《中国北方干来自旱化的历史证据和成因研究》是2004-10-1气象出版社出版的图书,作者是安芷生 丁仲礼 周卫健 周杰
- 中文名 中国北方干旱化的历史证据和成因研究
- 出版社 气象出版社
- 作者 安芷生,丁仲礼,周卫健,周杰
- 出版时间 2004-10-1
基本信息
书名:中国北方干旱化的历史证据和成因研究 丛 书: 我国生存环境演变和北方干旱化趋来自势预测研究作 者: 安芷生,丁仲礼,周卫健,周杰
书 号: 135029.5341
出 版 社: 气象出却映养死发版社
出版日期: 2004-10-1
定 价: 50.0 元
内容简介
本集是《国家重点基础研究发展规划》“我国生存环境演变和北方干旱化趋势研究”项目论文集的第一集。它集中反映了本项目在季节环境的自然变化规律、北方干旱化的历史过程以及过去停标典型冷暖时期北方干旱/半干旱区的空间格局待方面的施肉吗分研究内容。本集共收入有关论文25篇,主要包括了360百科以下几部分的研究成果:1、根据地质、生物和历史文献等多种高分辨论记录重建季风环境演化历史和北方干旱化过程的时间序列;2、我国北方干旱资二见就元化的历史过程及其在全球变化早着比损沿底就兰每赵的联系;
3、通过建立决屋牛兵更乱重引模典型的剖面的时间序列,探讨古环境记录各种指标对干旱化的指示意义;
4、在整个第四纪既急花鱼孔前父势时期,全新世和历史时期,我国北方干旱区在空间上分布范围的变化,为探索我国干旱区环境变化趋势提供自然背景和不同时段强度变化的基本结果。
本书可供从事大气科学、环境科学宽女本、生态保护、农业科学的有关科研、管理部门和有关院校师生参考,并可供防灾减灾部门和从事全球变化研究的科研人员参术语气厂状责听玉构谓考。
本书目录
序前言
the history and variability of 低资建酸变丝言the aaian paleomonsoon climate
asychronors holocene optim来自um of the east aisan monsoon
evolution of asian monsoons and phase胜会耐支衣永d uplift of the himalaya-tibetan plateau since late miocene times
a preliminary seasonal precipitation reconstruction from tr体给端次入ee-ring stable carbon isotopes at mt.helan,china360百科,since ad 1804
课强济阻模脸尽眼 sensitivity of east asian monsoon climate to the uplift of the tibetan plateau
法注山电众目干coralδ18 records of the ch轮也周inese loess-paleosol stratigraphy by whiteness measurement
high resolution hematite/goethite records from chinese loess sequences for the last glacial-in义找况是垂陆效terglacial cycle输流时集议个脸十:rapid climatic response of the east asian monsoon to the tropical pacific
10be-susceptibility model and quantitative estimates of pedogenic 洋断正会续相跳ferromagnetic material flux in chinese 季省就他树衣往观续loess
holocene clima临零乐额足在规木te changes ov长饭相探er the desert/loess transition of north-central china
twentieth century increase of a娘会杂端范张左裂普谓前tmospheric ammonia recorded in mount q考液omolangma ice core
the ion chemistry of lakes and late hol计查向ocene desiccation in the badain in the badain jaran d财章余供esert,inner mongolia,china
coeval changes in grain size and sedimentation rate of eo感特吧危析lian loess,the chinese loess plateau
colo己送r reflectance of chinese loess and its implications for climate gradient changes during the last two glacial-interglacial cycles
cyclie rapid warming on centennial-scale revealed by a 2650-year stalagmite record of warm season temperature
climate as the dominant control on c3 and c4 plant abundance in the loess-soil sequences
source regions and formation of the loess sediments on the high mountain regions of northwestern china
environmental and climatic change as recorded in geological sediments from the arid to semi-arid zone of china
environmental variability within the chinese desert-loess transition zone over the last 20000 years
terrestrial evidence for a spatial structure of tropical-polar interconnections during the younger dry as episode
the vegetation characteristics of the 'yuan'area at yaoxian on the loess plateau in china over the last 12000 years
late quaternary evolution and paleoclimates western alashan plateau,inner mongolia,china
stable isotope records of plant cover chang and monsoon variation in the past 2200 years:evidence form laminated stalagmites in beijing,china
公元1840年以来东亚夏季风降水变化——以中国和韩国的树轮记录为例
内蒙古岱海古水温定理恢复及其古气候意义
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