warm period 中文意思是什麼
warm period
解釋
暖期-
2 microzooplankton of jiaozhou bay were composed chiefly of neritic warm - temperate and estuarine low - salinity species. eurythermic and euryhaline species were sparse. cold - water, oceanic hypersaline and tropical warm - water species were not found during the study period
2 、膠州灣小型浮遊動物以暖溫帶近岸、河口低鹽種為主，廣溫廣鹽種較少，尚未發現冷水種、外海高鹽種和熱帶暖水種。 -
Warm with the fancies of youth, pretty with the insipid prettiness of the formative period, possessed of a figure promising eventual shapeliness and an eye alight with certain native intelligence, she was a fair example of the middle american class - two generations removed from the emigrant
不過從她的身段已經可以看出將來發育成熟時的美妙體態了。她的眼睛里透著天生的聰明。她是一個典型的美國中產階級少女-她們家已是移民的第三代了。 -
In the warm period, the aquatic bivalvia was well - developed, and the gastropod fauna was obviously prosperous and characteristic by large amount of the aquatic species. the alternative appearance of both cold and the warm mollascan assemblage tpyes reflects the features of the quaternary climate changes in this area
在冷期因氣候乾燥，環境中水量減少，腹足類化石以陸生肺螺類最為發育；在暖期水生雙殼類較為發育，腹足類群明顯繁盛，以水生種類的大量出現為特徵。 -
" evangelization year " can be seen as a warm - up activity of the long - term evangelization plan. within the period of one year or so, every level of the hong kong diocese is mobilized to evangelize ad gentes
福傳年實踐期可以視為長遠福傳計劃的熱身，在一年多時間內積極推動香港教區上下一心，向教外人傳揚福音。 -
By comparing i8o curve with annual growth rate and grey level curve in the stalagmite during the same period, the author brings forward that that climate in shennongjia region mostly embodies matching modes of warm / wet, cold / dry over the past 2000 years, but temperature was out of harmony with precipitation in the course of climate transforming, which shows that shennongjia climate embodies matching modes of cold / wet, warm / dry at part period of time
近2000年中17次太陽活動和1400aad以來29次火山活動對氣候變化影響的印跡在石筍氧同位素中都有明顯的記錄，表明氣候事件與太陽活動、火山活動有較好的相關性。石筍各代用指標譜分析顯示126a 、 100a 、 81a 、 60a 、 40a 、 22a 、 11a等周期成分，也進一步支持了太陽活動對季風區短尺度氣候變化的驅動作用。 -
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。 -
Many research such as clay minerals, suspend in the sea, the grain size trend analysis of surface sediment, poc 6 cu and 8 c13 in bottom sediments etc. showed that : the yellow sea warm current divided the south yellow sea into two, the terrestrial material of modern sediment on the west shelf plain mainly came from the modem yellow river suspend carried by the alongshore current, and the sediment difference between the west and east side of yellow sea trough was represented by the sedimentation thickness in postglacial period, sedimentation stratum, and oxygen isotope record
粘土礦物、碳酸鹽、粗碎屑、海域懸浮體、表層沉積物粒度趨勢分析、 poc c ~ （ 13 ）及底質沉積物的c ~ （ 13 ）等多方面研究表明：以黃海暖流為主導，南黃海堆積陸架平原西側現代沉積物陸源物質主要源於黃海沿岸流攜帶的現代黃河懸移物質，黃海槽東西兩側的沉積差異主要表現在冰消期以來沉積厚度、沉積層序、氧同位素記錄上。 -
The whole jurassic period santanghu basin was undergone a sedimental cycle : river - lake - river, the environment changed from warm - wet to drought
三塘湖盆地整個侏羅紀經歷了一個由河流?湖泊?河流的沉積旋迴，環境由溫暖潮濕逐漸向半乾旱?乾旱的環境轉變。 -
Conclusion our data indicate that the method of continuous warm blood cardioplegia is safe and effective and represents a new conceptual approach to maintaining excellent myocardial preservation during a long period cardiac arrest
結論持續灌注溫血停搏液技術可使心臟在停搏期間有充足的血液供應，是一種理想的心肌保護方法，特別適用於需長時間停搏和高危病例。 -
