Observed Dust Storm in the Taklimakan Desert on April 13, 2002

Nobumitsu Tsunematsu

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Observed Dust Storm in the Taklimakan Desert on April 13, 2002

机译：2002年4月13日在塔克拉玛干沙漠观察到的沙尘暴

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References(14) Cited-By(1) Supplementary materials(1) Analysis results of data from lidar and AWS observations performed in the northwestern part of the Taklimakan Desert show a sudden increase in the backscattering ratios in the lower troposphere on 13 April 2002, with strong easterly winds. The Terra satellite reveals that the sudden increase is caused by the outbreak of an extensive dust storm. Numerical simulations, using a regional model, reproduce the strong easterly winds prevailing in a wide area of the desert, originating from north of the Tienshan Mountains. These conclude that the strong easterly winds lift a large amount of sand particles off the ground and results in the dust storm. In addition, a nose-shaped profile of the increased backscattering ratios indicates passage of a gravity current.

机译：参考文献（14）被引用的资料（1）补充材料（1）塔克拉玛干沙漠西北部的激光雷达和AWS观测数据的分析结果表明，2002年4月13日对流层低层的反向散射比突然增加，强劲的东风。 Terra卫星显示，突然增加的原因是一场沙尘暴的爆发。使用区域模型进行的数值模拟再现了从天山山脉以北的沙漠广大区域盛行的强东风。这些结论表明，强东风将大量沙粒从地面抬起，并导致沙尘暴。另外，增加的反向散射比的鼻形轮廓指示重力流的通过。

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《SOLA: Scientific Online Letters on the Atmosphere》 |2005年第2期|共页
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Nobumitsu Tsunematsu;
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中图分类大气科学（气象学）;
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1. The structure of the dust layer over the Taklimakan desert during the dust storm in April 2002 as observed using a depolarization lidar [J] . Kai K, Nagata Y, Tsunematsu N, Journal of the Meteorological Society of Japan . 2008,第1期

机译：使用去极化激光雷达观测到的2002年4月沙尘暴期间塔克拉玛干沙漠上空的尘埃层结构
2. The Structure of the Dust Layer over the Taklimakan Deser during the Dust Storm in April 2002 as Observed Using a Depolarization Lidar [J] . Heon-Sook KIM, Hongfei ZHOU, Kenji KAI, ournal of the Meteorological Society of Japan . 2008,第1期

机译：用去极化激光雷达观测到的2002年4月沙尘暴期间塔克拉玛干沙漠上空的尘埃层结构
3. Variation Of Dust Layer Height In The Northern Taklimakan Desert In April 2002 [J] . Heon-Sook Kim, Yuichi Nagata, Kenji Kai Atmospheric environment . 2009,第3期

机译：2002年4月塔克拉玛干沙漠北部沙尘层高度的变化
4. Aerosol characteristics at Qira Oasis during the three intensive observation periods(IOPs) from April 2002 to March 2004 in the southern edge of Taklimakan Desert [C] . Fanjiang ZENG, Sadayo YABUKI, Ximing ZHANG, ADEC Workshop . 2005

机译：2002年4月至2004年3月在塔尔玛卡纳沙漠南部边缘（IOPS）在三次强化观察期（IOPS）期间QIRA OASIS的气溶胶特性
5. Martian global dust storm 2001A as observed by the Mars Global Surveyor Thermal Emission Spectrometer. [D] . Elteto, Attila. 2009

机译：火星全球测量师热发射光谱仪观测到的火星全球沙尘暴2001A。
6. First long-term detection of paleo-oceanic signature of dust aerosol at the southern marginal area of the Taklimakan Desert [O] . Qi Zhou, Juan Li, Jian Xu, -1

机译：塔克拉玛干沙漠南部边缘地区首次远距离探测尘埃气溶胶的古海洋特征
7. The Structure of the Dust Layer over the Taklimakan Deser during the Dust Storm in April 2002 as Observed Using a Depolarization Lidar [O] . Kenji KAI, Yuichi NAGATA, Nobumitsu TSUNEMATSU, 2008

机译：使用去极化激光雷达观察到的2002年4月在2002年4月的塔尔玛干沙漠中灰尘层的结构

Observed Dust Storm in the Taklimakan Desert on April 13, 2002

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