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HESS | Articles | Volume 22, issue 9
Hydrol. Earth Syst. Sci., 22, 4685–4697, 2018
https://doi.org/10.5194/hess-22-4685-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: Integration of Earth observations and models for global water...

Hydrol. Earth Syst. Sci., 22, 4685–4697, 2018
https://doi.org/10.5194/hess-22-4685-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 07 Sep 2018

Research article | 07 Sep 2018

Global re-analysis datasets to improve hydrological assessment and snow water equivalent estimation in a sub-Arctic watershed

David R. Casson et al.
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Cited articles  
Allen, R. G., Pereira, L. S., Raes, D., and Smith, M: Crop evapotranspiration-Guidelines for computing crop water requirements, FAO Irrigation and drainage paper, 56, 6541, 1998. 
AMAP: Arctic Climate Issues 2011: Changes in Arctic Snow, Water, Ice and Permafrost, SWIPA 2011, Gaustadalléen 21, 0349 Oslo, Norway, 2012. 
Beck, H., van Dijk, A., Leviizzani, V., Schellekens, J., Miralles, G., Martrens, B., de Roo, A., Pappenberger, F., Huffman, G., and Wood, E.: MSWEP: 3-hourly 0.1? fully global precipitation (1979–present) by merging gauge, satellite, and weather model data [Abstract], Geophysical Research Abstracts, 19, 2017. 
Beck, H. E., van Dijk, A. I. J. M., Levizzani, V., Schellekens, J., Miralles, D. G., Martens, B., and de Roo, A.: MSWEP: 3-hourly 0.25 global gridded precipitation (1979–2015) by merging gauge, satellite, and reanalysis data, Hydrol. Earth Syst. Sci., 21, 589–615, https://doi.org/10.5194/hess-21-589-2017, 2017. 
Bergström, S.: The HBV Model – its structure and applications, NORRKÖPING, Sweden, 1992. 
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In high-latitude (> 60° N) watersheds, measuring the snowpack and predicting of snowmelt runoff are uncertain due to the lack of data and complex physical processes. This provides challenges for hydrological assessment and operational water management. Global re-analysis datasets have great potential to aid in snowpack representation and snowmelt prediction when combined with a distributed hydrological model, though they still have clear limitations in remote boreal forest and tundra environments.
In high-latitude ( 60° N) watersheds, measuring the snowpack and predicting of snowmelt runoff...
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