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  • Glacial morphology and snow-lines of younger Quaternary around the Yari-Hotaka Mountain range, northern Alps, central Japan
  • In this paper, the authors attempt to elucidate the glacial geomorphology to clarify the ages of glacial stages by correlating with some glacial stages in other areas, to study some problems of snow-line reconstruction, and to reconstruct the change
  • of the altitude of snow-line using geomorphological and meteorological data. (L'A.).
  • Glaciation ; Himalaya ; Lateglacial ; Moraine ; Nepal ; Palaeo-environment ; Quaternary ; Snow line
  • On the basis of empirical findings and inductive conclusions, the least extent of glaciation during the last ice age can be shown for 2 areas on the southern slopes of the Himalayas in Nepal. For the Rolwaling Himal, the snow line during the last
  • ice age is calculated at 4000 m asl., i.e., 1500 m below the recent snow line. The last high-glacial snow line in the Kangchenjunga Himal is thought to be at 4350 m asl., the snow line depression here is 1150 m.
  • Spatial and temporal analysis of the snow line in the Alps based on NOAA-AVHRR data.
  • AVHRR ; Alps (The) ; Altitude ; Comparative study ; NOAA ; Numerical model ; Remote sensing ; Satellite imagery ; Snow ; Snow line ; Switzerland
  • Relocation of snow and its effects in the treeline ecotone . With special regard to the Rocky Mountains, the Alps and Northern Europe
  • Ecology ; Ecotone ; Snow line ; Temperate zone ; Tree line ; Wind
  • and Khumbakarna Himal) including informations on late-glacial, neoglacial, and historical glacier stages, their snow-line depressions and ages
  • The maximum Ice Age (Würmian, Last Ice Age, LGM) glaciation of the Himalaya - a glaciogeomorphological investigation of glacier trim-lines, ice thicknesses and lowest former ice margin positions in the Mt. Everest-Makalu-Cho Oyu massifs (Khumbu
  • Asia ; Glaciation ; Glacier ; Glacier fluctuation ; Himalaya ; Karokoram ; Palaeoclimate ; Palaeogeography ; Quaternary ; Snow line ; Wurm
  • The role of snow and ice in the global climate system : a review
  • Climate ; Cryosphere ; Frozen ground ; Ice ; Ice sheet ; Impact ; Multidimensional scaling ; Sea ice ; Snow ; Snow cover ; Snow line
  • The impact of elevation, topography and snow load damage of trees on the position of the actual timberline on the fells in central Finnish Lapland
  • Altitude ; Biogeography ; Cold area ; Finland ; Forest ; Lapland ; Snow ; Topography ; Tree line
  • affecting these positions and snow load damage to trees on the fells Aakenustunturi, Yllästunturi and Pyhätunturi. The potential for ascending timberlines in the region is also discussed.
  • Glacial features and snow-line trend during the last glacial age in the Southern Apennines (Italy) and on Albanian and Greek mountains
  • Albania ; Appennino ; Climatic variation ; Crete ; Front moraine ; Glacial features ; Greece ; Italy ; Mountain ; Palaeogeography ; Palaeogeomorphology ; Postglacial ; Snow line ; Vertical movement ; Wurm
  • Asia ; Geochronology ; Glaciation ; Glacier ; Grain size distribution ; Himalaya ; Lateglacial ; Mass movement ; Model ; Moraine ; Palaeogeography ; Roche moutonnée ; Snow ; Snow line ; Tibet ; Vertical movement
  • is proved; a snow-line (ELA)-depression of 820-1250 m in relation to the present relief has been calculated. Modelling by means of those snow-line depressions and estimations of the precipitation provide ideas about surface heights, ice thicknesses and flow
  • behaviour of the ice sheet. The hypothesis of a global triggering of the ice age by the uplift of the subtropical Tibet up to above the snow-line motivates the investigations presented here.
