森林草原帶 的英文怎麼說
中文拼音 [sēnlīncǎoyuándài]
森林草原帶
英文
forest steppe zone- 森 : 形容詞1. (樹木多) full of trees2. [書面語] (繁密; 眾多) multitudinous; in multitudes 3. (陰暗) dark; gloomy
- 林 : 名詞1 (成片的樹木或竹子) forest; woods; grove 2 (聚集在一起的同類的人或事物) circles; group 3...
- 草 : Ⅰ名詞1 (草本植物的統稱) grass 2 (指用作燃料、飼料等的稻、麥之類的莖和葉) straw 3 (草稿) dra...
- 原 : Ⅰ形容詞1 (最初的; 原來的) primary; original; former 2 (沒有加工的) unprocessed; raw Ⅱ動詞(原...
- 森林 : forest; timber; sylva; silva; eng-forest; boscage; bush
- 草原 : grasslands; steppe; prairie
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From loud barks to thunderous booms, hornbill cries resound across a range that extends from the dry savannas of sub - saharan africa to the lush forests of melanesia
無論在撒哈拉以南非洲的乾燥熱帶草原還是在美拉尼西亞茂密的森林中都可以聽到犀鳥如雷的叫聲。The shape index tends to increase with growth of the patch area. the shape indices of the forest and the farm landscape between 1. 10 and 1. 30 and the shapes of them are close to rotundity. however, the shape indices of the herbage and the shrub landscape of temperate zone between 1. 30 and 3. 00 and the shapes of them are long and narrow
五臺山地區的斑塊形狀指數隨著斑塊面積的增加有逐漸增大的趨勢,該地區各類景觀要素中,各類森林景觀和農田景觀的斑塊形狀指數大多在1 . 10 1 . 30 ,其斑塊的形狀較接近於?形(即緊密型形狀) ;而溫帶灌叢景觀、溫帶草原及灌草叢景觀和山地草甸景觀的斑塊形狀指數大多在1 . 30 3 . 00 ,這幾類景觀要素的斑塊由於面積較大,大多以狹長為主(即鬆散型形狀) 。So far as the north demarcation line of the forest zone is called the forest line, the north demarcation line of the forest - steppe zone should be called the tree line
相對于森林地帶北界森林線,森林草原地帶北界應為樹木線。Yunnan hot regions were classified into three geographical forest regions : 1 ) of southeastern yunnan including yuanjiang river region, nanpanjiang river and southern subtropical area ; 2 ) southern yunnan, including lancangjiang river area, nujiang river and yiluowadi river area ; 3 ) northern yunnan, including the dry and hot valley areas of jinshajiang river and tropical sparse forest grassland area
把雲南熱區分為3個森林地理區:雲南東南部元江、南盤江流域熱帶北緣、南亞熱帶森林區,雲南南部西南部瀾淪江、怒江、伊洛瓦底江流域熱帶北緣、南亞熱帶森林區,雲南北部金沙江河谷熱帶性、南亞熱帶性稀樹草原森林區。The number of forest patches in forest - meadow regions is greater than that in the forest zone and in meadow - steppe regions
在森林-草原交錯帶森林草甸區森林斑塊的數量最多,其次為森林帶,再次為森林-草原交錯帶草甸草原區,草原帶沒有森林斑塊。Steppe diversity, however, is characterized by higher plant diversity in the ecotone, especially in the forest - meadow region. diversity indices of plant communities reached peak values at the boundaries between the ecotone and the forest zone or the steppe zone, and between the forest - meadow region and the meadow - steppe region within the ecotone
在森林-草原交錯帶多樣性指數較高,表現在多樣性指數在森林-草原交錯帶與森林帶和草原帶之間以及森林-草原交錯帶內森林草甸區和草甸草原區之間的邊界不同程度地出現峰值。The species and genera of the vegetation cover mainly consisted of warm - dry plants whose main type is the alternation of the forest grassland or grassland
植物種屬以溫帶乾旱植物為主,植被類型多為森林草原及草原交替出現為主。Vegetation construction should n ' t be confined to such a land use pattern as " the 28 - word general plan " put forward by zhu xianmo. the objective reality of thin woods and sparse shrubberies in the forest - steppe zone cannot be ignored
植被建造不應局限於一種土地利用模式,如朱顯謨「 28字方略」 ,不能無視疏林及稀疏灌叢在森林草原地帶的客觀存在。Meanwhile, most aspects about this perspective are concerned, which include quantification of the soil water background of the plateau area, the regional spatial variation of soil water background and variation along the slope, mosaic structure and seasonal changes etc. the results show that : ( 1 ) for the fundamental circumstance for vegetation development is the original debilitated slope, so the perspective of soil water background specially for the loess plateau refers to the soil water conditions on the original slope. ( 2 ) the value of soil water background appears to be a descending trend from south to north based on the difference of vegetation zones. in the forest zone, soil moisture contents beneath 3m depth from the soil surface are more than 12 % usually ; in the forest - pasture zone, the values of soil moisture content beneath 4m depth underground are more than 6 % and stable, and tend to be ascending while the depth increases ; but the values in the dry pasture zone is lingering between 4 % to 6 % from the surface layer to sub - layers
