古尔班通古特沙漠腹地输沙风能及地貌学意义

干旱区研究 ›› 2011, Vol. 28 ›› Issue (4): 580-585.

古尔班通古特沙漠腹地输沙风能及地貌学意义

郭洪旭^1,2, 王雪芹¹, 蒋进¹, 赵新军³, 胡永锋¹

1. 中国科学院新疆生态与地理研究所中国科学院生物地理与生物资源重点实验室, 新疆乌鲁木齐 830011;
2. 中国科学院广州能源研究所, 广东广州 510640;
3. 新疆额尔齐斯河流域开发工程建设管理局, 新疆乌鲁木齐 830000

收稿日期:2010-08-11 修回日期:2010-10-25 出版日期:2011-08-25 发布日期:2011-09-06
通讯作者: 王雪芹.E-mail:xqwang@ms.xjb.ac.cn
作者简介:郭洪旭(1984-),男,新疆哈密人,在读博士生,主要从事荒漠环境与风沙地貌研究.E-mail:guohx@163.com
基金资助:
国家自然科学基金项目(40771032)和中国科学院知识创新工程项目(KZCX2-YW-336)资助

Wind Regime and Its Geomorphologic Significance in the Hinterland of Gurbantonggut Desert

GUO Hong-xu^1,2, WANG Xue-qin¹, JIANG Jin¹, ZHAO Xin-jun³, HU Yong-feng¹

1. Key Laboratory of Biogeography and Bioresources in Arid Land, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;
2. Guangzhou Institute of Energy Conversion, Chinese Academy of Sciences, Guangzhou 510640, China;
3. Project Construction Administration of Ertix River Basin in Xinjiang, Urumqi 830011, China

Received:2010-08-11 Revised:2010-10-25 Online:2011-08-25 Published:2011-09-06

摘要/Abstract

摘要： 根据古尔班通古特沙漠腹地2个气象台站2003-2006年气象资料,分析起沙风况和输沙势,并对其地貌学意义进行探讨。结果表明:沙漠中部全年起沙风出现频率为0.25％,以东北风和西北风为主;南部起沙风出现频率为0.11％,以西北风和西南风为主。沙漠中部和南部均属于低风能环境,中部地区的总输沙势(DP)为66.7 VU,合成输沙势(RDP)为25.7 VU,合成输沙方向(RDD)为197.0°,方向变率指数为0.56;南部地区总输沙势(DP)为29.8 VU,合成输沙势(RDP)为16.3 VU,合成输沙方向(RDD)为108.4°,方向变率指数为0.65。沙漠中部4～10月输沙势占全年总输沙势的90%以上,其中7月的输沙势占全年的20%以上;沙漠南部输沙势主要集中于4～8月,约占全年的85%。沙漠中部受东北风和西北风的影响,与之相应的地面沙垄长而直,基本沿合成输沙方向延伸;沙漠南部受天山山脉的影响,主导风向转为西北和西南风,与之相应的地面沙垄开始向东偏转,并出现了副梁。

关键词: 起沙风, 输沙势, 沙垄走向, 古尔班通古特沙漠

Abstract: Gurbantonggut Desert is the largest fixed and semi-fixed desert in China. In this study a statistical analysis on wind regime and sand drift potential at two weather stations located in the hinterland of the Gurbantonggut Desert was carry out during the period from 2003 to 2006. The results are as follows: The occurring frequency of sand transport wind is 0.25% in the central area of the desert and 0.11% in the south area. The prevailing wind directions are northeast wind and northwest wind in the central area but southwest wind and northwest wind in the south area. In the central area, the sand drift potential (DP) and resultant sand drift potential (RDP) are 66.7 VU and 25.7 VU respectively, and the resultant sand drift direction (RDD) is 197.0°. DP and RDP in the south area are 29.8 VU and 16.3 VU respectively, and RDD is 108.4°. Both the central and south areas of the Gurbantonggut Desert belong to the low wind energy environment according to Fryberger's classification. Sand transport wind in the study area occurs mainly in spring and summer, the percentage of DP from April to October accounts for 90% in the central area, and that from April to August in the south area accounts for 85%. Affected by strong wind and corresponding wind directions (northeast and northwest) in the central area, the ridge of longitudinal dune-chains extends along the resultant wind direction, and the dune chains are high. Affected by southwest and northwest winds in the south area, an eastward deflexion of the ridge of longitudinal dune-chains occurs, and a subsidiary ridge appears.

