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subtropical characteristic
相关语句
  亚热带特色
     Influence and Countermeasure for Guangxi Subtropical Characteristic Agriculture after Joining WTO
     加入WTO对广西亚热带特色农业发展的影响及对策
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  “subtropical characteristic”译为未确定词的双语例句
     Among them, ner-itic low salinity warm community and euryhaline warm community were dominant, which embodied the subtropical characteristic of community structure.
     以沿岸低盐暖水性类群和广盐暧水性类群为主体,体现亚热带性质的群落结构特点。
短句来源
     In the 25 species of arborous layer, 76% is the middle subtropical zonal type, 16% south subtropical zonal type and 8% north subtropical zonal type, of which the first 6 positions of important value index (IVI) were all middle subtropical zonal type. This showed that the community was subtropical characteristic.
     2 5个乔木层树种中 ,中亚热带地理分布类型的占 76 % ,南亚热带地理分布类型的占 16 % ,北亚热带地理分布类型占 8% ,重要值指数排列前 6名的均为中亚热带地理分布类型 ,所以该群落为亚热带性质。
短句来源
     America disjointed. In the dominant species of arborous layer,83% is middle subtropical zonal type,of which the first 4 positions of important value index were all middle subtropical zonal types. This showed that the community was subtropical characteristic.
     乔木层 16个优势种中 ,属中亚热带地理分布类型的有 13种 ,占81.3% ,其中重要值排列前 4位的种类均为中亚热带类型 ,所以元宝山冷杉群落为亚热带性质。
短句来源
  相似匹配句对
     To compare characteristic
     区域产业集群特色竞技
短句来源
     On Characteristic Agriculture
     论特色农业
短句来源
     Influence and Countermeasure for Guangxi Subtropical Characteristic Agriculture after Joining WTO
     加入WTO对广西亚热带特色农业发展的影响及对策
短句来源
     The Micromorphology and Chemical Characteristic of Iron-Manganese Cutans in Typical Subtropical Soils in China
     亚热带典型土壤铁锰胶膜的微形态与化学特性
短句来源
     On Subtropical Zone of China
     关于中国的亚热带
短句来源
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It is found from the data for the period of 1971--1980 that the East-Asian summer monsoon associated with the rain band over eastern Chi-na is of subtropical characteristics and the isodrosotherm of 14°C at850 hPa may serve as a criterion for the monsoon activity. Analysisalso suggests that the monsoon coincides in activity with the subtropicallong waves at 500 hPa.The combination of their seasonal variationswith the quasi 40-day oscillation may cause the northward advance andstagnation of the monsoon...

It is found from the data for the period of 1971--1980 that the East-Asian summer monsoon associated with the rain band over eastern Chi-na is of subtropical characteristics and the isodrosotherm of 14°C at850 hPa may serve as a criterion for the monsoon activity. Analysisalso suggests that the monsoon coincides in activity with the subtropicallong waves at 500 hPa.The combination of their seasonal variationswith the quasi 40-day oscillation may cause the northward advance andstagnation of the monsoon and the resulting rain band while the short-period oscillation may yield their north-south swing during theirstagnant stage.

本文利用1971—1980年的资料分析发现,夏季与中国东部雨带相联系的东亚季风属于副热带性质,850百帕14℃等露点线可以作为它的活动指标。副热带季风活动与500百帕上副热带长波活动相协调,它们的季节性变化与准40天周期振荡相结合可以引起副热带季风及其相伴雨带的北跳和停滞,而短的周期振荡则可引起它在停滞期内的南北摆动。

In this paper, by using data on monthly mean meridional and zonal windfields of global tropical ocean from 1973 to 1989 (ECMF, KWBC), OLR (CAC), and various subtropical characteristic indexes of the western Pacific Ocean, the influence of the wind field variations in the global tropical ocean on anti-Walker circulation between the Indian Ocean and the western Pacific Ocean, equatorial westerly and air current across the equator is studied, and the physical mechanism of their influence on subtropical...

In this paper, by using data on monthly mean meridional and zonal windfields of global tropical ocean from 1973 to 1989 (ECMF, KWBC), OLR (CAC), and various subtropical characteristic indexes of the western Pacific Ocean, the influence of the wind field variations in the global tropical ocean on anti-Walker circulation between the Indian Ocean and the western Pacific Ocean, equatorial westerly and air current across the equator is studied, and the physical mechanism of their influence on subtropical ridge reinforcement and westward extension is discussed as well.

本文主要利用1973年以来,全球热带历年逐月各标准等压面月平均风场(ECMWF,KWBC),OLR(CAC)资料及西太平洋副高各种指数(国家气象局),分析了热带风场变异对印度洋-西太平洋反沃克环流、赤道西风、越赤道气流的影响,及其对西太平洋副高脊加强、西伸的影响过程。

Mt.Damingshan locates just at the Tropic of Cancer,between 23°24′-23° 30′N,and between 108°22′-10°24′E.Pteridophyte flora in Mt. Damingshan is rather rich,there are 290 species represented 114 genera and 49families there.The types of pteridophytic area pattern t that place are rich also,the genera and species area pattern have 12 types and 13 types respectively.It's a notable phenomenon that the species are rare in pteridophyte genera and families in Mt.Damingshan.This flora is subtropical characteristics,of...

Mt.Damingshan locates just at the Tropic of Cancer,between 23°24′-23° 30′N,and between 108°22′-10°24′E.Pteridophyte flora in Mt. Damingshan is rather rich,there are 290 species represented 114 genera and 49families there.The types of pteridophytic area pattern t that place are rich also,the genera and species area pattern have 12 types and 13 types respectively.It's a notable phenomenon that the species are rare in pteridophyte genera and families in Mt.Damingshan.This flora is subtropical characteristics,of which according to genera area pattern,the tropical elements are 70%,the subtropical elements are 12.28%,while according to species area pattern,the tropical elements are 47.82%. The rather obvious endemic phenomena is another characteristic of this pteridophte flora,47 chinese endemic species including 9 endemic species of Mt.Damingshan have been found.This flora is most similar to that of tropical area,especially Indo-China.The genera and species affinity rate between the flora and that of Indo-China are 97% and 65.39% respectively.

大明山位于北回归线上,北纬23°24′~23°30′,东经108°22′~108°24′。蕨类植物非常丰富,现已发现49科、114属、290种。区系地理成分复杂多样,属可划分为12类型(变型),种可划分为13种类型(变型),科内、属内种类贫乏。本区系具亚热带性质,带有明显的热带性,热带分布属占70%,热带分布种占47.82%,亚热带分布属占12.28%。特有现象明显,有中国特有种47个,其中大明山特有种9个。本区系与热带植物区系特别是印度支那蕨类区系有密切的联系,属的相似率高达97%,种的相似率为65.39%。

 
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