Watershed Data Report

This report was created with the free Global Watersheds web app on . Creative Commons License BY 4.0.

Contents

  1. Political Boundaries
  2. Population
  3. Land Cover
  4. Hydrology
  5. GRACE Terrestrial Water Storage
  6. Irrigation
  7. Dams
  8. Longest River
  9. Topography
  10. References

This report is for the watershed with an outlet near 20°30'00"N, 85°49'01"E, or (20.500, 85.817), with a drainage area of around 133,000 km².

Political Boundaries

The watershed is entirely within India, and in five states, as shown in Table 2.

Table 2. States in the watershed.

State Area (km²) Percent of watershed
Odisha 56,900 43%
Maharashtra 351 0%
Chhattisgarh 75,600 57%
Jharkhand 246 0%
Madhya Pradesh 278 0%

Data on political boundaries comes from Natural Earth, https://www.naturalearthdata.com.

Population

The watershed has an estimated population of 36,600,000 in the year 2020. Figure 1 shows how population has changed from 1990 to 2020. The population grew at an average rate of 1.6% per year over this time period.

Figure 1. Estimated watershed population from 1990 to 2020.

Population data comes from GlobPop, Global Gridded Population Estimates, created by researchers at Beijing Normal University (Liu 2024).

Human population growth can affect water quality via increased pollution from households, industry, and agriculture. Further, land use and land cover change associated with population growth can have a major impact on watersheds (see the next section of this report).

Land Cover

The most common land cover type in the watershed is cropland, covering 46,100 km² in 2020. More detailed information about land cover and how it has changed is shown in Table 3 and Figure 2 below. Pairs of bars represent the area for each land cover type in the years 2000 and 2020.

Figure 2. Land cover in the watershed.

Table 3. Land cover in the watershed.

Land Cover Type Area in 2000, km² Area in 2020, km²   Change
Cropland 39,800 46,100 15%
Tree cover 42,000 42,300 0%
Dense short vegetation 45,700 37,400 -18%
Built-up 1,590 3,540 122%
Open surface water 2,170 3,290 51%
Semi-arid 935 822 -12%
Wetland + dense short vegetation 1,030 213 -79%

Land cover data comes from the GLAD: Global Land Cover and Land Use Change, 2000-2020 (Popatov et al. 2022). This dataset, created by researchers at the University of Maryland, is available online here. Classification is based on satellite imagery from Landsat and machine learning tools.

Land cover change can profoundly influence watershed hydrology and water quality. Urbanization and development can increase the impervious cover, causing more water to run off rather than infiltrate into the ground. This can decrease groundwater recharge and river baseflows, or the flows that occur during dry times. Deforestation and agricultural development are often accompanied by an increase in soil erosion and sediment loads. Other land use types are associated with water pollution. For example, agriculture can increase loads of pesticides and nutrients (nitrogen and phosphorus) from fertilizers. Urbanization and industrialization can cause contamination from a wide range of chemicals used in households and industry.

Hydrology

The average annual precipitation over the watershed is 1,358 mm/year. (Precipitation includes all forms of water, including snow and rain.) Some of this water leaves the watershed surface via evaporation and transpiration, or the loss of water from plants. Annual evapotranspiration is estimated at 617 mm/year. The basin climatology, or the monthly average precipitation and evapotranspiration, is shown in Figure 4.

Figure 4. Watershed climatology: monthly average precipitation and evapotranspiration over the watershed.

Precipitation data comes from WorldClim, a global gridded dataset by researchers at the University of East Anglia (Harris et al. 2020). This dataset is based on downscaling and bias-correcting the CRU-TS dataset (Fick and Hijmans 2017), which is based on a large collection of station observations that span 1901–2018.

Evapotranspiration is even more difficult to estimate than precipitation. Here, we use a dataset, GLEAM v3.6B, which combines modeling and remote sensing data (Martens et al. 2017; Miralles et al. 2011).

It is difficult to estimate water cycle variables over large areas. So you should keep in mind that these estimates are uncertain (not perfect).

Terrestrial Water Storage Anomaly

The GRACE satellites provide information about changes in the amount of water over different locations on the Earth. Figure 3 shows the average terrestrial water storage anomaly over the watershed.

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Figure 3. GRACE terrestrial water storage anomaly from 2002 to 2025.

