little ice age 中文意思是什麼
little ice age
解釋
小冰河期-
Whether the decreased solar activity was somehow responsible for the little ice age is still unknown.
太陽活動的衰減是否會以某種方式引起小冰川期，這還不清楚。 -
The little ice age indicated by the 18o curve is divided into five cold valleys and four warm peaks
其中，中世紀暖期呈現兩峰夾一谷變化，小冰期劃分為5個冷谷4個暖鋒。 -
During the little ice age precipitation is little. due to different resolution, every record has difference in detail and also reflects area character
結合孢粉資料分析，在冷暖氣候變化中本區植被類型變化不大，以落葉闊葉木本植被為主，草本植被為輔。 -
In contrast, the consensus view among paleoclimatologists is that the medieval warming period was regional, that the worldwide nature of the little ice age is open to question and that the late 20th century saw the most extreme global average temperatures
然而，古氣象學家的共識與之不同，他們認為中世紀暖期屬于區域現象，全球性的小冰期則尚無定論，而且20世紀后葉的全球平均氣溫是最極端的情形。 -
Lesser challenges probably drove the vikings out of greenland during the most recent cold snap, called the little ice age, which started around a. d. 1400 and lasted 500 years
當時氣候條件並非最極端，卻可能是迫使維京人自格陵蘭絕跡的元凶。 -
And during the little ice age ). the main discrepancy of climatic and environmental changes of the southern margin of tarim basin and the eastern region of china appeared to be the collocation patterns which were the synchronism in cold or warm conditions and the difference in hydrological conditions. meanwhile, the discoveries of abrupt climate changes in the past have raised an urgent request for paleoclimatic and paleoenvironmental records
（ 2 ） 、中全新世氣候適宜期（ 6 . 7 3 . 0kab . p . ）尤其是近4 . 0ka以來及小冰期，南疆塔里木盆地南緣與我國東部季風區存在著冷、暖同步，干、濕相異的特徵；並以相對冷濕? ?相對暖乾的演變模式與我國東部季風區的相對冷干? ?相對暖濕的特徵相區別。 -
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 -
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。
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