warm humid climate 中文意思是什麼
warm humid climate
解釋
溫濕氣候-
The green environment of blue sky and crystal water, beautiful scenery, warm and humid climate, fresh and clear air, profound historic culture, well - known yangzhou table delicacies, complete commercial and habitant facilities and careful health service have made gaoyou an ideal city for starting a undertaking, studying and living
藍天碧水綠色的環境底蘊深厚的歷史文化聞名遐邇的維揚美食配套全的商住設施細致周到的醫療服務，使高郵成為創業學習生活的理想城市。 -
Present palynological studies together with previous palynological data suggest a montane subtropical warm and humid climate during the neogene period in yunnan
植物群中被于植物佔69刀，裸子植物佔4石，蔽類植物佔24 l ，藻類植物佔2 -
Setenaly according to the analyses from selected profiles, we know that, it is cold and dry in this region during the early holocene when east asian winter monsoon ' s influence is obvious, so, it is a transition period from sand deposit to sandy soil deposit, when the layers become thinner gradually from north to south. during middle holocene, it is warm and humid, influenced evidently by east asian summer monsoon, so, it is an obivious pedogenesis, when there are generally well - developped holecene palaeosol ( so ) from north to south, and the pedogenesis in the south is better than that in the north, the soil is also thicker than that of the north. from late holocene to now, the climate changes to be dry and cold, but its changing scope is smaller than that of last glacial period
2 、就所選剖面分析來看，本區在全新世早期氣候回返，相對較寒冷乾燥，東亞冬季風影響較明顯，此時為沙層堆積向砂質土壤過渡，自北至南堆積的沙粒漸細；全新世中期氣候溫暖濕潤，東亞夏季風影響顯著，此時為明顯的成壤期，表現在自北至南普遍可見發育較好的黑壚土層，且南部的成壤作用比北部好，土壤的厚度也要大；全新世晚期至今，氣候向乾冷方向轉化，但變化幅度遠小於末次冰期。 -
Since the influence of clay materials here, the high calculations of magnetic susceptibility in fossil soil do not represent the climate elements of this layer, but represent the most warm and humid climate elements - of the upper layer
由於該區黏土物質遷移等影響，古土壤磁化率高值段一般不能代表該層段的氣候要素，而是表徵上層段最溫濕階段的氣候要素。 -
Cook has a tropical rainforest climate from december to march, the climate is warm and humid, with the possibility of severe stoms
全境屬熱帶雨林氣候， 12月至3月氣候炎熱潮濕，多暴風雨。 -
Most low - lying areas in hunan, warm and humid climate, times, " belcher wet land ", and mentioned hot chili, appetizers, qushi, flooding wind effect, it is deeply loved by the people of hunan
湖南大部分地區地勢較低，氣候溫暖潮濕，古稱「卑濕之地」 ，而辣椒有提熱、開胃、祛濕、驅風之效，故深為湖南人所喜愛。 -
Topographically, chongqing features hills and low mountains. it has a humid subtropical monsoon climate, characterized by warm winter, hot summer, little frost and snow, heavy fog and less - than normal sunshine
在地形上，重慶以小山和低山為主要特色。它以潮濕的亞熱帶季風氣候為主，其獨特的天氣特色是冬暖，夏熱，少霜雪，濃霧和低於常規的日照。 -
The existence of two taxa of taxodiceae reflects a warm - humid local environment under subtropical climate during late miocene. there are 4 taxa, pinus armandii, ericaceoxylon longlingense, ericaceoxylon hymenanthesoides and
他們反映的古植被為針闊混交林，生長于亞熱帶溫涼濕潤的山地氣候環境中，當時當地的誨拔高度在1800 3000米之間。 -
Comparison and study of the biotic characters in the jinggu and longchuan basins in yunnan province show that : ( 1 ) the two basins underwent the developing period, expanding period and shrinking period from early miocene epoch to pliocene epoch ; ( 2 ) the climate in the region was dry in early miocene epoch, warm and humid in middle - late miocene epoch and dry in pliocene period ; ( 3 ) the basins expanding in middle - late miocene epoch formed a semi - deep - lake to deep - lake environment
