Table 1 Satellite-derived sediment discharge (SSD) summary

From: Assessing modern river sediment discharge to the ocean using satellite gravimetry

River

In situ

SSD

Grain size

Grain size range

Range of the sedimentation zone area

SNR in GRACE data

Mt year−1

Mt year−1

µm

µm

×1000 km2

Amazon

778

560±90

10

10

630

2.4

610 ± 165

5

5

3000

0.8

Ganges-Brahmaputra

1081

1140±200

10

10

210

1.2

−890 ± 750

0.1

Changjiang

477

430±100

5

5

110

1.3

330 ± 100

20

10–100

40–12

1.0

Mississippi

51

−130±310

0.1

−190 ± 380

0.1

Irrawaddy

333

−1100±610

0.5

50 ± 270

10

10

220

0.3

Indus

206

150±70

30

30–100

15–10

0.6

350 ± 120

10

10

80

1.5

Orinoco

76

−250±450

0.2

−110 ± 240

0.1

Godavari

119

230±90

70

70–100

24–12

3.0

650 ± 120

40

40–50

71–43

5.8

Mekong

75

580±150

40

20–100

12–8

0.4

80 ± 110

40

40–100

8

0.4

Magdalena

150

460±90

40

40–50

50–30

2.3

670 ± 90

50

40–70

50–16

4.8

Fly

111

−1980±660

0.9

−570 ± 470

0.3

Congo

32

150±90

100

50–100

8–5

0.9

170 ± 300

5

5

590

0.1

Huanghe

152

−860±450

0.5

−60 ± 150

0.1

  1. Results for GRACE s1 and s2 solutions are in bold and italic fonts, respectively. “Grain size” is the grain sizes that minimize the difference between the SSD and the in situ sediment discharge, for each river and each hydrological correction applied on GRACE solutions (only for rivers which are SSD positive). “Grain size range” gives the range of grain sizes for which the SSD does not differ by more than 10% from the best SSD (obtained for the best grain size). Narrow grain size ranges suggest that GRACE could help constraining the grain size of the particles that are responsible for the largest mass accumulation out of each river. The entire range of grain sizes tested in this work is 5–100 µm. The area of the sedimentation zone associated to the grain size range is also given. The last column is the SNR for each river (see also Methods)