Abstract. Satellite remote sensing is a convenient tool for studying snow and glacier ice, allowing us to conduct research over large and otherwise inaccessible areas. This paper reviews various methods for measuring snow and glacier ice properties with satellite remote sensing. These methods have been improving with the use of new satellite sensors, like the synthetic aperture radar (SAR) during the last decade, leading to the development of new and powerful methods, such as SAR interferometry for glacier velocity, digital elevation model generation of ice sheets, or snow cover mapping. Some methods still try to overcome the limitations of present sensors, but future satellites will have much increased capability, for example, the ability to measure the whole optical spectrum or SAR sensors with multiple polarization or frequencies. Among the methods presented are the satellite-derived determination of surface albedo, snow extent, snow volume, snow grain size, surface temperature, glacier facies, glacier velocities, glacier extent, and ice sheet topography. In this review, emphasis is put on the principles and theory of each satellite remote sensing method. An extensive list of references, with an emphasis on studies from the 1990s, allows the reader to delve into specific topics.
INTRODUCTIONThere have been tremendous technological achievements in the twentieth century that enable scientists to undertake research at virtually every spot on Earth. In parallel, advances in space technology during the last decades have provided us with a rapidly increasing number of satellite platforms that can be used to study complex physical processes of the Earth-atmosphere system. The development within this field concerns not only the growing number of satellites but also the rapid progression of sensor capabilities. In the future a major challenge will be connected with combining various sources of information gathered from space, i.e., data assimilation, and to make use of this information in a systematic, repetitive manner to monitor temporal and spatial variability, for example, in climate-change research.In the field of glaciology, satellite remote sensing has proven to be a particularly useful tool because areas of interest are often inaccessible. Further, in many regions at high latitudes, like the Greenland and Antarctic ice sheets, it is only during parts of the year that effective ground-based research can be carried out due to the harsh climate environment and the lack of daylight. Satellite remote sensing often permits real-time, yearround, and long-term studies. Also, the large spatial coverage of satellite remotely sensed data enables monitoring and process studies over large areas. In this way, satellite data help in understanding processes and teleconnections on the regional, continental, or even global scale, for example, global satellite-derived maps of snow cover. Such products are particularly important because they assist interpretation and analysis concerning global change.Also, on smaller scales, sate...