The GRACE satellites make highly accurate measurements of the Earth's gravitational field, and provide measurements of changes in the mass of water on a monthly time scale. These measurements do not tell us how much water there is in a region, but rather, how it the amount of water has changed compared to a baseline. The measurement includes all forms of water, including water in rivers, lakes, and reservoirs, soil moisture, groundwater, glaciers, snow, and ice. For an introduction to GRACE, see the section of my PhD thesis on Remote Sensing of the Water Cycle.

The total amount of water in the watershed appears to be trending upwards at a rate of 0.9 cm per decade (P = 0.54). This P-value indicates that the observed trend is not statistically significant. In other words, there is insufficient evidence to conclude that there is a meaningful trend in the data.

GRACE Terrestrial Water Storage Anomaly data is from the Center for Space Research at the University of Texas, Austin (Save et al. 2016, 2022).

Irrigation

The watershed had about 13779.6 km² of land equipped for irrigation in 2005. This is about 10.3% of the watershed. Figure 5 shows the development of irrigated area from 1900 to 2005. These estimates are based on a global dataset published by an international team of researchers (Siebert et al. 2015).

Figure 5. Area equipped for irrigation in the watershed from 1900 to 2005

Irrigation brings many benefits for growing crops. In arid regions, it enables production where it would be otherwise impossible. In humid regions, irrigation can increase crop quality and yield, and provide more certainty against unpredictable climate. Yet, the expansion of irrigation can have impacts on watersheds that need to be carefully managed.

Increased irrigation usually requires more water to be withdrawn from rivers, lakes, or groundwater sources, which can reduce streamflow and alter natural flow patterns. This reduced flow can harm aquatic ecosystems and diminish the water available downstream for other uses. Irrigation often introduces fertilizers and pesticides into the watershed, and may increase soil erosion and sediment transport. When nutrients run off into rivers and streams, they can lead to nutrient pollution, algal blooms, and eutrophication. This plus chemical pesticides and herbicides negatively impacts aquatic life and water quality for human uses.

Dams

This watershed contains 403 dams identified in the Global Dam Watch database, with a total storage capacity of 18,000 million m³.

Information on these dams is listed in Table 4. The number and size of dams in a watershed is one measure of hydromodification, or how much the natural hydrologic cycle is influenced by human activities.

Table 4. Dams in the watershed. Unknown or missing data shown with a dash.