( 2 ) there is stage of soil formation from the evolution of pedogenic environment in the weihe valley during holocene. soil formation shows the law of evolving from warm and wet strong soil formation period to cold and dry dust deposition period ( weak soil formation period ) and to warm and wet strong soil formation period again. the loess - soil sequence is a compound soil sectional system of different kinds of soil evolution under different bio - environment and pedogenic processes
（ 2 ）通過對全新世渭河流域成壤環境演變問題的討論，揭示了全新世渭河流域土壤的發育具有階段性，表現為由溫濕的強成壤期向冷乾的沉積期（弱成壤期）演變、再向溫濕的強成壤期演變的規律；黃土一古土壤序列是不同生物氣候環境下、不同成壤過程發育的不同土壤類型演替而形成的復合型土壤剖面體系；而且由於冬夏季風環流及其環境效應在空間上的差異，使得復合型土壤剖面體系也存在著南北差異。 -
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。 -
How can people in warm climates prepare for this period
居住在溫暖的氣候的人們要如何準備這個時期？ -
Within several hundreds or thousands of years after the start of a typical warm period, the climate reverted to slow cooling followed by quick cooling over as short a time as a century
典型暖期開始后的數百年至數千年內，氣候先緩慢轉冷，接著在一世紀左右的短期內迅速冷卻。 -
( 1 ) the winter air temperature in north - east china was in cold period before 1985, and lowest in 1960 ' s ; were in warm period after 1985, and got warmest in this period, the catastrophic time is 1986
研究結果表明： （ 1 ）東北冬季氣溫80年代中期以前處于冷期， 60年代達到低谷， 80年代中期以後處于暖期，並達到49a最高峰， 1986年是由冷轉暖的明顯突變點。 -
The possible influence of the global warming to storm surge frequency has been one of the concerned questions at present for researchers. some of them consider that the frequency will increase according to the results of observation and simulation, but some others do n ' t agree to it. to verify the speculated conclusions, the coastal storm surge frequency in middle jiangsu province during the warm period of middle holocene is discussed in this thesis
風暴潮頻率在全球氣候變暖后的可能變化已引起了廣泛的關注，而目前研究者們通過模擬與觀測所獲得的結論並不一致，基於此，本文從地質時期氣候冷暖變化與熱帶氣旋頻率變化之間的關系對這一問題作了驗證與探討。 -
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。 -
The 40 - 50 years periodic change divides the temperature variation into three main cold and warm vicissitudes of the last 50 years, which include the warm period before mid 1960s, the cold period from later 1960s to 1980s and the warm period after the 1980s ; ( 2 ) the precipitation variations in heilongjiang province have multi - time scale and jump characteristics
近50年來黑龍江省的氣溫變化在40 55a尺度上表現為兩個暖期和一個冷期，它們分別是60年代中期以前的偏暖期， 60年代後期到80年代的偏冷期和80年代以後的偏暖期：黑龍江省的降水變化也具有多時間尺度特徵和突變特徵。 -
During the medieval warm period, the lasting time is shorter and shorter from the south to the north in china, and the east china is more obvious than the central china ; the beginning time of the little ice age in shennongjia region ( 1480aad ) is later than that in other regions ( 1420aad ), but they all display a persistent decrease process of temperature
與中國東亞季風區各種溫度記錄對比表明，東漢時期是一較暖的時期，但冷暖程度不同；中世紀暖期大致從南往北時間跨度越短，中部地區沒有東部明顯；神農架小冰期開始時間（ 1480aad ）晚于其它記錄（ 1420aad ） ，都顯示了持續的降溫過程。 -
All records show the characteristics of high precipitation and large swing before 1100aad, but the characteristics of low precipitation and small swing after 1100aad. during the medieval warm period there is a very dry period
相同時段氧同位素與紋層厚度、灰度對比表明，過去2000多年主要是暖濕、乾冷的氣候組合方式，但在氣候轉型期溫度、降水並沒有完全表現同步變化，體現乾暖、冷濕組合。
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