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        "roles": [
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    "sat:platform_international_designator": "2014-016A",
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        "citation": "Doin, M.-P., Lodge, F., Guillaso, S., Jolivet, R., Lasserre, C., Ducret, G., Grandin, R., Pathier, E., Pinel, V. (2011). Presentation of the small baseline NSBAS processing chain on a case example: The Etna deformation monitoring from 2003 to 2010 using Envisat data. In Proceedings of FRINGE 2011 ESA Workshop, Frascati, Italy,19–23 September 2011, ESA Publication SP-697.",
        "doi": ""
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        "citation": "Raphaël Grandin (Institut de Physique du Globe de Paris, France) (2015). \"Interferometric Processing of SLC Sentinel-1 TOPS Data \". In Proceedings of FRINGE’15: Advances in the Science and Applications of SAR Interferometry and Sentinel-1 InSAR Workshop, Frascati, Italy, 23-27 March 2015, Ouwehand L., Ed., ESA Publication SP-731.",
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      "description": "# Filtered Wrapped Interferogram\n\n> This product corresponds to the **filtered wrapped interferogram**.\n>\n> The geotiff file has 2 bands:\n>\n> - band 1 is the filtered wrapped phase (phase difference between the two acquisitions) of the interferogram, corrected from stratified atmospheric delay (if asked) and from spectral diversity. It is by default filtered by a moving average, triangular window, filter. Multilooking is that defined with Rlooks_unw and given in nsbas.proc file.\n> - band 2 is either the product of the two image’s amplitudes (if ROIPAC Goldstein filter is used) or a coherence (if a Sliding window filter is used (SW)). The coherence is obtained when the sliding window average is applied on the wrapped interferogram phase: it thus quantifies the quality of the filtered phase (1: good quality, 0: no coherence).\n>\n> The png file has 1 band:\n>\n> - band 1 is the filtered wrapped phase of the interferogram, normalized by a color palette.\n\n[source](https://formater.pages.in2p3.fr/flatsim/products/InWF.html)\n",
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