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

Cleveland

書目名稱Cryopedology影響因子(影響力)




書目名稱Cryopedology影響因子(影響力)學科排名




書目名稱Cryopedology網(wǎng)絡(luò)公開度




書目名稱Cryopedology網(wǎng)絡(luò)公開度學科排名




書目名稱Cryopedology被引頻次




書目名稱Cryopedology被引頻次學科排名




書目名稱Cryopedology年度引用




書目名稱Cryopedology年度引用學科排名




書目名稱Cryopedology讀者反饋




書目名稱Cryopedology讀者反饋學科排名

憤怒歷史

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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諂媚于人

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

驚呼

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