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氷楔

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Permafrost temperature profile. Permafrost occupies the middle zone, with the active layer above it, while geothermal activity keeps the lowest layer above freezing. The vertical 0 °C or 32 °F line denotes the average annual temperature that is crucial for the upper and lower limit of the permafrost zone, while the red lines represent seasonal temperature changes and seasonal temperature extremes. Solid curved lines at the top show seasonal maximum and minimum temperatures in the active layer, while the red dotted-to-solid line depicts the average temperature profile with depth of soil in a permafrost region.

永久凍土の正体と地球環境への影響気候変動がもたらすリスクと科学的視点

永久凍土気候変動メタン放出能動層
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Example of a periglacial landscape with both pingos and polygon wedge ice near Tuktoyaktuk, Northwest Territories, Canada

周氷河環境のメカニズムと地形的特徴

周氷河永久凍土凍結融解作用周氷河地形
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