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Showing 1 - 20 results of 59 for search '"meltwater"', query time: 0.40s Refine Results
  1. 1
    ... simulations, the authors show that clouds enhance Greenland ice sheet meltwater runoff by more than 30%....
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  2. 2
    ...Forty years of satellite imagery reveal that meltwater lakes on the margin of the Greenland Ice...
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  3. 3
    ...Forty years of satellite imagery reveal that meltwater lakes on the margin of the Greenland Ice...
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  4. 4
    ... GRACE-based solutions and different meltwater runoff estimates (namely, RACMO2.3, SNOWPACK, and MAR3.9...
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  5. 5
    ... GRACE-based solutions and different meltwater runoff estimates (namely, RACMO2.3, SNOWPACK, and MAR3.9...
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  6. 6
    .... In total, we calculate that 6.6 ± 1.0 km3 of surface meltwater ran off the ice sheet in the Kangerlussuaq...
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  7. 7
    .... In total, we calculate that 6.6 ± 1.0 km 3 of surface meltwater ran off the ice sheet in the Kangerlussuaq...
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  8. 8
    ... of surface meltwater production, resulting in the migration of melt and percolation regimes to higher...
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  9. 9
    ... of surface meltwater production, resulting in the migration of melt and percolation regimes to higher...
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  10. 10
    ... lubricating seasonal meltwater to reach the base of the Greenland Ice Sheet. Here we use new surface velocity...
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  11. 11
    ... lubricating seasonal meltwater to reach the base of the Greenland Ice Sheet. Here we use new surface velocity...
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  12. 12
    ... meltwater percolates into the firn pack in summer, which is then buried by snowfall and does not refreeze...
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  13. 13
  14. 14
    ... negative surface mass budget (SMB) and surface meltwater run-off. The observed run-off was due to a large...
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  15. 15
    ... time series with respect to both modeled meltwater runoff, obtained from RACMO2.3p2, and glacier front...
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  16. 16
    ... of the firn layer is critical to linking meltwater production to meltwater runoff. Firn-densification models...
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  17. 17
    ... of the firn layer is critical to linking meltwater production to meltwater runoff. Firn-densification models...
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  18. 18
    ... and the remainder by D. The decrease in SMB is fully driven by an increase in surface melt and subsequent meltwater...
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  19. 19
    ... and the remainder by D . The decrease in SMB is fully driven by an increase in surface melt and subsequent meltwater...
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  20. 20
    ... meltwater percolates into the firn pack in summer, which is then buried by snowfall and does not refreeze...
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