Table 1 The observed mean ice speed from 2018, the observed and modelled rate of change in ice speed, the observed total and percentage change in ice speed from 1994 to 2018.

From: Widespread increase in dynamic imbalance in the Getz region of Antarctica from 1994 to 2018

Flow unit

2018 Mean speed (m/yr)

Observed rate of speed change (m/yr²)

Modelled rate of speed change (m/yr²)

Observed total speed up over 25 years (m/yr)

Observed percentage speed change over 25 years (%)

Rate of elevation change 1992–2017 (m/yr)

Grounding line migration 1996–2017 (km)

Ice thickness (m)

Bed elevation (m)

1

173.7 ± 11.5

0.7

0.8

18.6

10.7

0.0

−1.3

649

−540

2

192.2 ± 17.2

0.2

0.1

5.5

2.9

−0.2

−1.1

674

−594

3

182.6 ± 14.4

1.9

1.9

46.5

25.5

−0.7

−2.7

639

−541

4

390.7 ± 33.3

3.7

3.4

92.4

23.6

−1.0

775

−651

5

532.4 ± 36.1

10.5

9.1

263.4

49.5

−1.6

728

−613

6

668.8 ± 90.8

15.6

15.2

391.2

58.5

−1.8

851

−727

7

424.8 ± 42.2

1.0

2.1

24.5

5.8

−0.5

−2.5

638

−552

8

518.8 ± 59.1

2.0

5.4

50.4

9.7

−0.5

501

−418

9

511.2 ± 64.6

2.8

3.8

69.4

13.6

−0.1

552

−473

10

879.2 ± 149.1

9.1

11.4

228.2

26.0

−0.6

659

−535

11

744.3 ± 125.0

5.7

5.1

141.5

19.0

−2.2

913

659

12

467.8 ± 65.5

8.2

6.2

205.5

43.9

−1.3

995

−806

13

1397.6 ± 163.7

11.4

6.0

285.8

20.4

−0.4

674

−524

14

1281.1 ± 122.6

8.0

7.3

198.9

15.5

−0.6

701

−560

  1. All measurements were extracted from a 5-km-diameter region at the grounding line, on all 14 flow lines (Fig. 1a) in the Getz study region. Measurements of grounding line migration are provided where observations exist, along with the mean FDM corrected ice thickness and bed elevation32 also extracted from the 5 km region at the grounding line. Ice sheet elevation change8 was extracted from a 20-km-diameter region due to the coarser spatial resolution of this dataset. Italics denote flow units (11 and 13) with less than 70% coverage in the 5 km region on the observed speed change map. Grounding line migration is calculated as the distance along the central flow line the grounding line has moved, negative indicating a movement inland.