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            "title": "Prospects for the Interactive Multisensor Snow and Ice Mapping System (IMS)",
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            "title": "Evaluation of snow products over the Tibetan Plateau",
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            "abstractNote": "Four satellite-based snow products are evaluated over the Tibetan Plateau for the 2007–2010 snow seasons. The Moderate Resolution Imaging Spectroradiometer (MODIS) Terra and Aqua snow cover daily L3 Global 500-m grid products (MOD10A1 and MYD10A1), the National Oceanic and Atmospheric Administration Interactive Multisensor Snow and Ice Mapping System (IMS) daily Northern Hemisphere snow cover product and the Advanced Microwave Scanning Radiometer – Earth Observing System Daily Snow Water Equivalent were validated against Thematic Mapper (TM) snow cover maps of Landsat-5 and meteorological station snow depth observations. The overall accuracy of MOD10A1, MYD10A1 and IMS is higher than 91% against stations observations and than 79% against Landsat TM images. In general, the daily MODIS snow cover products show better performance than the multisensor IMS product. However, the IMS snow cover product is suitable for larger scale (~4km) analysis and applications, with the advantage over MODIS to allow for mitigation for cloud cover. The accuracy of the three products decreases with decreasing snow depth. Overestimation errors are most common over forested regions; the IMS and Advanced Microwave Scanning Radiometer – Earth Observing System Snow Water Equivalent products also show poorer performance that the MODIS products over grassland. By identifying weaknesses in the satellite products, this study provides a focus for the improvement of snow products over the Tibetan plateau. The quantitative evaluation of the products proposed here can also be used to assess their relative weight in data assimilation, against other data sources, such as modelling and in situ measurement networks. Copyright © 2015 John Wiley & Sons, Ltd.",
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            "title": "Using Satellite-Derived Snow Cover Data to Implement a Snow Analysis in the Met Office Global NWP Model",
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                    "firstName": "C.",
                    "lastName": "Xiyu"
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            "abstractNote": "The Interactive Multisensor Snow and Ice Mapping System (IMS) combines multiple data sources to map global snow cover. IMS can discriminate snow cover beneath clouds using time sequential imagery from geostationary satellites and passive microwave observations. During the snow disaster of 2008 in southern China, the IMS snow cover data identified more snow than those retrieved from passive microwave remote sensing data. In this study, the IMS snow cover mapping accuracy was assessed against the Landsat Enhanced Thematic Mapper Plus (ETM+) imagery. Land cover and terrain effects on the snow cover accuracy were considered. Good agreements (> 90%) was observed over flat cropland surfaces. For forested, mountainous areas, a pronounced disagreement was observed between the two datasets. The accuracy of the IMS in these regions was less than 50%. Due to the sparse distributed snow cover in these regions, the effects of snow cover fragmentation degrees were studied.",
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            "publicationTitle": "Arabian Journal of Geosciences",
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            "title": "The interactive multisensor snow and ice mapping system",
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            "abstractNote": "The interactive multisensor snow and ice mapping system (IMS) was developed to give snow and ice analysts the tools, on one platform, to inspect visually the imagery and mapped data from various sensor sources to determine the presence of snow and ice and to depict snow- and ice-covered areas on a map on a daily basis, in one hour or less. Snow and ice analysts in the National Environmental Satellite, Data, and Information Service have been creating weekly maps showing the extent of snow cover for the Northern Hemisphere since 1966 using visible imagery from polar-orbiting and geostationary satellites and surface observations as data sources. The current process is mostly manual and time-consuming, taking up to 10 hours to produce a map during the snow season. Where cloud cover precludes an unobstructed view of an area during the entire week, the analysis from the previous week is carried forward. Each week the analyst draws a new map by hand, then digitizes the extent of snow and ice cover using an 89×89 line grid overlaid on a stereographic map of the Northern Hemisphere. The hand-drawn map is photocopied and distributed and the digitized map is saved to a file for use in National Weather Service numerical models and for archival storage. IMS was designed and built to replace and improve this process by producing a more accurate and timely product. © 1998 John Wiley & Sons, Ltd.",
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