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      Additional Arctic observations improve weather and sea-ice forecasts for the Northern Sea Route

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          Abstract

          During ice-free periods, the Northern Sea Route (NSR) could be an attractive shipping route. The decline in Arctic sea-ice extent, however, could be associated with an increase in the frequency of the causes of severe weather phenomena, and high wind-driven waves and the advection of sea ice could make ship navigation along the NSR difficult. Accurate forecasts of weather and sea ice are desirable for safe navigation, but large uncertainties exist in current forecasts, partly owing to the sparse observational network over the Arctic Ocean. Here, we show that the incorporation of additional Arctic observations improves the initial analysis and enhances the skill of weather and sea-ice forecasts, the application of which has socioeconomic benefits. Comparison of 63-member ensemble atmospheric forecasts, using different initial data sets, revealed that additional Arctic radiosonde observations were useful for predicting a persistent strong wind event. The sea-ice forecast, initialised by the wind fields that included the effects of the observations, skilfully predicted rapid wind-driven sea-ice advection along the NSR.

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          Storm-induced sea-ice breakup and the implications for ice extent.

          The propagation of large, storm-generated waves through sea ice has so far not been measured, limiting our understanding of how ocean waves break sea ice. Without improved knowledge of ice breakup, we are unable to understand recent changes, or predict future changes, in Arctic and Antarctic sea ice. Here we show that storm-generated ocean waves propagating through Antarctic sea ice are able to transport enough energy to break sea ice hundreds of kilometres from the ice edge. Our results, which are based on concurrent observations at multiple locations, establish that large waves break sea ice much farther from the ice edge than would be predicted by the commonly assumed exponential decay. We observed the wave height decay to be almost linear for large waves--those with a significant wave height greater than three metres--and to be exponential only for small waves. This implies a more prominent role for large ocean waves in sea-ice breakup and retreat than previously thought. We examine the wider relevance of this by comparing observed Antarctic sea-ice edge positions with changes in modelled significant wave heights for the Southern Ocean between 1997 and 2009, and find that the retreat and expansion of the sea-ice edge correlate with mean significant wave height increases and decreases, respectively. This includes capturing the spatial variability in sea-ice trends found in the Ross and Amundsen-Bellingshausen seas. Climate models fail to capture recent changes in sea ice in both polar regions. Our results suggest that the incorporation of explicit or parameterized interactions between ocean waves and sea ice may resolve this problem.
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            Verification of global numerical weather forecasting systems in polar regions using TIGGE data

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              Author and article information

              Journal
              Sci Rep
              Sci Rep
              Scientific Reports
              Nature Publishing Group
              2045-2322
              20 November 2015
              2015
              : 5
              : 16868
              Affiliations
              [1 ]National Institute of Polar Research , Tokyo, Japan
              [2 ]Japan Agency for Marine-Earth Science and Technology , Kanagawa, Japan
              [3 ]SOKENDAI (Graduate University for Advanced Studies) , Tokyo, Japan
              [4 ]Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research , Potsdam, Germany
              [5 ]Environment Canada , Toronto, Canada
              [6 ]The University of Tokyo , Chiba, Japan
              Author notes
              Article
              srep16868
              10.1038/srep16868
              4653624
              26585690
              62f7bc84-fc25-4240-b1eb-76456531d396
              Copyright © 2015, Macmillan Publishers Limited

              This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

              History
              : 22 May 2015
              : 21 October 2015
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