气候的集成研究成果。

To summarize molecular, morphology, chromosome and pollen characters, the conclusion was reached that Epimedium was an nd monophyletic taxon. To divide the genus into any groups would be artificial. It is proposed that the disjunction by space, climate and seas were the main reason of respectively differentiation of each group by the view of geographic and climate changes in the temperate zone of the world. Because of its evolution-conservation, the disjunction did not bring about obvious divergence on the level of molecular and morphology.

综合分子特征和形态、细胞学、孢粉学等性状,提出淫羊藿属是一个进化上极为保守的、自然的单系的植物类群,进行属下任何阶元的划分都将是人为的,从旧世界温带的地质变化及气候变迁的角度推测,空间、气候和海洋的隔离是产生类群各自分化的主要原因,但由于其进化上极度保守,这些隔离尚未产生出类群间形态上和分子水平上的明显趋异。

Spring weather in previous years to pick this year is middle of the climate, though a few days after May 4, poor weather, continuous rain, but spring a few days to pick the most crucial May 2-4 is fine the weather is good the middle of the season, the Yu Garden, general manager of tea tree An told reporters that won this year's spring days, the key to a good climate for a few days Tieguanyin quality spring conditions given birth.

与往年春茶采摘气候相比,今年的气候属中等偏上,虽然5月4日后几天,气候不佳,阴雨绵绵,但春茶采摘最关键的几天5月2日至4日是晴朗天气,是产好茶的时节,裕园茶业总经理林木安告诉记者,今年的春茶赢得了天时,关键几天的好气候为铁观音春茶品质赋予了先天条件。

Based on the data analysis and numerical simulation, the Arctic sea ice climate variability was researched, the result were as following:(1) The analysis on the seasonal cycle of the Arctic Ocean and atmosphere showed that: The seasonal surface wind is somewhat trade wind like in some regions in the Arctic. The surface air temperature is robustly determined from the underlying environments such as sea ice and Greenland glaciers. In the sea ice region the precipitation rate is larger than that of evaporation. Furthermore, the Arctic Ocean hydrology is profoundly influenced by the surrounding rivers discharge. These are the decisive factors on the ocean salinity pattern. Sea ice flux through the Fram Strait is larger in winter than in summer. From the 40s in the 20th century on, the ice volume flux has an increasing trend. The Arctic rivers flood season is about the melt period, the winter rivers discharge has a significant increasing. Correlation analysis shows that 7 to 10 years is a characteristic time scale that rivers discharge leads Fram Strait ice volume export.(2) Considering 9 major arctic rivers, the Arctic Ocean circulation was simulated through BOM. The result shows that: The BOM can reproduce the main Arctic Ocean circulation pattern. The"Islandization"which is commonly used in OGCMs to treat the North Pole, not only influences the ocean current near the pole, but also influences the current in the Northern Atlantic Ocean, thus the bogus island might influence global climate through thermohaline circulation in the Atlantic Ocean.

在资料分析和数值模拟的基础上,对北极海冰的气候变率进行了深入的研究,结果如下:(1)对北极地区大气和海洋季节循环特征的分析表明,气候平均风场在部分地区具有&信风&的性质;而气温场与海冰分布及格陵兰半岛冰原的下垫面特征有密切关系;在北极海冰区的降水量大于蒸发量,并且在全球大洋中北冰洋受到河流径流的影响最大,对北冰洋的盐度分布有决定作用;通过弗瑞姆海峡的海冰通量在冬半年大于夏半年,并且从20世纪40年代起,海冰的体积输送有增加趋势;北极河流的汛期主要在融化季节,冬季的河流流量有显著增加的趋势;相关分析表明7到10年是北极河流流量影响弗瑞姆海峡海冰体积输送的一个特征时间尺度;(2)采用BOM海洋模式对北冰洋海洋环流进行了模拟研究,在模式中考虑了北极9条主要河流的作用,结果表明该海洋模式可以较好模拟出北冰洋海洋环流的基本特征;多数大洋环流模式采用&北极岛化&的方法处理北极点,模拟结果表明&北极岛化&不仅影响到极点附近的海流,还会对相对较远的北大西洋海流造成影响,并可能通过大西洋的热盐环流对全球气候产生影响;(3)采用CSIM4海冰模式对北极海冰的气候态进行了模拟。

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