通過對雲南景谷盆地及隴川盆地新生代生物群特徵的對比，探討了新生代兩大盆地環境演變：早中新世到上新世為湖盆發展期湖盆擴大萎縮期，氣候為早期的千燥中新世早期的溫暖濕潤中新世中晚期的寒冷陰濕上新世的乾燥，而中新世中晚期湖盆的擴大形成的半深湖深湖環境為油氣的形成提供了有利條件。 -
Abstract : comparison and study of the biotic characters in the jinggu and longchuan basins in yunnan province show that : ( 1 ) the two basins underwent the developing period, expanding period and shrinking period from early miocene epoch to pliocene epoch ; ( 2 ) the climate in the region was dry in early miocene epoch, warm and humid in middle - late miocene epoch and dry in pliocene period ; ( 3 ) the basins expanding in middle - late miocene epoch formed a semi - deep - lake to deep - lake environment
文摘:通過對雲南景谷盆地及隴川盆地新生代生物群特徵的對比，探討了新生代兩大盆地環境演變：早中新世到上新世為湖盆發展期湖盆擴大萎縮期，氣候為早期的千燥中新世早期的溫暖濕潤中新世中晚期的寒冷陰濕上新世的乾燥，而中新世中晚期湖盆的擴大形成的半深湖深湖環境為油氣的形成提供了有利條件。 -
The modem equivalents of the 14 species suggest that a subtropical evergreen broad - leaved forest was growing in the area surrounding mangdan during miocene, under warm and humid subtropical climate. 2. numerous specimens of fruit and seed of ruppia were, for the first time, found from the zhangcun formation in the age of late pliocene ( 2. 3 - 3. 5 millions years old ) in yushe basin, shanxi, north china
山西省榆社盆地張村地區晚上新世（ 2 . 3ma - 3 . 5ma ）水生植物川蔓藻屬（ ruppia ）果實和種子的大量發現及其與川蔓藻屬2個化石種和5個現代種的比較表明，這些果實和種子屬於一個新種?榆社川蔓藻只ruppiayushensissp . nov . 。 -
They represent a humid and warm climate condition
昆蟲群落反映的是一種溫暖濕潤的氣候條件。 -
( 2 ) the analysis by characteristic section planes can draw that the ancient climate in deposit period of the characteristic section plane one sediments ( about seventeen thousand years before present ) is warm - dry and has relative humid and dry evolution rule, from fifteen to thirty years as its evolution period, that the ancient climate in deposit period of the characteristic section plane two sediments ( about fourteen thousand years before present ) is humid and has relative alternate very humid and humid evolution rule, from two to fourteen years as its evolution rule
（ 2 ）通過對兩個典型剖面的綜合分析得出，典型剖面沉積物沉積時期（距今約17kab . p . ）的古氣候特徵總體上為暖干，並具有以15 30年為演化周期，相對的濕潤-乾燥-濕潤的演變規律。典型剖面沉積物沉積時期（距今約14kab . p . ）的古氣候總體特徵為濕潤，並具有以2 14年為演變周期，相對的很濕潤-濕潤交替的演化規律。 -
The climate belongs to the tropics and the subtropics warm humid climate. it has the phenomenon that the warm - moist and the warm - arid climate changed alternately
總體氣候屬于熱帶和亞熱帶的溫暖濕潤氣候，存在著溫暖濕潤和溫暖乾旱的氣候交替的現象。 -
Due to its warm and humid climate, and abundant rainfalls and sunshine, the products here are rich, making wuzhen well - known as " the town of fish, rice and silk.
由於氣候溫暖潮濕，而且有著充足的雨水和陽光，這里物產豐富。這使得烏鎮被贊譽為「魚米之鄉」 。 -
It was a period of warm humid climate with large areas lf temperate and subtropical forest, but only limited grasslands, as the grasses were of very recent origin
當時氣候溫暖潮濕，除了有限的草地之外，擁有大面積的溫帶及亞熱帶雨林，這是因為大量草本植物是在近代才進化產生的。 -
In the final stage of the liangzhu culture, warm - humid climate, heavy precipitation and rising temperature led to sea - level rising, rivers running impeded, water areas large, in addition that the sites in the last stage of the liangzhu culture were mostly located in low - lying areas, which had liangzhu ancients suffered a unparalleledbig flood disaster resulting in the cultural decline
良渚文化末期，氣候暖濕，溫度增加，導致海平面上升，入海河流宣洩不暢，水域面積擴大，加之良渚文化晚期遺址多分佈在地勢低洼地區，因此良渚先民遭受了一場大洪水災難，遂使良渚文化迅速衰落。
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