Titlebook: Cryopedology; James G. Bockheim Book 2015 Springer International Publishing 2015 Antarctic Soils.Arctic Soils.Cryosols.Permafrost Book.Soi

Cleveland

书目名称Cryopedology影响因子(影响力)




书目名称Cryopedology影响因子(影响力)学科排名




书目名称Cryopedology网络公开度




书目名称Cryopedology网络公开度学科排名




书目名称Cryopedology被引频次




书目名称Cryopedology被引频次学科排名




书目名称Cryopedology年度引用




书目名称Cryopedology年度引用学科排名




书目名称Cryopedology读者反馈




书目名称Cryopedology读者反馈学科排名

愤怒历史

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

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谄媚于人

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

CODA

CODA

Exposure

GLADE

Nibble

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