Articles | Volume 15, issue 3
Ocean Sci., 15, 615–630, 2019
https://doi.org/10.5194/os-15-615-2019

Special issue: The Copernicus Marine Environment Monitoring Service (CMEMS):...

Ocean Sci., 15, 615–630, 2019
https://doi.org/10.5194/os-15-615-2019

Research article 29 May 2019

Research article | 29 May 2019

Validation metrics for ice edge position forecasts

Arne Melsom et al.

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Arne Melsom
The Cryosphere, 15, 3785–3796, https://doi.org/10.5194/tc-15-3785-2021,https://doi.org/10.5194/tc-15-3785-2021, 2021
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Cited articles

Arzel, O., Fichefet, T., and Goosse, H.: Sea ice evolution over the 20th and 21st centuries as simulated by current AOGCMs, Ocean Model., 12, 401–415, https://doi.org/10.1016/j.ocemod.2005.08.002, 2006. a
Bell, M.-J., Schiller, A, Le Traon, P.-Y., Smith, N. R., Dombrowsky, E., and Wilmer-Becker, K.: An introduction to GODAE OceanView, J. Op. Oceanogr., 8, 2–11, https://doi.org/10.1080/1755876X.2015.1022041, 2015. a
Breivik, L.-A., Eastwood, S, Godøy, Ø, Schyberg, H, Andersen, S., Tonboe, R. T.: Sea Ice Products for EUMETSAT Satellite Application Facility, Can. J. Remote Sens., 27, 403–410, https://doi.org/10.1080/07038992.2001.10854883, 2001. a
Carrieres, T., Casati, B., Caya, A., Posey, P., Metzger, E. J., Melsom, A., Sigmond, M., Kharin, V., and Dupont, F.: System evaluation, in: Sea Ice Analysis and Forecasting, edited by: Carrieres T., Buehner M., Lemieux J. F., and Pedersen, L. T., Cambridge University Press, https://doi.org/10.1017/9781108277600, 2017. a, b
Dukhovskoy, D. S., Ubnoske, J., Blanchard-Wrigglesworth, E. , Hiester, H. R., and Proshutinsky, A.: Skill metrics for evaluation and comparison of sea ice models, J. Geophys. Res.-Oceans, 120, 5910–5931, https://doi.org/10.1002/2015JC010989, 2015. a, b, c, d, e
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Retreating sea ice in the Arctic Ocean gives rise to increased naval traffic with shorter navigation distances. Hence, information about the position of the sea ice edge is crucial for safe navigation. In the present study we explore methods for examining the quality of sea ice edge forecasts. We conclude that the forecast quality can be monitored with results from a set of four quantities. We also recommend the use of maps which display discrepancies in the positions of the sea ice edge.