scholarly journals Little Ice Age Phenomenon and Its Social and Economic Aspects Shown in Mt. Jiri Region In the 17th Century

영남학 ◽  
2010 ◽  
Vol null (17) ◽  
pp. 113-148
Author(s):  
박용국
Rangifer ◽  
2005 ◽  
pp. 21-30
Author(s):  
Sverre Fjellheim

Until today most researchers have named central Sweden and the Arjeplog area as the cradle of reindeer nomadism. However, there are reasons to believe that the practice of nomadic reindeer herding goes at least as far back in Røros and surrounding areas. The transition was probably initiated by large-scale climatic changes during the 16th and 17th century. Local historian, Anders Reitan, characterises the end of the 16th and the beginning of the 17th century as very difficult for the Røros district, with cold weather and crop failure. He refers to the year 1591 as the "black year", when "the grass didn't turn green north of Dovre", and in 1599 there was "general crop failure throughout northern Europe". 1635 was ostensibly as bad as the "black year", and it was told that in 1647 several people died right next to the trees they had stripped for bark to eat. The cold climate is confirmed by today's climate researchers. In the sources the period from 1550 to 1850 is referred to as "the little ice-age". For the Trøndelag area this meant regular north-westerly and north-easterly winds during the spring, causing later snow-melting and more frequent snowfall and periods of frost than we have today. Summers were shorter and colder, and there was less sun and more rain than in our days. Under such circum¬stances there must have been a good market for meat, which must have put considerable pressure on the wild reindeer stock. However, the cold climate with shortage of food and famine during the 16th and 17th century did not only lead to an increase in the hunting of wild reindeer, but it must also have had a direct influence on the wild reindeer population. Researchers have found that the spring in particular was getting colder during the "little ice-age". And spring weather is of crucial importance to the dynamics of population and the procreative powers of wild reindeer. According to Julie Axman the weather was bad and conditions for the reindeer very difficult in the Røros area around 1867. Reindeer calves died as a result of the long and cold springs, and her father had to borrow money in order to buy more animals. When climatic conditions during the 1860s had such a dramatic impact on the population of wild reindeer, it must have had at least as great consequences in the Røros area during the 16th and 17th century. Even though the reindeer in nomadic times were very tame and under continuous supervision, the herds were left to graze freely on open lands. With the presence of a large population of wild reindeer close to the tame herds, the risk of losing reindeer would be great, especially during winter and in the mating season. The wild reindeer population in Røros would therefore have to be reduced, either before or in parallel to an increase in the number of tame reindeer. The climate contributed to this reduction, and the Sami took care of the rest as far as it was necessary. This could take place in parallel to the building up of herds of tame reindeer. According to the sources there were at least 6 Sami villages in the 17th century, from Tydal in the north to Østerdalen in the south, which kept herds of tame reindeer, and at the same time the Sami population was accused of extinguishing the wild reindeer. A picture emerges. In sum, we can see that circumstances at the time were in favour of a change in strategy, from a hunting-based economy to nomadic reindeer herding.


2006 ◽  
Vol 52 (176) ◽  
pp. 110-118 ◽  
Author(s):  
Antoine Rabatel ◽  
Abraham Machaca ◽  
Bernard Francou ◽  
Vincent Jomelli

AbstractCerro Charquini, Bolivia (Cordillera Real, 5392 ma.s.l.) was selected as a site to reconstruct glacier recession since the maximum of the Little Ice Age (LIA) in the central Andes. Five glaciers, located on differently exposed slopes, present comprehensive and well-preserved morainic systems attributed to former centuries. The moraines were dated by lichenometry and show a consistent organization on the different slopes. The past geometry of the glaciers was reconstructed using ground topography and aerophotogrammetry. Lichenometric dating shows that the LIA maximum occurred in the second half of the 17th century, after which the glaciers have receded nearly continuously. Over the last decades of the 20th century (1983–97), recession rates increased by a factor of four. On the northern and western slopes, glaciers receded more than on the southern and eastern slopes (by 78% and 65% of their LIA maximum area, respectively). The mean equilibrium-line altitude (ELA) rose by about 160 m between the LIA maximum and 1997. Recession rates were analysed in terms of climatic signal, suggesting that glacier recession since the LIA maximum was mainly due to a change in precipitation and that the 19th century may have been drier. For the 20th century, a temperature rise of about 0.6°C appears to be the main cause of glacier recession. Recent climatic conditions from 1983 to 1997 correspond to a mass deficit of about 1.36m w.e.a–1. If such conditions persist, the small glaciers below 5300ma.s.l. in the Cordillera Real should disappear completely in the near future.


