13 research outputs found

    Version 2 of the EUMETSAT OSI SAF and ESA CCI sea-ice concentration climate data records

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    We introduce the OSI-450, the SICCI-25km and the SICCI-50km climate data records of gridded global sea-ice concentration. These three records are derived from passive microwave satellite data and offer three distinct advantages compared to existing records: first, all three records provide quantitative information on uncertainty and possibly applied filtering at every grid point and every time step. Second, they are based on dynamic tie points, which capture the time evolution of surface characteristics of the ice cover and accommodate potential calibration differences between satellite missions. Third, they are produced in the context of sustained services offering committed extension, documentation, traceability, and user support. The three records differ in the underlying satellite data (SMMR &amp; SSM/I &amp; SSMIS or AMSR-E &amp; AMSR2), in the imaging frequency channels (37&thinsp;GHz and either 6 or 19&thinsp;GHz), in their horizontal resolution (25 or 50&thinsp;km), and in the time period they cover. We introduce the underlying algorithms and provide an evaluation. We find that all three records compare well with independent estimates of sea-ice concentration both in regions with very high sea-ice concentration and in regions with very low sea-ice concentration. We hence trust that these records will prove helpful for a better understanding of the evolution of the Earth's sea-ice cover.</p

    Fra Sputnik... - til moderne iskortlægning

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    Siden opsendelsen af den f&oslash;rste&nbsp;satellit i 1957 er der sket en rivende&nbsp;udvikling inden for anvendelsen af&nbsp;satellitdata. I Danmark har man for&nbsp;eksempel brugt data til meteorologiske&nbsp;analyser p&aring; DMI. I de seneste &aring;r&nbsp;har kortl&aelig;gningen af havis-udbredelsen&nbsp;med satellit v&aelig;ret et v&aelig;sentligt&nbsp;bevis p&aring;, at vores klima er under&nbsp;forandring

    Nordpolen på skrump - dækket af "tynd" vinteris

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    Siden man begyndte at kortl&aelig;gge&nbsp;havisen i Polhavet med satellitdata,&nbsp;har Nordpolen b&aring;de sommer&nbsp;og vinter v&aelig;ret d&aelig;kket af fl ere &aring;r&nbsp;gammel og 3-4 m tyk is &ndash; ogs&aring; kaldet&nbsp;polaris. Polarisen d&aelig;kkede f&oslash;r&nbsp;i tiden n&aelig;sten hele Polhavet med&nbsp;undtagelse af havet nord for Alaska,&nbsp;Bering Str&aelig;det og de Sibirske shelfomr&aring;der.&nbsp;I l&oslash;bet af februar 2008&nbsp;h&aelig;ndte det s&aring;, at et us&aelig;dvanligt&nbsp;stort omr&aring;de med is dannet denne&nbsp;vinter (vinteris) fra Bering Str&aelig;det&nbsp;og Sibirien for f&oslash;rste gang, mens&nbsp;man har m&aring;lt, n&aring;ede helt hen over&nbsp;Nordpolen. Vinteris bliver typisk&nbsp;ikke mere end 2 m tykt i l&oslash;bet af en&nbsp;hel vinter i Polhavet
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