holocene climate 中文意思是什麼

holocene climate 解釋
全新世氣候
  • holocene : adj. 【地質學；地理學】全新統的，全新世的。n. 【地質學；地理學】全新世。
  • climate : n. 1. 氣候；水土，風土；地帶。2. （社會思想等的）趨勢，傾向，風氣，思潮。
  1. The holocene loess - soil sequence in the loess plateau constitutes an excellent record of evolution of soil formation, monsoonal climate, aeolian dust accumulation and influences of arable farming of over 8000 years

    長期農牧業的發展，使得天然植被在大多數地方已蕩然無存，大片的林地被開墾為農田或被開辟為城市用地。
  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。
  3. Late - glacial and holocene climate change recorded in loess profile in weibei loess tableland

    渭北旱塬黃土記錄的晚冰期以來短尺度氣候變化
  4. In the area, the holocene climate alternately changed from cold to warm and from dry to wet and is mainly cool - dry

    得出此地區全新世氣候以冷暖、干濕交替出現，主要以溫涼乾旱為主。
  5. The holocene climate period is a fast developmental stage of human culture. in resent years, many researchers have investigated and found the close relationship between the environmental change of the holocene and human cultural development. laoguantai cultural relics is an early one since the new stone age

    全新世氣候期是人類文化飛速發展的時期，近十幾年來眾多學者對全新世氣候環境演變和人類文化發展之間的關系進行了深入的探討，發現二者之間存在著密切的關系。
  6. At the end of late pleitocene, influenced by the climate of glacier period, the last great event of the region in the geological time was taken place so that the migration and extinction of organism species were resulted, loess accumulation was generally developed throughout the whole region, in the holocene, the most important environmental change was fluvial process, which was still influnced by two factors - neotectonics and palaeoclimatic changes

    更新世晚期末，受末次冰期氣侯的影響，本區發生了地史時期的最後一次大事件，造成了物種遷移和絕滅，全區廣泛發育黃土堆積。進入全新世，本區環境變化以河流作用最為顯著，沉積物主要分佈在各大水系的河谷中，構成一、二級階地和近代河床與河漫灘堆積。
  7. The holocene events, therefore, appear to be the most recent manifestation of a pervasive millennial - scale climate cycle operating independently of the glacial - interglacial climate state

    所以，全新世事件似乎是（距今）最近的千年氣候周期的傑作。這種常見周期（刪- -的運行）是獨立於冰期-間冰期交替氣候的
  8. As the climate has become dry, and dust storms and dust - fall occurred frequently in whole weihe valley, the recent loess ( l0 ) has beg un to accumulate and gradually covered the mid - holocene soil ( s0 )

    在3100abp ，由於季風格局的突變，整個渭河流域進入了一個相對乾旱缺雨、成壤環境的惡化時期。
  9. It was obvious that the climate and environment had the tendency of drought after the maximum optimum period of holocene

    同時，其環境也經歷了由荒漠? ?荒漠草原? ?荒漠的演變過程。
  10. The climate of this period is almost as warm and wet as the stage 5e of the last interglacial. the mean temperature is 2 - 4 c higher and the precipitation is much larger than that of the today, the holocene which we live in. while in the climatic records of deep ocean, antarctic and greenland ice - core, marine isotope stage ( mis ) 3 is a weakly warm period, though a little warmer than marine isotope stage ( mis ) 2 and marine isotope stage ( mis ) 4, evidently colder than the last interglacial and holocene favorable period

    末次冰期中期，即深海氧同位素第3階段的氣候在我國，尤其是青藏高原地區表現出明顯不同於深海沉積物和極地冰芯記錄的特徵：青藏高原古里雅冰芯的~ （ 18 ） o曲線表明3階段存在特強夏季風事件，其氣溫和降水接近於末次間冰期5e階段，超過全新世，其暖濕程度已經達到間冰期的程度；而深海氧同位素3階段在深海、南極、格陵蘭冰芯的氧同位素記錄中均為弱暖期，雖較2階段、 4階段溫暖，但顯著低於全新世大暖期和末次間冰期。
  11. The profile includes two major cold peaks at 4. 580 - 5. 275 abp and 6. 120 - 6. 375 abp. the centennial - scale climate instability is obvious, which exists even in holocene optimum

    隨著氣候的逐漸好轉，喬木花粉在孢粉帶3 . 0904 . 580 abp上重新出現，但喜暖樹種較少。
  12. During the banpo man time or in the middle holocene, 5000 ~ 6000 bp, the climate within the modern glaciation best fitted vegetation and the intrusion of some sub - tropic trees was postulated to have taken place

    古土壤代表間冰期夏季風盛行的濕熱氣候，植被比較繁盛；黃土代表冰期冬季風盛行的乾冷氣候，植被凋凌。
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