坡地氣候 的英文怎麼說
中文拼音 [pōdeqìhòu]
坡地氣候
英文
climate of slopes-
The plant communities were surveyed, and the microclimates were observed, and the soil fertilities were determined in jinyun mountain in a series of fragmental evergreen broadleaved forests with different size and slope aspect, in comp " is n with continuous evergreen broadleaved forest
本實驗以不同大小、處于不同坡向的典型片斷化常綠闊葉林為對象，並以連續常綠闊葉林作對照，在縉雲山進行了植物群落調查、群落小氣候觀測以及樣地土壤肥力的測定。Kilimanjaro s vast slopes host five distinct climate zones. dense rainforests occupy the first zone of the mountain
吉力馬扎羅山的遼闊山坡可分為五大氣候地帶在山腳下是雨林區。The topography and the physiognomy of the south china sea are very complex such as continental slop, continental shelves, seamounts, sea basin, etc. the south china sea lies between qingzang plateau, which is as the main driver of the variety of climate, and the western part of the pacific, which is called warm pool, and is influenced by some current systems, such as coastal current, kuroshi, etc. the south sea has considerable species
南海具有陸坡、陸架、海溝、海盆等復雜的地形、地貌；南海位於作為地球氣候變化的主要驅動力的青藏高原和西太平洋暖池之間；南海受到沿岸流、南海暖流水、黑潮入侵水等流系的影響；南海具有豐富的物種分佈；上述因素共同影響南海生源要素的分佈、輸送和遷移。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。We cannot create an overall climate that encourages the learning of history if such a myopic and mercenary attitude persists. and people who could not care less about history will have a perfect excuse so what i ' m not the only one who is ignorant
如果新加坡人這種短視的功利主義的態度不改，全社會仍缺少一個重視歷史學習的大氣候，史盲們就可以毫無愧色地大聲說「吾道不孤」 ！According to climate condition, soil condition and afforesting tree species and water requirement rule of forest and grass, the paper analysed and calculated the slope length for collecting stream of three site preparation methods which were reverse - slope terrace, level trench and scale - hole, and the slope length for collecting stream of deferent gradients and planting bandwidths were acquired
摘要根據寧南山區的氣候、土壤、造林樹種等，按照林草植被建設的水分需求規律，對不同水上流失區的反坡梯田、水平溝、魚鱗坑3種整地方式的集流坡面長度進行分析與推算，計算出了不同坡度、植樹帶寬度下的集流坡長。However, it has rugged surface configuration, high mountains, steep slope, deep valley, barren soil, frequent mountainous and climatic disaster and fragile ecological environment
然而，在該區境內，地表崎嶇，山高、坡陡、谷深、土薄，山地災害與氣候災害頻繁，生態環境脆弱。It is suggested that the distribution of the depositional systems and the depositional facies have the clear characteristic that in the north of the research area, the alluvial fan sediment, the fluvial system and the delta system are the main styles of the depositional system, towards to the direction of basin the lacustrine, the barrier, the carbonate ramp system become the main depositional systems
受海平面升降變化控制，區內沉積體系和沉積相的分佈具有明顯的分帶性，北部靠近源區以沖積扇或河流及三角洲沉積為主，向盆地方向以湖泊或海岸障壁-瀉湖、碳酸鹽緩坡沉積為主。中二疊世北部源區發生構造抬升，當時古氣候逐漸乾燥，成煤環境結束，沉積物以陸相河流、湖泊三角洲占優勢。We also take into account the relation of wind direction and hilly aspect to calculate the wind accurate distribution in chongqing for different wind direction. the networkware ' s hilly aspect date is calculated with the chongqing dem ( 100m 100m ). it can provide base datum for chongqing agriculture region compartment
由重慶市1 ： 25萬dem計算了100m 100m網格點的坡向，由此計算了不同風向下的精細風速分布圖，為重慶地區農業氣候區劃提供可參考的基礎資料。Temporally, annual potential evapotranspiration is from 882 to 107 lmm, with a mean value of 974mm at qiabuqia ; and it is positively correlational to precipitation and temperature, so it is beneficial for plant growth because precipitation and heat ocurs at the same growth period. ; spatially, annual potential evapotranspiration is from 485mm to 1174mm, with a mean value of 1027mm, and it ' s spatial distribution is negatively correlational to precipitation and slope, whereas positively correlational to temperature and extra solar radiation, therefore the spatio - temporal difference of water become the key factors to plant growth and plant climate potential productivity
在青海共和盆地，歷年潛在蒸散平均974mm ，各月潛在蒸散與降雨和溫度之間是很好的正相關，所以雨熱同季有利於作物生長：年潛在蒸散的空間分佈范圍從485 ? 1174mm ，平均1027mm ，而且年潛在蒸散空間分佈與降雨和坡度是負相關，與溫度和大氣外層輻射正相關，因此水分和溫度的是影響作物水分耗散的重要因子，決定了共和盆地植被的氣候生產力。In order to find otit a new set of measures to control soil erosion on sloping cultivated farmland in three gorges reservoir area, we have adopted narrow terrace and put agroforetryjmd contour hedgerows into effect by means of sustainable development theories, ecological theories, and social economic theories since feb. 2001
本文針對三峽庫區的具體環境、氣候條件，為探索庫區陡坡耕地水土流失綜合治理的新方法，在庫區的陡坡耕地上，應用可持續發展理論、生態系統原理、社會經濟學理論，採用水平階整地方式，實施農林復合經營和生物籬埂技術。分享友人