Key words: wind regime, sand drift potential, strike of longitudinal dune-chain, Gurbantonggut Desert

中图分类号:

P931.3

郭洪旭, 王雪芹, 蒋进, 赵新军, 胡永锋. 古尔班通古特沙漠腹地输沙风能及地貌学意义[J]. 干旱区研究, 2011, 28(4): 580-585.

GUO Hong-xu, WANG Xue-qin, JIANG Jin, ZHAO Xin-jun, HU Yong-feng. Wind Regime and Its Geomorphologic Significance in the Hinterland of Gurbantonggut Desert[J]. , 2011, 28(4): 580-585.

参考文献

[1] Fryberger S G,Goudie A S. Arid geomorphology[J]. Progress in Physical Geography,1981,5(3):20-428.

[2] Skidmore E L.Assessing wind erosion forces:Directions and relative magnitudes[J].Soil Science Society of America Proceedings,1965,29:587-590.

[3] Goudie A S.Dust storms in space and time[J].Progress in Physical Geography,1983,7:502-530.

[4] 朱震达.中国沙漠、沙漠化、荒漠化及其治理对策[M].北京:中国环境出版社,1999:113-115.

[5] 吴正.风沙地貌学[M].北京:科学出版社,1987.

[6] 俎瑞平,张克存,屈建军,等.塔克拉玛干沙漠地面风场特征及周边地区沙丘排列关系分析[J].应用气象学报,2005,16(4):468-475.

[7] 陈渭南,董治宝,杨佐涛,等.塔克拉玛干沙漠的起沙风速[J].地理学报,1995,50(4):360-367.

[8] 王训明,陈广庭,韩致文,等.塔里木沙漠公路沿线的起沙风与输沙强度[J].中国沙漠,1997,17(2):168-172.

[9] 李振山,陈广庭.塔克拉玛干沙漠起沙风状况[J].中国沙漠,1999,19(1):43-45.

[10] 韩致文,王涛,董治宝,等.塔克拉玛干沙漠公路沿线风沙活动的时空分布[J].地理科学,2005,25(4):455-460.

[11] 谭芳,张岩,郭擎宇.古尔班通古特沙漠风沙运动规律及防沙治沙研究[J].科学中国人,2003(4):55-58.

[12] 马淑红,戈峰,陈晓光,等.古尔班通古特沙漠瞬间最大风速的时空分布特征[J].资源科学,2007,29(4):46-53

[13] 李红军,何清,杨青.近40 a新疆输沙势的分析[J].中国沙漠,2004,24(6):706-710.

[14] Wang X Q,Wang T,Jiang J,et al.On the sand surface stability in the southern part of Gurbantunggut Desert[J].Science in China:Series D,2004,34(8):763-768.

[15] 张立运,陈昌笃.论古尔班通古特沙漠植物多样性的一般特点[J].生态学报,2002,22(11):1 923-1 932.

[16] 王雪芹,雷加强.古尔班通古特沙漠半固定沙垄面的蚀积特征[J].干旱区研究,1998,15(1):35-39.

[17] 吴正.风沙地貌与治沙工程学[M].北京:科学出版社,2003.

[18] 吴正.中国沙漠与海岸沙丘研究[M].北京:科学出版社,1997:29-43.

[19] Freberger S G.Dune Form and Wind Regime:A Study of Global Sand Seas[M].Washington:US Government Printing Office,1979,1 052:137-170.

[20] Lancaster N.Linear dunes of the Namib sand sea[J].Zeitschrift für Geomorphologie,1983,45(Suppl.):27-49.