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Landscape evolution model

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The earliest landscape evolution models were developed in the 1970s. In those models, flow of water across a mesh was simulated, and cell elevations were changed in response to calculated
63:, and other surface processes. These changes occur in response to the land surface being uplifted above sea-level (or other base-level) by surface 131: 263: 24:
that simulates changing terrain over the course of time. The change in, or evolution of, terrain, can be due to:
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Barnes, Richard (2019). "Accelerating a fluvial incision and landscape evolution model with parallelism".
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to aid in decision making, most recently in the area of degraded landscapes.
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Coulthard, T. J. (2001). "Landscape evolution models: a software review".
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and other acceleration hardware and software, to run more quickly.
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Landscape evolution models are used primarily in the field of
29: 121: 48: 78:. As they improve, they are beginning to be consulted by 89:. Modern landscape evolution models can leverage 274: 257: 264: 250: 132:Community Surface Dynamics Modeling System 193: 152: 275: 179: 216: 51:, more intermittent events such as 47:, the slow movement of material on 13: 14: 304: 220: 204:10.1016/j.geomorph.2019.01.002 173: 146: 1: 140: 236:. You can help Knowledge by 7: 99: 10: 309: 215: 91:graphics processing units 18:landscape evolution model 155:Hydrological Processes 67:, and also respond to 20:is a physically-based 293:Mathematical modeling 288:Geomorphology models 283:Geomorphology stubs 106:Hillslope evolution 45:regolith production 37:sediment transport 245: 244: 115:CAESAR-Lisflood, 300: 266: 259: 252: 224: 217: 208: 207: 197: 177: 171: 170: 150: 308: 307: 303: 302: 301: 299: 298: 297: 273: 272: 271: 270: 213: 211: 178: 174: 167:10.1002/hyp.426 151: 147: 143: 102: 96: 87:erosional power 22:numerical model 12: 11: 5: 306: 296: 295: 290: 285: 269: 268: 261: 254: 246: 243: 242: 225: 210: 209: 172: 144: 142: 139: 138: 137: 129: 124: 118: 113: 108: 101: 98: 9: 6: 4: 3: 2: 305: 294: 291: 289: 286: 284: 281: 280: 278: 267: 262: 260: 255: 253: 248: 247: 241: 239: 235: 232:article is a 231: 230:geomorphology 226: 223: 219: 218: 214: 205: 201: 196: 191: 187: 183: 182:Geomorphology 176: 168: 164: 160: 156: 149: 145: 136: 133: 130: 128: 125: 122: 119: 117: 114: 112: 109: 107: 104: 103: 97: 94: 92: 88: 83: 81: 80:land managers 77: 76:geomorphology 72: 70: 66: 62: 58: 54: 50: 46: 42: 38: 34: 31: 27: 23: 19: 238:expanding it 227: 212: 185: 181: 175: 158: 154: 148: 126:pyBadlands, 95: 84: 73: 57:debris flows 17: 15: 120:LANDIS II, 277:Categories 195:1803.02977 141:References 69:subsidence 61:landslides 49:hillslopes 41:deposition 188:: 28–39. 110:SIBERIA, 53:rockfalls 100:See also 161:: 165. 33:erosion 30:fluvial 26:glacial 65:uplift 228:This 190:arXiv 234:stub 39:and 200:doi 186:330 163:doi 28:or 279:: 198:. 184:. 159:15 157:. 134:, 59:, 55:, 43:, 35:, 16:A 265:e 258:t 251:v 240:. 206:. 202:: 192:: 169:. 165::

Index

numerical model
glacial
fluvial
erosion
sediment transport
deposition
regolith production
hillslopes
rockfalls
debris flows
landslides
uplift
subsidence
geomorphology
land managers
erosional power
graphics processing units
Hillslope evolution




Community Surface Dynamics Modeling System

doi
10.1002/hyp.426
arXiv
1803.02977
doi
10.1016/j.geomorph.2019.01.002

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