發展了「土壤水分背景」的概念,並以之為基礎對其各個方面進行了研究,使之形成一個相對獨立和完整的體系,主要包括黃土高原土壤水分的背景值、土壤水分背景的區域分異、坡面分異、鑲嵌結構及其季節分異等: ( 1 )由於植被生長發展、演替的基礎階段是天然草被群落,故認為黃土高原的土壤水分背景在概念上是特指該區天然草被群落下的土壤水分狀況; ( 2 )黃土高原的土壤水分背景值,根據植被地帶的不同表現出自南向北逐漸降低的規律:森林地帶3米以下土層水分背景值普遍穩定地高於12 ,森林草原地帶4米以下土層水分背景值穩定大於6 ,且均隨土層的加深水分含量逐漸增加,而草原帶的土壤水分背景值自土表至底土層一直在4 6之間徘徊。The north slope on the east part of qilian mountains was separated into 6 vertical distribution zones : alpine cold desert meadow 、 alpine meadow 、 alpine bush meadow 、 mountain forest grassland 、 mountain grassland 、 and mountain desert grassland, there are also some areas of alternative distribution
祁連山東部北坡根據氣候、土壤、地貌等因素,分為6個垂直分佈帶:高山寒漠草甸帶、高山草甸帶、高山灌叢草甸帶、山地森林草原帶、山地草原帶和山地荒漠草原帶,有交替分佈的地段。The result of analysis shows that the climate of the period during which these strata were formed was mainly dry and cold, and the pollen of herbs is predominant. in the later part of this period the temperature and humidity increased a little, especially between the two cultural layers there was a short but clear section of wet and warm climate and a temperate forest steppe landscape existed
古環境分析表明,文化層出現前後的這一段時期,一直以乾冷氣候為主,草本花粉占絕對優勢,中後期溫濕度有所增加,尤其上下文化層之間曾有一個短暫而明顯的較為溫濕的時期,出現了溫帶森林草原景觀。Also, it has many kinds powerful rivers, wide plains and grasslands, lakes of all sizes, high mountains, great forests, sunny beaches, and lands of endless winter
有雄偉的河流、無垠的草原、大大小小的湖泊、高山峻嶺、遼闊的森林地帶,有陽光燦爛的海岸以及終年冰冷的地區。The world economy is depleting the earth ' s biodiversity, ocean fisheries, grasslands, tropical forests, and oil and gas reserves
世界經濟正消耗著地球的生物多樣性、海洋漁場、草原、熱帶森林、石油與天然氣的儲藏量。Rapid expansion of soybean plantations in south america could displace 22 million hectares ( 54 million acres ) of tropical forest and savanna in the next 20 years
在南美洲,大豆種植面積迅速擴大,這可能會導致未來20年熱帶森林和熱帶草原面積減少2200萬公頃( 5400萬英畝) 。In order to construct vegetation in line with local conditions, in addition the paper analyzes the viewpoints relevant to vegetation properties of the loess plateau along with regional differentiation of bio - climatic conditions and vegetation zonality. it is shown that the loess plateau might be regionalized into different vegetation zones of forest and steppe. it could n ' t be believed that zonal environment do n ' t be possessed in the loess plateau
為因地制宜地建造植被,本文還分析了黃土高原植被屈性的有關觀點,以及生物氣候條件在不同地域之間的分異性和植被地帶性特徵,說明黃土高原可表徵為森林、草原等地帶,不能認為黃土高原不具有森林發育的地帶性環境。The east transect was classified thirty five vegetation types using ndvi data from 1995 - 1996 by gis technique. the paper concludes that the ndvi from meteorological satellite is sensitive indicator of vegetation growing condition, times series curves of ndvi can truly curve vegetation growing principle by drawing the seasonal change curve of ndvi data by three groups. the paper also concludes that the forest ' s ndvi curve is commonly single apex, while farmland ' s or shrub ' s curve is mostly double apex, the peak value of forest ' s ndvi is commonly higher than grassland, farmland and some other vegetation types
應用地理信息系統技術處理1995 - 1996年1kmndvi數據,將南方樣帶劃分為35類,分三組繪制35類植被的ndvi季節變化曲線,得出氣象衛星ndvi是反映植被生長狀況的敏感指示器, ndvi時間序列曲線真實地刻畫出植被的生長規律;經分析得知森林ndvi曲線一般為單峰曲線,而農田灌叢多為雙峰曲線;森林ndvi峰值一般高於草原、農田等其它類型。Abstract : the forest - steppe ecotone in northern hebei and eastern inner mongolia is characterized by high biodiversity
文摘:河北北部、內蒙古東部森林-草原交錯帶富於高的生物多樣性。分享友人