Dam Name Reservoir Name River Main Use Year Dam Height (m) Capacity (10⁶ m³) Latitude Longitude URL
22.456 82.055
22.301 82.083
22.288 82.087
22.258 82.094
22.059 82.331
22.025 82.331
21.954 82.325
21.939 82.317
21.917 82.306
21.951 83.391
21.916 82.929
21.913 83.406
21.888 83.400
21.880 82.314
21.861 82.339
21.864 82.927
21.844 82.926
21.844 82.351
21.824 82.359
21.796 82.372
21.795 82.920
21.772 82.379
21.780 82.808
21.803 82.783
21.755 82.900
21.771 82.948
21.714 82.296
21.569 83.161
21.495 81.631
21.478 81.630
21.508 83.136
21.482 81.663
21.442 82.623
21.275 82.636
21.213 82.643
20.774 83.340
20.378 82.658
20.388 82.657
19.719 82.900
20.022 83.240
22.393 82.027
22.397 82.032
23.292 82.309
22.748 83.510
22.560 81.935
22.533 82.018
22.518 82.047
22.533 83.359
20.956 80.864
20.899 80.823
21.965 82.933
20.453 85.736
21.859 82.095
21.867 82.029
21.837 82.117
21.847 82.159
21.820 81.944
21.826 82.187
21.806 81.927
21.780 82.188
21.771 81.808
21.761 81.708
21.758 82.219
21.750 81.747
21.754 82.254
21.725 82.786
21.725 82.305
21.748 82.294
21.714 82.346
21.716 82.601
21.689 83.270
21.663 81.672
21.628 81.691
21.625 82.384
21.574 81.678
21.494 82.267
21.292 82.123
21.873 82.066
21.539 81.380
21.797 82.731
21.621 81.546
21.609 81.436
21.614 81.605
21.580 81.653
21.476 81.361
21.429 81.379
21.367 81.322
21.116 81.245
20.970 81.872
22.124 82.636
22.031 82.639
20.736 81.951
20.709 81.688
22.030 83.157
21.973 82.217
21.988 82.224
21.956 82.226
21.903 82.207
21.860 82.201
21.883 82.199
21.842 82.198
21.566 82.563
21.505 82.608
21.460 81.678
21.395 81.629
21.410 81.637
21.300 81.535
21.250 81.542
21.058 81.245
21.045 81.240
21.054 81.605
21.012 80.912
21.001 81.255
20.982 80.846
20.975 80.824
20.979 80.891
20.980 80.866
20.866 80.820
20.834 80.792
20.779 80.767
20.808 80.776
20.770 80.750
20.756 80.705
20.499 81.384
20.474 81.419
20.455 81.443
20.302 81.543
22.372 82.026
Hirakud Hirakud Mahanadi Irrigation Built 1957 59.0 8100.0 21.520 83.855
Bango Bango Reservoir Hasdeo Hydroelectricity Built 1990 87.0 3416.0 22.605 82.599
Ravishankar Sagar Ravishankar Sagar Mahanadi Irrigation Built 1979 31.0 909.0 20.614 81.565
Tandula Tandula Irrigation Built 1923 25.0 312.3 20.702 81.198
Dudhawa Mahanadi Irrigation Built 1963 24.0 287.8 20.305 81.758
Gondli Tank 223.3 20.743 81.130
Sikasar Local Nalla Irrigation Built 1977 32.0 216.5 20.518 82.319
210.8 20.702 81.214
Sondur Local Nalla Irrigation Built 1988 38.0 198.0 20.226 82.098
Kharung Irrigation Built before 1985 21.0 195.2 22.290 82.219
Kharkhara Tank Kharikhara Built 1967 169.9 20.831 80.988
Murumsilli Murumsilli Silliyari Irrigation Built 1923 26.0 165.0 20.539 81.665
Kodar Kodar Nalla Irrigation Built 1981 23.0 160.3 21.198 82.182
Maniyari Maniyari Irrigation Built 1930 29.0 151.2 22.392 81.591
Built 2007 141.2 20.756 80.664
114.2 20.596 82.590
Mahanadi Mahanadi Irrigation Built 1978 30.0 91.0 21.144 82.002
87.4 21.167 81.374
85.0 22.307 81.977
Upper Jonk Jonk Irrigation Built 1993 25.0 81.0 20.735 82.444
Built before 1985 80.5 20.884 80.938
Hariharjore Hariharjore Irrigation Built 1995 19.0 79.0 21.040 84.015
68.7 23.262 82.530
67.2 20.340 84.797
61.6 20.531 81.030
Chhirpani Phon Irrigation Built 1994 32.0 51.3 22.202 81.198
51.0 20.806 82.664
46.2 20.409 83.159
45.2 20.793 82.024
43.9 21.293 80.960
41.5 22.345 84.120
40.7 21.686 80.996
Built before 1985 39.2 21.534 82.485
Built 2003 38.3 22.383 82.124
37.4 20.852 82.684
Saroda Uttari Stream Irrigation Built 1964 32.0 37.1 21.981 81.139
36.8 22.427 83.569
36.5 21.052 82.769
35.9 21.455 83.298
Maroda-1 33.9 21.180 81.366
33.1 20.423 84.340
32.5 22.408 82.696
Built 1996 31.3 21.957 84.268
30.6 21.542 80.929
Built before 1985 26.8 20.655 81.563
25.1 21.563 82.973
23.9 21.461 83.968
23.8 20.453 85.604
Built 2002 23.4 21.217 80.952
Built 1990 22.9 21.731 81.223
Built 1999 21.8 23.319 82.565
Budhabudiani Budhabudiani Irrigation Built 1967 24.0 21.8 19.964 85.019
Built 2001 20.5 22.653 83.555
18.9 20.900 81.171
Built before 1985 18.3 21.264 81.796
18.1 22.186 83.765
Built 1991 16.1 20.723 82.879
16.0 20.415 81.280
Built before 1985 15.9 20.998 82.112
15.8 21.554 81.884
15.7 20.957 80.734
15.5 21.147 82.550
15.5 22.287 81.780
15.2 20.315 83.218
Built 1998 14.9 20.590 85.293
14.2 20.969 82.375
Built 1996 14.2 23.260 82.354
Built before 1985 13.6 21.648 82.102
13.6 20.788 82.178
13.6 20.562 84.966
13.2 21.207 82.923
13.0 20.452 82.698
Khapri Local Nalla Built 1909 11.0 13.0 21.015 81.369
