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Cartography of snowcover properties from topographical, vegetation and meteorological data.

机译:根据地形,植被和气象数据绘制的积雪性质地图。

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摘要

A Multi Layer Snow Accumulation Model (MLSAM) was developed to simulate snow cover properties. The simulations include snow depth, snow density and snow-cover. The model was tested near Schefferville (54°48'N, 66°49'W) for the years (1986-1987 and 1987-1988). The MLSAM combines three sub models: 1) An intermediate-complexity, quasi-physically based, meteorological model (MicroMet), 2) A Point Energy/Mass Balance (PEMB) model and 3) A Distributed Blowing Snow Model (DBSM). The MLSAM employs digital terrain models with grid increments of 20 m and run with temporal increments of 24 hours using standard Canadian digital elevation and vegetation models and climate data.;The model outputs for snow-layer depth and density as well as snow cover remaining at different times during the melt season were compared with available data from the Schefferville climate station and from previous snow research at Schefferville. Landsat images were used for assessing simulations of snow cover during melt.;In general, the model performed well until the onset of melt. Thereafter the model greatly over-predicted melt rates. There were also problems with melt water transfers in the snow cover which will need to be addressed in future versions of the model. Improvements will also need to be made to the routines handling vapour transfers in the snowpack and snow density calculations. However, with these modifications the model shows some promise to become a useful model for simulation of spatial and temporal variations in snow cover properties.;Keywords: Snow depth, Snow density profile, Snow Melt, Snow Cover mapping, Landsat image, Mass and Energy Balance, Geographic Information System (GIS).
机译:开发了多层积雪模型(MLSAM)以模拟积雪的性质。模拟包括雪深,雪密度和积雪。多年来(1986-1987年和1987-1988年)在谢弗维尔(54°48'N,66°49'W)附近测试了该模型。 MLSAM组合了三个子模型:1)中等复杂度,基于准物理的气象模型(MicroMet),2)点能量/质量平衡(PEMB)模型和3)分布式吹雪模型(DBSM)。 MLSAM使用数字地形模型,网格增量为20 m,并使用标准的加拿大数字高程和植被模型以及气候数据以24小时的时间增量运行;模型输出的雪层深度和密度以及积雪量保持在将融雪季节的不同时间与Schefferville气候站和先前Schefferville降雪研究的可用数据进行了比较。 Landsat图像用于评估融雪期间的积雪模拟。通常,该模型在融雪开始之前表现良好。此后,该模型极大地高估了熔化速率。积雪中融水的转移也存在问题,该模型的未来版本中将需要解决。还需要对处理积雪和雪密度计算中的蒸气转移的例程进行改进。然而,经过这些修改,该模型显示出有望成为模拟积雪性质的时空变化的有用模型。关键词:积雪深度,积雪密度剖面,积雪融化,积雪覆盖图,Landsat图像,质量和能量天平,地理信息系统(GIS)。

著录项

  • 作者

    Harirforoush, Hilda.;

  • 作者单位

    Universite de Sherbrooke (Canada).;

  • 授予单位 Universite de Sherbrooke (Canada).;
  • 学科 Physical Geography.;Environmental Sciences.;Remote Sensing.
  • 学位 M.Sc.
  • 年度 2012
  • 页码 88 p.
  • 总页数 88
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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