wet period 中文意思是什麼
wet period
解釋
濕潤周期-
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。 -
History the professor still tells a reporter, even if sufferred from acuteness wet wart is not terrible also, they are being developed " the spirit that do not have care " the discovery in the process, follow theory of doctor of traditional chinese medicine and chinese traditional medicine the principle of conpatibility of medicines, the medicine in using is peculiar " make classics drug " mechanism, can make the active ingredient of medicaments direct inside the nucleolus of cell of action yu ji, make verrucous body shrinks gradually, necrotic, fall off, let original skin cell regain a new life, 2002 between 2006, their task group treats 972 acuteness wet wart in all, cure period of treatment the shortest have 3 days only ( verrucous body falls off entirely ), average 8 days, cure rate is as high as 99. 07 %, and recrudescent rate is extremely low
史教授還告訴記者，就算患了尖銳濕疣也並不可怕，他們在研製「無憂靈」過程中發現，遵循中醫理論和中藥配伍的原則，採用中醫藥特有的「引經藥」機理，可使藥物的有效成分直接作用於棘細胞的細胞核內，使得疣體漸縮、壞死、脫落，讓原來皮膚細胞重新獲得新生，在2002年2006年間，他們的課題小組共治療972例尖銳濕疣，治愈療程最短的只有3天（疣體全部脫落） ，平均8天，治愈率高達99 . 07 % ，且復發率極低。 -
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。 -
The time period of alcmaeon, who proposed four ' powers ' of the body : hot, cold, wet, and dry. also asked the question, " where does the nous live ?
阿爾克邁翁（又譯阿爾克芒）時期，提出身體的四種「力量」 ：熱、冷、干、濕。還提出了「心靈居於何處？ 」的疑問。 -
There was a positive correlation between wet gluten content and average day temperature and average sunshine in the same period
濕麵筋含量與同期平均日均溫和平均日照時數呈正相關。 -
In ported trials, wu gave the minimum tr of all plants, and its diurnal maximum tr persisted stability the most within the range of soil moisture 20. 4 % - 6. 4 %. ; nx lowered its tr and shrank its high - low lines after had experienced irregular wet - drought hardening period during culturing ; kerqin performed a plasticity as compared to field ; c. lanata also stood the most stability but on the basis of middle - high maximum tr level ; tr by caragana korshinski was high when soil water was abundant, but was lowest for lack of water ( 6. 4 % )
盆栽試驗表明，華北駝絨藜蒸騰最弱，且在土壤含水量20 . 4 6 . 4的范圍內最高蒸騰速率穩定性最強；經脅迫鍛煉寧夏駝絨藜蒸騰降低，變幅減小；科爾沁駝絨藜與大田相比蒸騰可塑性較強；土壤水分變化中，北美駝絨藜蒸騰在中高水平上維持穩定的能力最強；水分良好時檸條蒸騰很強，水分脅迫中蒸騰極大降低。 -
( 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。 -
Suppose that a peak harvest - season day involves 18, 000 barrels of berries, 70 % of them wet - harvested, arriving over a twelve - hour period from 7 a. m. to 7 p. m
假設高峰收獲季節一天有18000桶漿果，其中70 %是潮濕狀態下收割的，經歷了早上7點到晚上7點12個小時。 -
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。 -
Although the monthly rainfall of 12. 4 millimetres for april 2002 was the third lowest on record, the accumulated rainfall for the first four months of the year was 280. 7 millimetres, near the normal figure of 299. 8 millimetres for the same period following a wet march
雖然四月的雨量僅為12 . 4毫米，是歷來第三低的紀錄，但由於三月多雨，本年首四個月的累積雨量達280 . 7毫米，與同期平均數值299 -
The late 1940s - early 1960s and early 1970s to middle 1980s is wet period. the early 1960s to early 1970s is dry period. the significant decrease of rainfall began in the 1990s
40年代末至60年代初期及70年代初期至80年代中期為多雨期， 60年代初期到70年代初期為少雨期， 90年代初期以後又有明顯的下降。 -
The study on the time series of global land average seasonal precipitation points out that the interannual and interdecadal fluctuations of the rainfall are clear. the late 1940s - late 1960s and the 1980s - 1990s corresponds to wet period and dry period respectively, and the 1970s expresses a apparent interannual variation of rainfall
指出降水有明顯的年際和年代際尺度的振蕩， 1940s末至1960s末為多雨期， 1980s至今降水多為負距平； 1970s降水的年際變化比較大。 -
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。 -
At its mature period of stone carving, sui dynasty produces many outstanding buddhist statues with unique characteristics and dignified gestures and magnificent dress. when it is the tang dynasty, buddha images were dressed in clothes so thin and light as if wet gauze sticked to the body
唐代的佛像雕刻在衣著外型上的一種表現形式，就是所謂「薄衣貼體」 ，即佛衣被刻劃得輕薄能顯出肉體感，猶如濕水貼體一般，后是對佛像形式的一種專稱。 -
The dry / wet changes of surrounding area of bohai sea during past 500 years are divided into 7 stages, based on dry / wet indexes ( d / w ) of this area from 1470 to 1985 then, the changes of dry / wet spatial types ( d / wst ) and its related dry / wet regional different iation ( d / wrd ) features among different stages are analyzed. the results show that there are 4 main kinds of d / wst in this area, whose notability and spatial distribution features in different stages are apparently different, which reflects, very well, the changing process of the d / wrd of this region in past500 years. further analysis also presents that, in warmer period, the d / wst and the d / wrd patterns are relatively unsteady, meanwhile, the dry / wet changing difference among different parts of the region is relatively great, but, in colder period, it is just on the contrary. however, in the most severely cold period of the little ice age, t he area ' s d / wst and the d / wrd pattern sareveryu nsteady, and its d / wrd extenti salsot he high estin the whole past 500 years
用研究區1470 1985年的旱澇等級資料，劃分了該地區500年來旱澇變化的7個階段，討論了不同階段間旱澇型的變化及其旱澇區域分異意義，結果表明， 500年來研究區有4類主要旱澇型，各型旱澇在不同階段的重要程度及場型特徵均有較大差異，深刻反映了該地區500年來旱澇區域分異特徵的變化，通過對500年來旱澇變化與溫度變化的對比發現，較溫暖期，研究區的旱澇型及旱澇區域分異格局較多變，旱澇變化的區域差異性較大，較寒冷期，旱澇型及區域分異格局較穩定，旱澇變化的區域差異性較小，而在小冰期最寒冷階段，旱澇型及旱澇區域分異格局的變動十分頻繁，旱澇變化的區域差異性亦最大 -
The coarser sedimentary layers reflect the period of warm and wet climate, during which the natural runoff of weihe river violently rose, the speed of flow increased and the flood easily occurred ; on the contrary, the finer sedimentary layers reflect the period of cool and dry climate, during which the natural runoff of weihe river fell and the speed of flow slowed
在氣候相對溫濕、降水量較大的時期，渭河水動力條件增強，流量增大，流速加快，出現粒度明顯變粗的沉積夾層，此時也是洪水多發時期；而在氣候相對涼干、降水量較少的時期，渭河水動力條件減弱，流量減少，流速變慢，因此出現粒度明顯變細的沉積夾層。
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