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Published byEmma French Modified over 6 years ago
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Annual accumulation for Greenland updated using ice-core data developed during & analysis of daily coastal data Roger Bales, UC Merced Dayong Shen, UC Merced Joe McConnell, Desert Research Institute John Burkhart, Norwegian Institute for Air Research Qinghua Guo, UC Merced
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PARCA 2001 accumulation map
Mean: 30 g cm2 a-1 South: g cm2 a-1 Northeast: g cm2 a-1 West: g cm2 a-1 Uncertainties High-accumulation gradients in south Coastal up to dry snow Bales et al., JGR 2001
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Coastal weather station data
2001 map 17 locations, monthly data Consolidated data from Ohmura’s 1999 analysis of 36 locations Only 8 stations with data past 1990, 5 more with records ending in 1980’s Wind corrections for undercatch in rain gages based on monthly averages Current analysis 22 DMI stations, daily data 13 with data past 2000 Most with data into 1980’s Wind corrections for undercatch in rain gages based on daily averages
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Trends at 8 stations co-located between Ohmura, 1999 & current analysis
6 sites: +2.6 mm/yr
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Offset at 8 stations co-located between Ohmura, 1999 & current analysis
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Bias corrections
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Data used in kriging 257 ice sheet points from Bales, 2001
39 new ice cores 20 new coastal stations 6 coastal stations from Ohmura, 1999
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Distribution of record lengths on ice sheet
Cumulative percent Years in record Mean about 10 yr Replaced single-year estimates
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PS-E Current minus 2001 map
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PS-E PC-E
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Total rather than solid precipitation as better estimate of accumulation in wet snow region?
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Basin-by-basin comparison
Current minus 2001 map Basin-by-basin comparison Basin Map values Pc-E Ps-E P-E* 1 38.4 37.7 2 39.0 40.0 3 53.5 42.4 49.1 4 65.2 60.7 52.0 5 56.5 55.2 49.7 6 35.6 34.3 7 18.2 18.0 8 13.6 13.3 13.9 9 12.3 10 15.3 15.2 15.4 11 28.0 27.2 27.4 12 32.7 32.0 32.5
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Summary of accumulation
Area Accumulation, g cm-2 yr-1 Pc - E Ps - E P-E* Greenland 36.5 29.0 29.8 Ice sheet 34.6 30.0 30.4 E ≥ 2000 m 31.8 29.9 1.7 1.1 – Standard error Standard error: from variance estimates plus covariance terms
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