Titlebook: Glacier Fluctuations and Climatic Change; Proceedings of the S Johannes Oerlemans Conference proceedings 1989 Springer Science+Business Med

Palliation

負(fù)擔(dān)

Outshine

Historic Glacier Variations in Scandinavia,heir maximum extension during the climatic deterioration in the 18th century, but some of the maritime glaciers in western Norway reached their maximum or near maximum as late as in the first part of the 20th century. Glacier advances in the early part of this century are associated with periods of

PARA

medieval

Contort

Effects of Topographic and Climatic Controls on 19th and 20th Century Glacier Changes in the Lyngene on rock plateaus about 900 m a.s.l. with a maximum summit altitude of 1200 m and ice thickness believed to be at least 100 m over substantial areas. The outlet glaciers flow down to about 400 m a.s.l., are receding at present and have been since the turn of the century..The southern Lyngen Alps li

Albinism

A Historical Perspective of the Nineteenth Century Ice Trade,e are records of Norwegian glacier ice being exported to Britain from c. 1820 onwards. In 1844, the first cargo of “Wenham Lake Ice” from the Boston area of America arrived in Liverpool. High pressure advertising ensued, with the result that a fashionable market in ice was created. The increase in d

表示向下

Mass Balance History of Blue Glacier, Washington, USA, from ice and firn melt with the residual snow remaining at the end of the summer season. In order to define confidence limits for the historical mass balance data set, it is necessary to quantify several sources of potential error. Preliminary analysis of the spatial variance of ice melt within the

撕裂皮肉

,Mass Balance and Volume of South Cascade Glacier, Washington 1958–1985, the net balance values for the 1958–85 period is ?10.0 meters water equivalent. Topographic maps of the glacier were made from late summer vertical aerial photography in 1958, 1961, 1964, 1977, 1980 and 1985. In addition, the topography in the late summer of 1970 is well known from the theodolite s

Anthropoid

Field Stations for Glacier-Climate Research, West Greenland,ions were operated near the margin of the Greenland ice sheet in Johan Dahl Land 1978–1983, at Qamanarssüp sermia 1980–1986 and at Tasersiaq since 1982. Measurements of snow accumulation and ice ablation are made at many stakes drilled into the ice. Ablation measurements are made daily at the stakes