  • Alaska ; Cirque ; Cold area ; Frost action ; Geomorphometry ; Periglacial features ; Snow ; Snow line ; Terrace
  • Correlation ; Cyclogenesis ; Former USSR ; IEC ; Northern hemisphere ; Snow ; Snow cover ; Snow line
  • The Historical Snow Survey of Great Britain: Digitised Data for Scotland
  • Data ; Risk management ; Scotland ; Snow ; Snow cover ; Snow line ; Spatial analysis ; United Kingdom
  • Mountain snowline is important as it is an easily observable measure of the phase state of water in the landscape. Changes in seasonal snowline elevation can indicate long-term trends in temperature or other climate variables. Snow-cover influences
  • local flora and fauna, and knowledge of snowline can inform management of water and associated risks. Between 1945 and 2007 voluntary observers collected a subjective record of snow cover across Great Britain called the Snow Survey of Great Britain (SSGB
  • ). The original paper copy SSGB data is held by the Met Office. This article details the digitisation of the Scottish SSGB data, its spatial and temporal extents, and a brief example comparison of Met Office snow-lying gridded data. The digitised SSGB data
  • Climate pattern, snow- and timberlines in the Altai mountains, Central Asia
  • Altai Mountains ; Asia ; Asian part of Russia ; Central Asia ; China ; Climate ; Geo-ecology ; Geomorphology ; Glacier ; Mongolia ; Mountain ; Precipitation ; Snow line ; Temperature ; Tree line
  • Altitude ; Glacial features ; Greece ; Karst ; Moraine ; Mountain ; Peloponnese ; Pleistocene ; Quaternary ; Roche moutonnée ; Snow line
  • considération altimétrique. Les témoignages du stade suivant, par contre, marquées par des petits cordons morainiques, permettent de calculer l'ELA (Equilibrium Line Altitude).
  • Climatic variation ; Glacier ; Glacier mass balance ; Palaeoclimatology ; Snow line ; Statistics ; Temperature ; United States
  • This paper reviews methods of climatic interpretation of glacier fluctuations on time scales of 103 to 104 years. Glacier dynamics are not considered; rather, the problem is approached from the perspective of pertubations in the equilibrium-line
  • Carbon cycle ; Ecosystem ; Ecotone ; Forest ; Model ; Montana ; Primary production ; Snow ; Soil moisture ; Tree line ; Tundra ; United States of America
  • The purpose of this research is to evaluate the relative importance of selected processes (snow redistribution and winter dessication) important at the alpine treeline ecotone (ATE) using an existing physiologically mechanistic model, FOREST-BGC
  • Risk analysis of snow disaster in the pastoral areas of the Qinghai-Tibet Plateau
  • China ; Climatic change ; Climatic hazard ; Natural hazards ; Pastoral ; Pastureland ; Plateau ; Qinghai ; Risk analysis ; Snow ; Snow cover ; Tibet ; Vulnerability
  • -Tibet Plateau is higher than that at the edge of the plateau. On the Qinghai-Tibet Plateau, the 30°N latitude line appears to be significant in the context of snow disaster.
  • Based on the hazard harmfulness data collected from historical records and data collected from entities affected by this hazard in 2010, a comprehensive analysis of the 18 indexes of snow disaster on the Qinghai-Tibet Plateau was conducted
  • , encompassing the hazard harmfulness, the amount of physical exposure the hazard-bearing entities face, the sensitivity to the hazard, and the capacity to respond to the disaster. Overall, the risk of snow disaster in high-altitude areas of the central Qinghai
  • Asia ; Central Asia ; Glaciation ; Model ; Moraine ; Palaeogeography ; Quaternary ; Snow line ; Tien Shan ; Wurm
  • : with a gradual and with an abrupt change in snow-line elevation. It yielded ice-marginal positions which agreed with the field observations.
  • Central Europe ; Cirque ; Czech Republic ; Europe ; Glacial valley ; Glaciation ; Mountain ; Pleistocene ; Poland ; Quaternary ; Snow line ; Sudety ; Topography
  • : the altitude of the summit parts well above the snow line, large extent of the summit surfaces of low relief and high degree of compactness of these surfaces as defined by their length:width ratio. The occurrence of initial depressions (valley heads) seems
  • Asia ; Glaciation ; Glacier fluctuation ; Holocene ; Karokoram ; Moraine ; Palaeoclimate ; Palaeogeography ; Snow line ; Tibet ; Tien Shan
  • The historical to post-glacial glacier positions have been reconstructed from the recent glaciation history of selected examples. A chronological classification of the glacial events in phases can be defined by calculating the snow-line depression