Different Responses of Vegetation to Frozen Ground Degradation in the Source Region of the Yellow Ri

• 作 者: WANG Rui DONG Zhibao ZHOU Zhengchao
• 机 构: School of Geography and Tourism,Shaanxi Normal University,Xi’an 710119,China
• 出 处: 中国地理科学（英文版）
• 发表日期: 2020年4期
• 关键词: permafrost seasonally frozen ground vegetation dynamics climate change source re

Frozen ground degradation under a warming climate profoundly influences the growth of alpine vegetation in the source re-gion of the Qinghai-Tibet Plateau. This study investigated spatiotemporal variations in the frozen ground distribution, the active layer thickness (ALT) of permafrost (PF) soil and the soil freeze depth (SFD) in seasonally frozen soil from 1980 to 2018 using the tempera-ture at the top of permafrost (TTOP) model and Stefan equation. We compared the effects of these variations on vegetation growth among different frozen ground types and vegetation types in the source region of the Yellow River (SRYR). The results showed that approximately half of the PF area (20.37％ of the SRYR) was projected to degrade into seasonally frozen ground (SFG) during the past four decades; furthermore, the areal average ALT increased by 3.47 cm/yr, and the areal average SFD decreased by 0.93 cm/yr from 1980 to 2018. Accordingly, the growing season Normalized Difference Vegetation Index (NDVI) presented an increasing trend of 0.002/10yr, and the increase rate and proportion of areas with NDVI increase were largest in the transition zone where PF degraded to SFG (the PF to SFG zone). A correlation analysis indicated that variations in ALT and SFD in the SRYR were significantly correlated with increases of NDVI in the growing season. However, a rapid decrease in SFD (