cold dry area 中文意思是什麼
cold dry area
解釋
乾冷區-
The changes of 14 assemblages reflect 11 paleoclimate evolutioinary stages in this area during the quaternary. in the cold period, the climate was dry and enviroment was deficient of water, therefore, the terrestrial pulmonata was dominant in the gastropod fauna
本文對北京平原區第四紀軟體動物化石進行了初步的研究，建立了14個組合帶，反映了本區第四紀時期經歷了大約11個古氣候演變階段。 -
With advantageous water, soil and organisms resources, the dadiwan culture, the yangshao culture, the longshan culture and the xiashang culture developed, original settling - down dry farming culture formed gradually, which laid sound foundation for agriculture civilization in the weihe valley ; among which, land use of arable farming was replaced largely by pastoral farming in the mixed area of agriculture and animal husbandry in north weihe region between 4 000 - 3 000 a b. p., because of dry and cold weather resulted in environment deterioration and soil degradation. at the beginning of 3 100 a b. p.,
在8500 3100abp全新世大暖期，渭河流域水、土、生物資源條件優越，人類發展了大地灣文化、仰韶文化、龍山文化和夏商文化，逐步形成了原始定居旱作農業類型文化，從而奠定了渭河流域農業文明的基礎，其間在4000刁000ab衛，渭河流域北部的農牧交錯帶，由於氣候的逐漸冷干化，導致水、土、生物資源退化，造成旱作農業土地利用方式由遊牧業取而代之。 -
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。 -
The highlight features of distribution of fossil and living three species microtine in the area are showed as followings : ( 1 ) the microtus oeconomus which keeps moist and cold was most in the 3rd cave, but absent in recent ; ( 2 ) meanwhile the caryomys ienz which prefers dry and warm was absent in 3rd cave, but live in recent ; ( 3 ) the caryomys eva which prefers moist and cool was a little in 3rd cave and live in near sites recent
本文所研究的三種田鼠的化石及現生種分佈的突出特徵表現為：喜冷濕的microtusoeconomus在第三層洞最多，現在該區沒有分佈；喜溫乾的caryomysinez陜西洛南張坪田鼠類化石研究在第三層洞尚未發現，現在該區有分佈；喜溫濕的cp叮weva在第三層洞較少，現在在鄰近地區還有分佈。 -
Maybe the environmental and climate change of the studied site and nearly area showed by distributions of the three fossil and living species microtine above is just as following : 430ka ? p, warm and moist : 262ka ? p, cool and moist ; 162ka ? p, cold and moist ; 57ka ? p, cool and moist ; recent, warm and dry
研究區及其附近，田鼠類化石與現生種的上述分佈特徵所反映出的環境變化可能為： 430ka土b衛，溫濕?一262ka土巳衛，涼濕?一162ka土b衛，冷濕?一57ka土bj ，涼濕?一現代，溫干。 -
Occupying 20, 000 square feet in total area, supreme sauna is furnished with dry and humid steam rooms, cold and warm bathing pools, restrooms and over 40 massage vip rooms
面積達二萬多平方尺，設施完善，備有乾、濕蒸房、冷熱大池、寬敞休息室及獨立按摩房四十多間。 -
The analysis of dry pv shows that the high pv dominate the area of typhoon, the higher is the center value of pv, the stronger is the typhoon. lt is also shown that the most important reason resulting in rainstorm is the cold air ( high pv ) which spreads to south from the upper troposphere or lower stratosphere and transports into the warm air. the joining situation of upper and lower pv area make vortex develop. pv transpotation reduces static stability, which increases the releasing of instability energy and makes rainstorm amplify
對干位渦的分析表明：臺風或臺風環流區為高值位渦區，臺風越強，位渦中心值越大；對流層上部或平流層下部冷空氣（高位渦）的擴散南下與暖濕氣流的交匯是造成特大暴雨的重要原因，因為上游斜壓性的發展使對流層頂發生折疊，平流層與對流層相互作用增強，上下位渦區相接的形勢使低層渦旋發展，上升運動加強，位渦的下傳有效地降低了靜力穩定度，有利於位勢不穩定能量的釋放，使得暴雨增幅。 -
3. there is much correspondence between the curve of the susceptibility and the strata. based on the analysis of the susceptibility, it can be concluded that the area has undergone many climatic fluctuations from dry - cold to warm - wet
磁化率曲線與地層具有很好的對應性，並通過磁化率分析認為該地區經過了乾冷-暖濕的多次氣候波動。 -
4, the summer rainfall anomaly in northeast china bears close correlation with the atmospheric circulation backgroud. while cold air in middle and high levels of troposphere is active in wet year with the positive anomalies over high - latitude and polar area, the active longwave ridge, the anomalous long - wave ridge in northeast china and inner - mogolia as well as the northward and eastward of the polar vortex, the contrary is in the dry year in northeast china
4東北地區夏季降水異常與大氣環流背景有密切的關系，東北地區夏季多雨年在對流層中、高層冷空氣比較活躍，高緯和極區主要由位勢高度的正距平所控制，貝加爾湖以北的地區長波脊較為活躍，在東北地區和蒙古地區有異常的長波槽發展，極渦位置偏北、偏東；而在東北地區夏季少雨年則容易出現與上述相反的異常環流形式。 -
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 company covers an area of 10, 000 square meters, among them, 3000 square meters of the standard axenic workshop with the capacity of quick - freezes & process of 40 tons per day, 1000 tons of the frozen storehouses ; 1500 square meters of the aquatic products dry & process workshop with the capacity of dry & process of 10 tons per day, and the cold wind storehouses of 100 tons is furnished
公司佔地1萬平方米，其中，標準的無菌加工車間3000平方米，日速凍加工能力40噸，冷凍庫1000噸；乾燥水產品加工車間1500平方米，日乾燥加工能力10噸，並配有100噸的冷風庫。
分享友人