12.9 21.178 82.813
12.5 21.154 80.655
12.4 21.368 82.001
Built 1996 12.1 21.473 83.423
12.1 19.957 82.610
11.9 21.048 82.273
Built 1999 11.8 20.573 82.851
Kumhari Kumhari Reservoir Banjari Nalla Irrigation Built 1927 12.0 11.6 21.493 81.909
Built before 1985 11.6 21.042 81.792
11.5 21.403 81.861
11.4 21.280 82.186
Built before 1985 11.4 21.956 82.344
Built before 1985 11.3 21.022 81.489
Built 1989 10.9 19.426 82.792
10.9 21.040 80.615
10.8 21.175 82.509
Built 1997 10.5 21.935 81.877
Built 1994 10.4 21.361 81.226
10.1 21.039 82.989
10.0 21.206 81.818
10.0 21.508 83.364
10.0 21.210 80.665
9.9 19.847 83.004
9.9 21.121 82.366
9.9 21.335 81.022
9.8 21.849 83.128
Built before 1985 9.8 21.393 81.870
9.4 21.564 82.323
9.4 21.468 81.785
Built before 1985 9.1 20.259 85.158
Built 1991 9.0 23.066 82.372
8.7 20.918 80.802
8.6 21.102 81.777
Built before 1985 8.5 21.765 81.484
8.5 21.290 82.349
8.5 21.448 80.830
8.4 21.964 83.168
8.4 20.935 80.622
8.3 22.270 81.943
Built 1994 8.1 21.246 82.763
8.0 20.956 83.515
7.9 22.113 82.450
7.8 21.455 81.268
7.8 21.027 81.788
7.6 21.919 82.128
Built before 1985 7.4 21.265 81.080
7.4 21.613 82.615
7.4 21.338 82.434
Built before 1985 7.3 20.406 81.389
Built 1998 7.2 21.133 82.413
7.2 19.830 82.840
7.1 20.623 82.960
7.1 21.134 82.247
Built 1990 7.1 20.956 82.282
7.0 22.164 82.481
Built 1991 6.9 21.010 81.014
6.9 20.800 80.717
6.8 21.924 82.423
6.7 23.498 82.485
Built before 1985 6.7 21.230 81.085
6.7 21.199 81.649
6.6 21.941 83.321
6.6 22.881 82.858
6.5 22.273 81.403
Built before 1985 6.3 21.180 82.535
6.2 22.331 82.435
6.2 20.709 80.768
6.2 22.039 81.256
6.1 21.676 82.140
Built 1997 6.0 20.317 82.913
Built before 1985 6.0 21.881 81.235
6.0 20.796 80.649
5.9 21.219 83.177
5.8 22.241 81.447
5.8 22.253 81.530
5.7 20.080 83.360
5.6 20.775 82.400
Built before 1985 5.6 21.400 82.902
5.4 21.407 80.876
Built before 1985 5.4 21.908 81.117
5.3 20.562 81.111
5.3 21.530 81.296
5.2 21.221 81.200
Built before 1985 5.2 21.273 82.756
5.2 21.986 82.200
5.2 21.510 81.407
5.0 21.263 81.030
Built 2008 5.0 21.507 80.865
5.0 21.546 83.090
Built before 1985 5.0 21.590 81.163
5.0 20.926 82.831
5.0 21.279 80.828
Built before 1985 4.9 21.178 81.045
Built before 1985 4.9 21.012 80.836
4.9 20.428 81.879
4.9 20.410 81.227
4.8 21.331 81.990
4.8 21.134 81.826
Built 1992 4.7 22.231 83.951
Built 1989 4.7 21.147 81.776
4.7 22.398 83.170
4.6 20.298 85.097
4.5 20.047 85.073
Built before 1985 4.5 21.035 80.831
4.4 20.216 85.101
4.4 21.129 82.443
Built 1993 4.3 20.248 83.294
4.3 20.344 81.456
4.2 22.303 81.739
4.2 22.274 82.518
4.2 21.194 83.463
4.1 21.216 81.066
4.1 20.781 82.226
4.0 21.148 80.988
4.0 20.896 80.563
4.0 21.110 81.827
Built before 1985 3.8 22.389 82.244
3.8 21.117 80.651
3.7 19.646 82.590
3.7 21.940 82.398
3.6 19.880 83.232
Built before 1985 3.6 21.706 81.801
3.5 21.870 83.095
3.5 20.860 80.850
3.5 22.347 81.676
3.5 22.737 83.289
3.4 21.207 82.417
3.4 21.062 80.772
3.4 21.298 83.191
3.3 21.215 80.693
3.3 20.269 82.685
3.3 21.900 82.379
3.3 20.440 81.361
3.3 21.067 81.785
3.2 21.102 80.877
3.2 21.012 81.459
3.2 21.851 83.180
3.2 22.152 82.766
Built before 1985 3.2 21.086 80.964
Built before 1985 3.2 22.323 81.727
3.1 19.766 82.759
Built 1999 3.1 21.012 80.814
3.1 22.387 82.467
3.1 20.368 84.210
3.0 22.310 81.493
3.0 22.716 82.449
3.0 21.270 80.873
3.0 21.630 80.950
Built 1995 3.0 21.981 83.227
3.0 22.040 81.288
3.0 20.971 80.615
2.9 21.857 81.089
2.9 22.406 82.309
Built before 1985 2.9 21.316 83.363
2.8 23.274 82.606
2.8 22.152 81.290
2.8 20.964 80.597
2.8 22.203 82.535
2.8 22.278 81.819
2.8 21.045 80.827
Built before 1985 2.7 20.693 80.869
2.6 22.303 81.757
2.6 21.164 82.431
2.6 21.381 81.047
2.6 21.367 82.846
2.6 21.199 80.929
2.6 21.227 81.628
2.5 22.187 82.921
2.4 20.239 82.647
2.4 21.907 82.475
2.3 20.627 81.282
2.3 21.027 81.057
2.3 21.270 83.758
2.3 20.119 85.204
2.2 21.963 81.247
2.2 20.132 82.805
2.2 22.265 82.840
2.1 23.052 82.484
2.1 20.175 82.778
2.1 20.549 81.081
Built before 1985 2.1 22.818 82.188
2.1 21.547 83.441
Built 1992 2.1 22.716 83.284
2.0 23.343 82.626
Built 1991 2.0 21.827 81.341
Built before 1989 2.0 21.360 80.881
2.0 20.228 82.743
1.9 22.203 82.863
Built 1996 1.8 21.952 81.955
1.8 21.261 80.905
1.8 22.185 84.390
1.7 19.864 83.176
Built 2004 1.6 22.269 81.868
1.6 20.243 83.259
1.6 20.562 81.072
1.5 21.392 80.918
1.5 21.100 80.978
Maroda Tank Local Nalla Built 1991 12.0 1.4 20.600 82.045
0.9 20.832 82.669
0.8 21.008 83.599
0.7 23.061 82.533
0.2 20.853 82.224

