Zhang

Changes in Freeze-Thaw and Permafrost Dynamics and Their Hydrological Implication over the Russian Arctic Drainage Basin: 

Changes in Freeze-Thaw and Permafrost Dynamics and Their Hydrological Implication over the Russian Arctic Drainage Basin Tingjun Zhang and R. G. Barry National Snow and Ice Data Center University of Colorado at Boulder Freshwater Investigators Meeting Boulder, Feb. 18-19, 2003 NSF OPP-0229766

Problems:: 

Problems: Zhang and Barry, 2003, NSIDC It has been reported (Yang et al., JGR, 2002; Serreze et al., JGR, 2002) that runoff has increased about 25% to 90% during cold season (October to April) over the Russian Arctic drainage basin in the past several decades. QUESTION: What causes the increase in discharge over the Eurasian arctic rivers, especially during the winter months?

Objective: to investigate the response of soil thermal, freeze-thaw, and permafrost dynamics to climatic change and their impact on the hydrologic cycle in the Russian arctic drainage basin over the past 50 years (1950-2000). Specifically, we will:: 

Objective: to investigate the response of soil thermal, freeze-thaw, and permafrost dynamics to climatic change and their impact on the hydrologic cycle in the Russian arctic drainage basin over the past 50 years (1950-2000). Specifically, we will: Investigate the impact of changes in freeze-thaw and permafrost dynamics on the arctic hydrological cycle Collect, rescue, and synthesize soil temperature, freeze-thaw cycle, and permafrost data from 400 stations over the Russian arctic drainage basin Zhang and Barry, 2003, NSIDC

Hypothesis:: 

Hypothesis: Climatic Warming Zhang and Barry, 2003, NSIDC

Data Sets Needed:: 

Data Sets Needed: Existing Data Sets: IPA permafrost map (1:10,000,000) (Brown et al., 1997; Zhang et al., 1999) Gridded air temperature and precipitation (Jones et al., 1995) River runoff, precipitation, etc. (Legates and Willmott, 1990; Groisman, 1991; Lammers et al., 2001) New Data Sets from this study: Digital Russian permafrost map (1:1,000,000) by Yershov et al. (1998). Soil and permafrost temperature Active layer thickness Thawing index of air temperature Length of thaw season Zhang and Barry, 2003, NSIDC

Slide6: 

240 stations (red dots): up to 1990; update to 2000. 110 new stations (blue dots) to 2000. 50 new stations (green dots) up to 1990. 110 new stations from Mongolia up to 2002 (not shown). Zhang and Barry, 2003, NSIDC

Soil temperature increase at each river basin (1969-1990): : 

Soil temperature increase at each river basin (1969-1990): Ob: 1.2oC Yenisey: 0.8oC Lena: 1.5oC Increase in soil temperature basin-wide leads to thickening the active layer and thawing of permafrost. Zhang and Barry, 2003, NSIDC

Active Layer:: 

Active Layer: Variations of active layer thickness from 11 stations from Lena river basin. Variation of the thawing index estimated from mean monthly air temperature for each basin. Ground-based measurements indicate that active layer thickness increased about 30 cm from late 1960 to 1985 over Lena river basin. Thawing index has increased significantly from late 1960s to the late 1990s, implying thickening of the active layer basin-wide. Zhang and Barry, 2003, NSIDC

Impacts to Runoff (Discharge):: 

Impacts to Runoff (Discharge): These values are estimated using ground ice data from IPA permafrost map. Runoff is in mm over the period from 1965 to 1985 and discharge in km3/yr. Zhang and Barry, 2003, NSIDC

Impact to Runoff (Discharge): 

Impact to Runoff (Discharge) During the period from 1965 through 1985, discharge equivalent due to the melting of excess ground ice over the Ob, Yenisey, and Lena river basins: Active Layer Thickness Increase Discharge Equivalent 10 cm 2.1 to 2.9 km3/year 20 cm 4.2 to 5.8 km3/year 30 cm 6.3 to 8.7 km3/year Possible water sources contributing to: Evaporation Wetland and thaw lake contribution River discharge Zhang and Barry, 2003, NSIDC

Impact on winter runoff: 

Impact on winter runoff Lateral thawing of permafrost contributes to winter runoff. Active layer thickness is positively correlated with winter runoff. Zhang and Barry, 2003, NSIDC

Acknowledgments:: 

Acknowledgments: This study is supported by: NSF Office of Polar Program Thank You!