Cleveland
发表于 2025-3-21 19:12:23
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愤怒历史
发表于 2025-3-21 22:26:28
Cryosols as a Three-Part System,st layer. Soil formation is especially pronounced in the active layer but also occurs in the transition from warmer periods. The active layer varies from 0.1 m in high latitude environments to more than 10 m in low-latitude mountains. The active layer shows the maximum degree of cryoturbation, may c
释放
发表于 2025-3-22 01:00:40
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谄媚于人
发表于 2025-3-22 08:20:05
Factors of Cryosol Formation,o continental. The mean annual air temperature ranges from +1 °C to −20 °C or colder; the mean annual precipitation ranges from <10 mm in interior Antarctica to more than 2,000 mm in high-mountain environments. High winds are common in many areas with cryosols. There is a variety of vegetation in th
惊呼
发表于 2025-3-22 11:43:58
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CODA
发表于 2025-3-22 16:06:09
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CODA
发表于 2025-3-22 18:11:47
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Exposure
发表于 2025-3-23 01:09:42
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GLADE
发表于 2025-3-23 04:05:27
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Nibble
发表于 2025-3-23 06:42:32
Alpine Cryosols,or −6 °C may be necessary for the active layer to be within 1–2 m of the ground surface in alpine regions. Many alpine plants are circumpolar, meaning that they occur throughout the Arctic and mountains at lower latitudes in the Northern Hemisphere. The properties of alpine cryosols are highly varia