The DOI matches its Crossref record; 25 of the 25 references it cites were found in a registry or an index.
Causes for the decline of suspended‐sediment discharge in the Mississippi River system, 1940–2007
Abstract
Before 1900, the Missouri–Mississippi River system transported an estimated 400 million metric tons per year of sediment from the interior of the United States to coastal Louisiana. During the last two decades (1987–2006), this transport has averaged 145 million metric tons per year. The cause for this substantial decrease in sediment has been attributed to the trapping characteristics of dams constructed on the muddy part of the Missouri River during the 1950s. However, reexamination of more than 60 years of water‐ and sediment‐discharge data indicates that the dams alone are not the sole cause. These dams trap about 100–150 million metric tons per year, which represent about half the decrease in sediment discharge near the mouth of the Mississippi. Changes in relations between water discharge and suspended‐sediment concentration suggest that the Missouri–Mississippi has been transformed from a transport‐limited to a supply‐limited system. Thus, other engineering activities such as meander cutoffs, river‐training structures, and bank revetments as well as soil erosion controls have trapped sediment, eliminated sediment sources, or protected sediment that was once available for transport episodically throughout the year. Removing major engineering structures such as dams probably would not restore sediment discharges to pre‐1900 state, mainly because of the numerous smaller engineering structures and other soil‐retention works throughout the Missouri–Mississippi system. Published in 2009 by John Wiley & Sons, Ltd.
Overview
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Self-check
Percentages, sums and reported differences re-computed from the paper’s own numbers.
The self-check needs the paper’s full text.
Citations
Cites
Downstream effects of dams on alluvial rivers
Williams, G. P., & Wolman, M. G. (1984) · Professional Paper · doi:10.3133/pp1286 · Cited by 1,134
Drowning of the Mississippi Delta due to insufficient sediment supply and global sea-level rise
Blum, M. D., & Roberts, H. H. (2009) · Nature Geoscience · doi:10.1038/ngeo553 · Cited by 1,032
Yield of sediment in relation to mean annual precipitation
(1958) · Eos, Transactions American Geophysical Union · doi:10.1029/tr039i006p01076 · Cited by 1,030
Field methods for measurement of fluvial sediment
Edwards, T. K., & Glysson, G. D. (1988) · Open-File Report · doi:10.3133/ofr86531 · Cited by 918
Horowitz, A. J. (2003) · Hydrological Processes · doi:10.1002/hyp.1299 · Cited by 459
A sediment budget for Coon Creek basin in the Driftless Area, Wisconsin, 1853-1977
Trimble, S. W. (1983) · American Journal of Science · doi:10.2475/ajs.283.5.454 · Cited by 434
Decreased Rates of Alluvial Sediment Storage in the Coon Creek Basin, Wisconsin, 1975-93
Trimble, S. W. (1999) · Science · doi:10.1126/science.285.5431.1244 · Cited by 410
Movement and storage of sediment in rivers of the United States and Canada
Meade, R. H., Yuzyk, T. R., & Day, T. J. (2015) · Surface Water Hydrology · doi:10.1130/dnag-gna-o1.255 · Cited by 353
Self-citationQuaternary geology of the Lower Mississippi Valley
Autin, W. J., Burns, S. F., Miller, B. J., Saucier, R. T., & Snead, J. I. (2015) · Quaternary Nonglacial Geology · doi:10.1130/dnag-gna-k2.547 · Cited by 323
Topping, D. J., Rubin, D. M., & Vierra, L. E. (2000) · Water Resources Research · doi:10.1029/1999wr900285 · Cited by 301
Suspended sediment dynamics in a large drainage basin: the River Rhine
Asselman, N. E. M. (1999) · Hydrological Processes · doi:10.1002/(sici)1099-1085(199907)13:10<1437::aid-hyp821>3.0.co;2-j · Cited by 278
Hudson, P. F., & Kesel, R. H. (2000) · Geology · Cited by 270
Contaminants in the Mississippi River, 1987-92
Meade, R. H. (1995) · Circular · doi:10.3133/cir1133 · Cited by 267
Self-citationBedform transport rates for the lowermost Mississippi River
Nittrouer, J. A., Allison, M. A., & Campanella, R. (2008) · Journal of Geophysical Research: Earth Surface · doi:10.1029/2007jf000795 · Cited by 201
Sediment dynamics in the lowermost Mississippi River
Mossa, J. (1996) · Engineering Geology · doi:10.1016/s0013-7952(96)00026-9 · Cited by 197
The Variability of Large Alluvial Rivers
Costa, J. E. (1995) · Eos · doi:10.1029/95eo00262 · Cited by 179
Human modifications to the sediment regime of the Lower Mississippi River flood plain
Kesel, R. H. (2003) · Geomorphology · doi:10.1016/s0169-555x(03)00159-4 · Cited by 175
Sediment Dynamics and the Hydromorphology of Fluvial Systems
Rowan, J. S., Duck, R. W., & Werritty, A. (2006) · Cited by 169
Hudson, P. F., Middelkoop, H., & Stouthamer, E. (2008) · Geomorphology · doi:10.1016/j.geomorph.2008.07.001 · Cited by 147
Historic Trends in the Sediment Flow Regime of the Mississippi River
Keown, M. P., Dardeau, E. A., & Causey, E. M. (1986) · Water Resources Research · doi:10.1029/wr022i011p01555 · Cited by 130
Horowitz, A. J. (2009) · Hydrological Processes · doi:10.1002/hyp.7425 · Cited by 92
Sediment regime constraints on river restoration—An example from the Lower Missouri River
Jacobson, R. B., Blevins, D. W., & Bitner, C. J. (2009) · Geological Society of America eBooks · doi:10.1130/2009.2451(01 · Cited by 76
Meade, R. H., & STEVENSJR, H. (1990) · The Science of The Total Environment · doi:10.1016/0048-9697(90)90235-m · Cited by 74
Self-citationMeade, R. H. (2007) · Large Rivers · doi:10.1002/9780470723722.ch4 · Cited by 66
Self-citationHarmar, O. P., Clifford, N. J., Thorne, C. R., & Biedenharn, D. S. (2005) · River Research and Applications · doi:10.1002/rra.887 · Cited by 66
Cited by
Allison, M. A., Demas, C. R., Ebersole, B. A., Kleiss, B. A., Little, C. D., Meselhe, E. A., Powell, N. J., Pratt, T. C., & Vosburg, B. M. (2012) · Journal of Hydrology · doi:10.1016/j.jhydrol.2012.02.020 · Cited by 296
Balch, J. K., Iglesias, V., Braswell, A. E., Rossi, M. W., Joseph, M. B., Mahood, A. L., Shrum, T. R., White, C. T., Scholl, V. M., McGuire, B., et al. (2020) · Earth's Future · doi:10.1029/2019ef001319 · Cited by 71
Hudson, P. F. (2018) · International Journal of River Basin Management · doi:10.1080/15715124.2017.1411921 · Cited by 6
Metadata
- Authors
- Meade, R. H., & Moody, J. A.
- Venue
- Hydrological Processes
- Publisher
- Wiley
- Published
- 2009-10-13
- Volume
- 24
- Issue
- 1
- Pages
- 35-49
- ISSN
- 0885-6087 (ISSN-L)
- 1099-1085
- OpenAlex
- W2146201073
- Cited by
- 466
- References
- 25
- FWCI
- 9.84
- Type
- journal article
- Language
- en
- Open access
- closed
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review
Data sources
Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.