Dams serve many useful purposes including electric generation, water supply, irrigation, flood control, and recreation. However, if not carefully planned and managed, dams can have a heavy environmental impact. Today, many governments are removing dams to bring rivers back to life.

For a detailed look at the impact of dams on people and the environment, I encourage you to read the book Silenced Rivers by Patrick McCully. To help conserve free-flowing rivers, consider supporting the nonprofit International Rivers.

Data on dams comes from the Global Dam Watch database, published in July 2024. For more details, see the journal article by lead researchers at McGill University (Lehner et al. 2024).

Longest River

The longest river is the watershed is 985 km long. It is shown highlighted in the map in Figure 5 below.

This is the longest continuous flowline in the source dataset, MERIT-Basins. It is not necessarily the mainstem of the river, or the one with the same name. When it comes to naming rivers, historical, legal, and cultural influences are also important.

Figure 5. The longest river that flows to the watershed outlet (highlighted).

Figure 6 shows the elevation profile of the longest river reach. Elevations on the plot are in meters above mean sea level. The river begins at 389 m, and the outlet is at 13 m.

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Figure 6. Elevation profile of the longest river reach.

Elevation data for the profile plot is from MERIT-DEM (Yamazaki et al. 2017). Actual distances on the plot may be underestimated somewhat. This is because river paths are based on a grid or raster data, which simplifies the meandering path of real-world rivers.

