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vegetation and climate
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  “vegetation and climate”译为未确定词的双语例句
     Evolution of Vegetation and Climate in the past 6500 Years on Chongming Island
     崇明岛地区6500年以来植被、气候演化
短句来源
     Study on the Relationship between Vegetation and Climate in China Using Factor Analysis
     基于因子分析方法的中国植被NDVI与气候关系研究
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     Bysporopollen analysis and ̄(14)C dating of the Atherurus macrourus dunghill in the Zhijin caveof Guizhou,it is reflected that the paleovegetation and paleoclimate in the cave area during last6710±130 years belong to the northern subtropical vegetation and climate.
     通过对贵州织金洞扫尾豪猪粪堆积层孢粉组合分析研究及 ̄(14)C年龄测定,明显地反映出织金洞地区近6710±130a来的古植被和古气候均属北亚热带的植被面貌及气候特征。
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     Based on the analysis of palynological assemblage in the piston core CSH1, DOC024 and Y179, combined with other methods such as oxygen and carbon isotopic compositions of foraminifer and AMS14C analysis results, the history of vegetation and climate variation in the middle-north part of Okinowa Trough were reconstructed in this paper.
     本文拟通过分析取自冲绳海槽北部与中部的三个柱状样DOC024、Y179及CSH1中的孢粉组合,结合浮游有孔虫氧、碳同位素数据、AMS~(14)C测年结果和已有的研究资料,对冲绳海槽中、北部地区末次冰期以来的古气候进行恢复。
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     In order to study the vegetation and climate related to the East Asian Monsoon System around 2.5MaB.P.
     为了重建东亚季风区域2.5MaB.P.
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  相似匹配句对
     vegetation degradation;
     植被退化;
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     THE VEGETATION OF PEKING
     北京市的植被
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     《HANDBOOK OF VEGETATION SCIENCE》
     《植被科学手册》——一套在林学上具有很大价值的世界学术名著
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     Ecology,Vegetation and Spring
     生态·植被·泉水
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     FEEDBACK OF VEGETATION ON CLIMATE
     植被对于气候的反馈作用
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  vegetation and climate
The first CCA axis represented the variation of vegetation and climate along the latitude gradient, while the second CCA axis the variation along the longitude gradient.
      
This study addresses the relationships between vegetation and climate of this area quantitatively at a large-scale, in order to determine the factors that control vegetation distribution.
      
Relationships between vegetation and climate on the Loess Plateau in China
      
Secondly, it appears from evidence in northern Scotland that at an ecotone between forest types, the relation between vegetation and climate is likely to be obscured except in regions of uniform soils.
      
The paper reports on the relationships between vegetation and climate in the Upper Catchment area of Narmada river in Central India.
      
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Based on the spore-pollen assemblages of the Holocene,the presentpaper deals with the change of the vegetation and climate of the Maha-nshan region during the past 8,340 years.The microfloral material stu-died here was collected from a natural section which is only 2.7m in thick-ness and lies at 3,560m above sea level of the northern slope of the Mt.Mahanshan.The micsofloralindicates that that the climate during theHolocene of this region underwent the following stages:little warm anpwet,little temperate,warm...

Based on the spore-pollen assemblages of the Holocene,the presentpaper deals with the change of the vegetation and climate of the Maha-nshan region during the past 8,340 years.The microfloral material stu-died here was collected from a natural section which is only 2.7m in thick-ness and lies at 3,560m above sea level of the northern slope of the Mt.Mahanshan.The micsofloralindicates that that the climate during theHolocene of this region underwent the following stages:little warm anpwet,little temperate,warm and wet,warm and wet,little temperateand dry,temperate and wet,and cool and wet respectively.

本文仅从马啣山北坡海拔3560米处,在2.7米厚的剖面中取得的孢粉分析资料.首次揭露出距今约8340年来,马啣山地区的植被变化,并推测出气候由较暖湿—较温湿—暧湿—较温干—温湿—凉湿的变化.

Based on palynological assemblages of 3 cores and the result of cluster analysis, the Late Quaternary palynological assemblages in the Pearl River Delta, can be divided into 5 spore and pollen zones in the following ascendant order.1. Pinus-Castanea-Gramineae-Polypodiaceae spore and pollen zone.2. Castanopsis-Castanea-Elaeocarpus spore and pollen zone.3. Castanea-Cyclobalanopsis-Gramineae-Polypodiaceae spore amd pollen zone.4. Castanopsis-Lithocarpus-Elaeocarpus-Polypodiaceae spore and pollen zone.5. Pinus-Castanopsis-Gramineae-Dicranopteris...

Based on palynological assemblages of 3 cores and the result of cluster analysis, the Late Quaternary palynological assemblages in the Pearl River Delta, can be divided into 5 spore and pollen zones in the following ascendant order.1. Pinus-Castanea-Gramineae-Polypodiaceae spore and pollen zone.2. Castanopsis-Castanea-Elaeocarpus spore and pollen zone.3. Castanea-Cyclobalanopsis-Gramineae-Polypodiaceae spore amd pollen zone.4. Castanopsis-Lithocarpus-Elaeocarpus-Polypodiaceae spore and pollen zone.5. Pinus-Castanopsis-Gramineae-Dicranopteris spore and pollen zone.The vegetation succession and climatic fluctuation phase representing the different climatic epochs, reflected by these spore and pollen zones since the Late Pleistocene in the region of the Pearl River Delta are as follows:Phase I . Northern subtropical evergreen and deciduous mixed broadleaf forest and temperate climate,corresponding to the Middle Wurm Sub-postglacial; Phase Ⅱ. Middle subtropical evergreen broad-leaf forest and warm climate, corresponding to the Late Wiirm Sub-poStglacal; Phase Ⅲ .Vegetation and climate in the early and late phase being similar to that of phase I and phase Ⅱ. corresponding to the Late Wiirm Glacial and the Rising Temperature Epoch of Early Holocene; Phase Ⅳ. Southern subtropical evergreen seasonal rain forest and hot climate; corresponding to the High Temperature Epoch of Middle Holocene; Phase V. Vegetation and climate of this phase being equal to that of the present, namely the Lowering Temperature Epoch of Late Holocene.

本文对珠江三角洲三个钻孔的样品作了孢粉分析。根据孢粉组合,初步探讨了珠江三角洲地区的植被演替规律和气候变化趋势,从而为古环境的研究和地层的划分提供了依据。

On the basic of on-the-spot investigation and a large sum of first-hand maiericals obtained thereby the article analyse the geological features of the mountain and its landform. holding that Mt.Maza-Tageh is a monocline mountain formed after hold and uplift.Back to the early Tertiary Period this region was still a bay,After the start of the Himalayar Movement, especially during the new structural movement in the Quaternary Period, this block uplifted, confronting with sand accumulation in the Taklamagan Desert,...

On the basic of on-the-spot investigation and a large sum of first-hand maiericals obtained thereby the article analyse the geological features of the mountain and its landform. holding that Mt.Maza-Tageh is a monocline mountain formed after hold and uplift.Back to the early Tertiary Period this region was still a bay,After the start of the Himalayar Movement, especially during the new structural movement in the Quaternary Period, this block uplifted, confronting with sand accumulation in the Taklamagan Desert, and eve-tually becomes an insular mountain in the hinterland of the desert.Its topographical effect produces great influence on devision of the geographical environment-geological structure, hydrology, sand form, vegetation and climate And the mountain itself is a division line

在实地考察基础上,讨论了沙漠腹地麻扎塔格山地质地貌的基本特征,并分析了其在地理上的意义。

 
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