2020 ◽  
Author(s):  
Alexis Metzger

Abstract. This article explores Dutch winter landscapes from the 17th century, in light of written climatic sources. It investigates different kinds of climatic elements and winter weather types that were favoured by the artists during the Little Ice Age. The comparison between a corpus of paintings and narrative records show an overrepresentation of cold and dry weather in painted representations, in comparison to the written documents. Indeed, we can estimate that such particularly cold and dry weather corresponded to less than 20 % of winter days. Thus, the Dutch painters produced a winter imagery supported by icy scenes, in which the Dutch practiced skating. We interpret this choice by examining hypotheses based around four themes: climatic, religious, political, and social. Finally, despite their historical relevance, these winter landscapes are a genre, and only show very partially the diversity of winter weather during the 17th century and the Little Ice Age.


2002 ◽  
Vol 54 (2) ◽  
pp. 135-141 ◽  
Author(s):  
Dan J. Smith ◽  
Joseph R. Desloges

Abstract This paper describes licheno- metric and dendroglaciological investigations of Little Ice Age (LIA) deposits at Tzeetsaytsul Glacier, Tweedsmuir Provincial Park, British Columbia. The glacier originates from an ice- field on the northeast flank of Tzeetsaytsul Peak and terminates in a moraine-dammed lake. A stream draining the lake has incised the moraine dam and flows through nested moraines into a second lake. Two end moraines near the lower lake record separate advances, with numerous morainic ridges found between the two lakes. A locally calibrated Rhizocarpon geographicum growth curve was constructed and provides relative ages for all the moraines. Absolute dates from wood fragments collected from within the morainic debris were determined by matching their annual growth ring patterns to a local Abies lasiocarpa tree-ring chronology. The outermost terminal moraine was deposited by a 17th century advance that culminated in ca. 1700. Following subsequent recession, Tzeetsaytsul Glacier readvanced to build a second terminal moraine by the mid-1800s. Recession of this glacier occurred within 40 years and by 1935 the glacier was beginning to calve into the uppermost lake. The research shows that the most recent LIA advance of Tzeetsaytsul Glacier was not the most extensive, and that multiple events characterized the late-LIA. Application of the Rhizocarpon growth curve indicates a previously unreported 17th century advance at other glaciers in the region. These findings serve to reinforce the synchroneity of late-LIA glacier fluctuations within the coastal cordillera of NW North America suggesting that they record regional climate forcing.


Author(s):  
W.P. De Lange

The Greenhouse Effect acts to slow the escape of infrared radiation to space, and hence warms the atmosphere. The oceans derive almost all of their thermal energy from the sun, and none from infrared radiation in the atmosphere. The thermal energy stored by the oceans is transported globally and released after a range of different time periods. The release of thermal energy from the oceans modifies the behaviour of atmospheric circulation, and hence varies climate. Based on ocean behaviour, New Zealand can expect weather patterns similar to those from 1890-1922 and another Little Ice Age may develop this century.


2013 ◽  
Vol 6 (1) ◽  
pp. 29-36 ◽  
Author(s):  
Anastasia Gornostayeva ◽  
◽  
Dmitry Demezhko ◽  
◽  
Keyword(s):  

2020 ◽  
Vol 42 (1) ◽  
pp. 4-12
Author(s):  
Valeriy Fedorov ◽  
Denis Frolov

Author(s):  
Greg M. Stock ◽  
◽  
Robert S. Anderson ◽  
Thomas H. Painter ◽  
Brian Henn ◽  
...  

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