Sea Ice

  • An evidence session with room for a better question

    An evidence session with room for a better question

    Design a school or community session around one source, a testable claim, accessible participation, and a traceable answer rather than a roomful of pledges.

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  • Read the Arctic Report Card beyond the headlines

    Read the Arctic Report Card beyond the headlines

    Follow a headline into its definition, table, calendar, and method, from daily sea ice minima to the limits of an observing-network assessment.

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  • Testing a changing Arctic food web

    Testing a changing Arctic food web

    A Bering and Chukchi Sea synthesis tests borealization against a different food-web mechanism. Mixed species responses, sampling gaps, and an exceptional first year sharpen the conclusion.

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  • What an ice chart cannot promise

    What an ice chart cannot promise

    Valid times, egg codes, partial concentrations, and chart coverage matter. Learn why a regional ice analysis cannot guarantee route connectivity, local strength, or a safe journey.

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  • A sea-ice pixel is not a habitat map

    A sea-ice pixel is not a habitat map

    Identical ice concentrations can conceal different floes, openings, and feeding opportunities. Habitat interpretation needs geometry, seabed context, compatible dates, and evidence of what animals actually use.

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  • The warmth beneath the Arctic surface

    The warmth beneath the Arctic surface

    Atlantic-origin warmth can sit below cold surface water. Density layers, currents, and mixing determine when stored ocean heat becomes heat delivered to sea ice.

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  • The bloom can begin before open water

    The bloom can begin before open water

    Under-ice blooms complicate the seasonal calendar. Light transmission, nutrients, consumer timing, and satellite blind spots explain why open water is not the food web’s starting gun.

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  • A drifting instrument is not a fixed station

    A drifting instrument is not a fixed station

    A rising temperature line may record movement through a water-mass boundary. Following position, depth, and salinity helps distinguish spatial structure from change through time.

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  • Snow on sea ice has two seasons

    Snow on sea ice has two seasons

    Why a snow blanket can slow winter ice growth yet delay spring melt, and why depth, density, timing, and wind redistribution belong in the comparison.

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