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959 | 959 | "\n",
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960 | 960 | "### References\n",
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961 | 961 | "\n",
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962 |
| - "1. Tilling, R. L., Ridout, A., & Shepherd, A. (2018). Estimating Arctic sea ice thickness and volume using CryoSat-2 radar altimeter data. Advances in Space Research, 62(6), 1203-1225, [<span style=\"color:blue\">https://doi.org/10.1016/j.asr.2017.10.051</span>](https://doi.org/10.1016/j.asr.2017.10.051).\n", |
| 962 | + "1. Tilling, R. L., Ridout, A., & Shepherd, A. (2018). Estimating Arctic sea ice thickness and volume using CryoSat-2 radar altimeter data. Advances in Space Research, 62(6), 1203-1225, [<span style=\"color:blue\"> https://doi.org/10.1016/j.asr.2017.10.051 </span>](https://doi.org/10.1016/j.asr.2017.10.051).\n", |
963 | 963 | "\n",
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964 |
| - "2. Müller, F. L., Paul, S., Hendricks, S., and Dettmering, D. (2023). Monitoring Arctic thin ice: a comparison between CryoSat-2 SAR altimetry data and MODIS thermal-infrared imagery. The Cryosphere, 17, 809–825, [<span style=\"color:blue\">https://doi.org/10.5194/tc-17-809-2023</span>](https://doi.org/10.5194/tc-17-809-2023).\n", |
| 964 | + "2. Müller, F. L., Paul, S., Hendricks, S., and Dettmering, D. (2023). Monitoring Arctic thin ice: a comparison between CryoSat-2 SAR altimetry data and MODIS thermal-infrared imagery. The Cryosphere, 17, 809–825, [<span style=\"color:blue\"> https://doi.org/10.5194/tc-17-809-2023 </span>](https://doi.org/10.5194/tc-17-809-2023).\n", |
965 | 965 | "\n",
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966 |
| - "3. Rampal, P., J. Weiss, and D. Marsan (2009). Positive trend in the mean speed and deformation rate of Arctic sea ice, 1979–2007, J. Geophys. Res., 114, C05013, [<span style=\"color:blue\">https://doi.org/10.1029/2008JC005066</span>](https://doi.org/10.1029/2008JC005066)." |
| 966 | + "3. Rampal, P., J. Weiss, and D. Marsan (2009). Positive trend in the mean speed and deformation rate of Arctic sea ice, 1979–2007, J. Geophys. Res., 114, C05013, [<span style=\"color:blue\"> https://doi.org/10.1029/2008JC005066 </span>](https://doi.org/10.1029/2008JC005066)." |
967 | 967 | ]
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968 | 968 | }
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969 | 969 | ],
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