Knowledge (XXG)

Kaidu River

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Land use-conversion is also a very problematic issue that is caused in the region of Northwest China due to climate change as well. Many of the people within this area have had to deal with deceases in natural grassland area. Cultivated land increased due to this issue as well. Land reclamations were
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Northwest China has been subjected to affects from the Kaidu River because of global warming and water perturbation. Studies have shown a correlation between the temperature and the precipitation being the leading cause to these issues. Additionally, the Kaidu River resides in an arid zone, causing
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The Kaidu River is a determinant factor of climate change in Northwest China. The river is a result of sensitivity due to climate variability. Due to studies through the usage of hydrologic sensitivity analysis, researchers were able to make this observation and make proof of it.
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Chen, Z., Chen, Y., & Li, B. (2012). Quantifying the effects of climate variability and human activities on runoff for Kaidu River Basin in arid region of northwest China. Theoretical and Applied Climatology, 111(3-4), 537-545.
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Chen, Z., Chen, Y., & Li, B. (2012). Quantifying the effects of climate variability and human activities on runoff for Kaidu River Basin in arid region of northwest China. Theoretical and Applied Climatology, 111(3-4), 537-545.
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Nara Shiruku Rōdo-haku Kinen Kokusai Kōryū Zaidan, Shiruku Rōdo-gaku Kenkyū Sentā: Opening up the Silk Road: the Han and the Eurasian world, Nara International Foundation Commemorating the Silk Road Exposition,
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Wang, Y., Chen, Y., Ding, J., & Fang, G. (2015). Land-use conversion and its attribution in the Kaidu–Kongqi River Basin, China. Quaternary International, 380-381, 216-223. doi:10.1016/j.quaint.2014.10.010
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what led to this, as well as an increase in the growth of socioeconomic development. This led to an increase in water management activities, which became an issue because of the consistent change of runoff.
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Mupenzi, J. D., & Li, L. (2011). Impacts of global warming perturbation on water resources in arid zone: Case study of Kaidu River Basin in Northwest China. Journal of Mountain Science, 8(5), 704-710.
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and an important source of water for the region. The Kaidu River is responsible for many substantial effects on the environment. Affecting the land and its people in many different ways.
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name "كۆنچى دەرياسى / Konchi Darya" which means "Tanner's River". The Kongque River flows through the
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for which it is the most important tributary. The river leaves the lake under the name Kongque River (
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The sources of the Kaidu River are located on the central southern slopes of the
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many different trends in temperature due to this climate change.
149: 141: 129: 121: 105: 97: 88: 78: 73: 53: 8: 410:Seespiegelschwankungen des Bosten-Sees 374: 155:107 m/s (3,800 cu ft/s) 133:22,000 km (8,500 sq mi) 50: 7: 208: 65:Kaidu River in the city center of 14: 213:Xinjiang Uyghur Autonomous Region 226:from where it flows through the 59: 306: 289: 273: 256: 191: 1: 444:doi:10.1007/s11629-011-2180-x 434:doi:10.1007/s00704-012-0680-4 382:doi:10.1007/s00704-012-0680-4 89:Physical characteristics 107: • elevation 491: 151: • average 475:Sites along the Silk Road 239: 230:and the Yanqi Basin into 200: 174: 159: 137: 125:610 km (380 mi) 117: 93: 58: 318:Settlements on the river 392:"Xinjiang River Guide" 34:42.04583°N 86.59333°E 352:Significant problems 286:traditional Chinese 30: /  470:Rivers of Xinjiang 397:2009-03-02 at the 270:simplified Chinese 39:42.04583; 86.59333 163: 162: 482: 454: 451: 445: 441: 435: 431: 425: 421: 415: 413: 407: 401: 389: 383: 379: 308: 299: 283: 258: 249: 210: 202: 193: 184: 152: 108: 63: 51: 45: 44: 42: 41: 40: 35: 31: 28: 27: 26: 23: 490: 489: 485: 484: 483: 481: 480: 479: 460: 459: 458: 457: 452: 448: 442: 438: 432: 428: 422: 418: 411: 408: 404: 399:Wayback Machine 390: 386: 380: 376: 371: 354: 337: 325: 320: 150: 106: 69: 49: 38: 36: 32: 29: 24: 21: 19: 17: 16: 12: 11: 5: 488: 486: 478: 477: 472: 462: 461: 456: 455: 446: 436: 426: 416: 402: 384: 373: 372: 370: 367: 353: 350: 349: 348: 343: 336: 333: 332: 331: 324: 321: 319: 316: 266:Iron Gate Pass 161: 160: 157: 156: 153: 147: 146: 143: 139: 138: 135: 134: 131: 127: 126: 123: 119: 118: 115: 114: 109: 103: 102: 99: 95: 94: 91: 90: 86: 85: 80: 76: 75: 71: 70: 64: 56: 55: 48:River in China 47: 13: 10: 9: 6: 4: 3: 2: 487: 476: 473: 471: 468: 467: 465: 450: 447: 440: 437: 430: 427: 420: 417: 414: 406: 403: 400: 396: 393: 388: 385: 378: 375: 368: 366: 362: 358: 351: 347: 344: 342: 339: 338: 335:Kongque River 334: 330: 327: 326: 322: 317: 315: 313: 309: 303: 298: 295: 292: 287: 282: 279: 276: 271: 267: 263: 259: 253: 248: 245: 242: 237: 233: 229: 225: 220: 218: 214: 209:قايدۇ دەرياسى 206: 198: 194: 188: 183: 180: 177: 172: 168: 158: 154: 148: 144: 140: 136: 132: 128: 124: 120: 116: 113: 110: 104: 100: 96: 92: 87: 84: 81: 77: 72: 68: 62: 57: 52: 46: 43: 449: 439: 429: 419: 405: 387: 377: 363: 359: 355: 305: 255: 228:Yulduz Basin 221: 190: 166: 164: 15: 412:(in German) 323:Kaidu River 312:Tarim Basin 310:) into the 307:Tiěmén Guān 232:Lake Bosten 167:Kaidu River 54:Kaidu River 37: / 464:Categories 369:References 329:Karashahar 257:Kǒngquè Hé 130:Basin size 25:86°35′36″E 341:Tashidian 224:Tian Shan 201:Хайду гол 197:Mongolian 142:Discharge 112:Tian Shan 22:42°2′45″N 395:Archived 192:Kāidū Hé 74:Location 236:Chinese 171:Chinese 79:Country 304:: 302:pinyin 288:: 272:: 262:Uyghur 254:: 252:pinyin 238:: 205:Uyghur 189:: 187:pinyin 173:: 145:  122:Length 101:  98:Source 346:Korla 217:China 83:China 67:Yanqi 424:2007 165:The 215:of 466:: 314:. 300:; 284:; 250:; 207:: 203:; 199:: 195:; 185:; 297:關 294:門 291:鐵 281:关 278:门 275:铁 268:( 247:河 244:雀 241:孔 182:河 179:都 176:开 169:(

Index

42°2′45″N 86°35′36″E / 42.04583°N 86.59333°E / 42.04583; 86.59333

Yanqi
China
Tian Shan
Chinese



pinyin
Mongolian
Uyghur
Xinjiang Uyghur Autonomous Region
China
Tian Shan
Yulduz Basin
Lake Bosten
Chinese



pinyin
Uyghur
Iron Gate Pass
simplified Chinese



traditional Chinese

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