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      Iceberg properties and distributions in three Greenlandic fjords using satellite imagery

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          ABSTRACT

          Icebergs calved from tidewater glaciers represent about one third to one half of the freshwater flux from the Greenland ice sheet to the surrounding ocean. Using multiple satellite datasets, we quantify the first fjord-wide distributions of iceberg sizes and characteristics for three fjords with distinct hydrography and geometry: Sermilik Fjord, Rink Isbræ Fjord and Kangerlussuup Sermia Fjord. We estimate average total iceberg volumes in summer in the three fjords to be 6.4 ± 1.5, 1.7 ± 0.40 and 0.16 ± 0.09 km 3, respectively. Iceberg properties are influenced by glacier calving style and grounding line depth, with variations in size distribution represented by exponents of power law distributions that are −1.95 ± 0.06, −1.87 ± 0.05 and −1.62 ± 0.04, respectively. The underwater surface area of icebergs exceeds the subsurface area of glacial termini by at least one order of magnitude in all three fjords, underscoring the need to include iceberg melt in fjord freshwater budgets. Indeed, in Sermilik Fjord, we calculate summertime freshwater flux from iceberg melt of 620 m 3 s −1 (±140 m 3 s −1), similar in magnitude to subglacial discharge. The method developed here can be extended across Greenland to assess relationships between glacier calving, iceberg discharge and freshwater production.

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          Most cited references15

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          Convection-Driven Melting near the Grounding Lines of Ice Shelves and Tidewater Glaciers

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            21st-century evolution of Greenland outlet glacier velocities.

            Earlier observations on several of Greenland's outlet glaciers, starting near the turn of the 21st century, indicated rapid (annual-scale) and large (>100%) increases in glacier velocity. Combining data from several satellites, we produce a decade-long (2000 to 2010) record documenting the ongoing velocity evolution of nearly all (200+) of Greenland's major outlet glaciers, revealing complex spatial and temporal patterns. Changes on fast-flow marine-terminating glaciers contrast with steady velocities on ice-shelf-terminating glaciers and slow speeds on land-terminating glaciers. Regionally, glaciers in the northwest accelerated steadily, with more variability in the southeast and relatively steady flow elsewhere. Intraregional variability shows a complex response to regional and local forcing. Observed acceleration indicates that sea level rise from Greenland may fall well below proposed upper bounds.
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              Classification and Extraction of Spatial Features in Urban Areas Using High-Resolution Multispectral Imagery

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                Author and article information

                Journal
                applab
                Annals of Glaciology
                Ann. Glaciol.
                Cambridge University Press (CUP)
                0260-3055
                1727-5644
                April 2017
                May 3 2017
                April 2017
                : 58
                : 74
                : 92-106
                Article
                10.1017/aog.2017.5
                5e4fb81c-e08c-40d0-be57-3b70c608cec0
                © 2017
                History

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