Topography

Terrain elevations in the watershed range from 24 m to 1,100 m above sea level. The average, or mean, elevation is 350 m. Figure 7 shows a distribution of terrain elevations in the watershed.

Figure 7. Distribution of terrain elevations in the watershed.
Scale for x-axis: Linear   Log

Elevation data is provided by EarthEnv (Amatulli et al. 2021), and is based on the Global Multi-resolution Terrain Elevation Data 2010 dataset (GMTED2010). Statistics are based on gridded elevation data with pixels that are about 5 km on a side. Because of the size of the pixels, some smoothing takes place, and so the statistics reported above may not capture the true minimum and maximum elevation.

References

Amatulli, G., Domisch, S., Tuanmu, M.-N., Parmentier, B., Ranipeta, A., Malczyk, J., & Jetz, W. (2018). A suite of global, cross-scale topographic variables for environmental and biodiversity modeling. Scientific Data, 5(1), 180040. https://doi.org/10.1038/sdata.2018.40

Fick, S.E., and R.J. Hijmans. 2017. “WorldClim 2: New 1‐km Spatial Resolution Climate Surfaces for Global Land Areas.” International Journal of Climatology 37 (12): 4302–15. https://doi.org/10.1002/joc.5086

Harris, I., Osborn, T.J., Jones, P. et al. Version 4 of the CRU TS monthly high-resolution gridded multivariate climate dataset. Scientific Data 7, 109 (2020). https://doi.org/10.1038/s41597-020-0453-3

Lehner, B., Beames, P., Mulligan, M. et al. The Global Dam Watch database of river barrier and reservoir information for large-scale applications. Scientific Data 11, 1069 (2024). https://doi.org/10.1038/s41597-024-03752-9

Liu, L., X. Cao, S. Li, and N. Jie. “A 31-Year (1990–2020) Global Gridded Population Dataset Generated by Cluster Analysis and Statistical Learning.” Scientific Data 11, no. 1 (January 24, 2024): 124. https://doi.org/10.1038/s41597-024-02913-0

Martens, B., Miralles, D.G., Lievens, H., van der Schalie, R., de Jeu, R.A.M., Fernández-Prieto, D., Beck, H.E., Dorigo, W.A., and Verhoest, N.E.C. 2017. GLEAM v3: satellite-based land evaporation and root-zone soil moisture, Geoscientific Model Development, 10, 1903–1925. https://doi.org/10.5194/gmd-10-1903-2017

Miralles, D.G., Holmes, T.R.H., de Jeu, R.A.M., Gash, J.H., Meesters, A.G.C.A., Dolman, A.J. 2011. Global land-surface evaporation estimated from satellite-based observations, Hydrology and Earth System Sciences, 15, 453–469. https://doi.org/10.5194/hess-15-453-2011

Potapov P., Hansen M.C., Pickens A., Hernandez-Serna A., Tyukavina A., Turubanova S., Zalles V., Li X., Khan A., Stolle F., Harris N., Song X.-P., Baggett A., Kommareddy I., Kommareddy A. (2022) The global 2000-2020 land cover and land use change dataset derived from the Landsat archive: first results. Frontiers in Remote Sensing. https://doi.org/10.3389/frsen.2022.856903

Save, H., S. Bettadpur, and B.D. Tapley (2016), High resolution CSR GRACE RL05 mascons, Journal of Geophysical Research Solid Earth, 121. https://doi.org/10.1002/2016JB013007

Save, H., 2020, "CSR GRACE and GRACE-FO RL06 Mascon Solutions v02." https://doi.org/10.15781/cgq9-nh24

Siebert, S., M. Kummu, M. Porkka, P. Döll, N. Ramankutty, and B. R. Scanlon. “A Global Data Set of the Extent of Irrigated Land from 1900 to 2005.” Hydrology and Earth System Sciences 19, no. 3 (March 25, 2015): 1521–45. https://doi.org/10.5194/hess-19-1521-2015.

Yamazaki, D., D. Ikeshima, R. Tawatari, T. Yamaguchi, F. O’Loughlin, J.C. Neal, C.C. Sampson, S. Kanae, & P.D. Bates. (2017). A high‐accuracy map of global terrain elevations. Geophysical Research Letters, 44, 5844–5853. https://doi.org/10.1002/2017GL072874.