The emission of dust particles into the atmosphere is governed by the aerodynamic and resistant factors which are quantified by the friction velocity v and the threshold friction velocity mu.iota, respectively The threshold friction velocity u.iota influences the Vertical dust flux and dust transport. Based on the micrometeorological data obtained in the springs of 2004 and 2006 over Hunshandake desert area Loess Plateau, and Gobi desert area the relationship between dust. concentration and friction velocity for the dust. events that occurred over Hunshandake desert area was investigated and the threshold friction velocities over the three different. dust source areas were estimated The results show that the value of dust, concentration is ...
Dust events have been observed in Japan with high frequency since 2000. On the other hand, the frequ...
This study investigated the effect of snow and vegetation covers on dust emission by the correlation...
Dust emission generated by wind erosion is a basic process before the transport and deposition of du...
Dust emission generated by wind erosion is the largest source of tropospheric aerosols. The Gobi Des...
The threshold friction velocities of potential dust sources in the US Southwest were measured in the...
The Taklamakan Desert and the Gobi Desert in East Asia constitute the second-largest sources of dust...
International audienceTo determine the location of the potential dust source regions and to evaluate...
A meteorological and dust monitoring tower with 20 m height set up at a Nomgon site in Umnugobi Aima...
In this study, the effects of soil moisture on sand saltation and dust emission over the Horqin Sand...
A severe dust storm (SDS) event occurred during March-20 to March-22, 2010 in China. A regional dyna...
Based on data from the dust storm monitoring station over Hunshandake Desert Area, Inner Mongolia, t...
Dust deposition is a crucial link of dust cycle that is less constrained in model studies. This stud...
Dust emission from the Gobi desert is one of the major sources of global atmospheric aerosols. Howev...
Based on observations and numerical simulations, the topographic impacts on dust transport in East A...
Northern China experienced two intense dust storms in March 2021, leading to reduced visibility and ...
Dust events have been observed in Japan with high frequency since 2000. On the other hand, the frequ...
This study investigated the effect of snow and vegetation covers on dust emission by the correlation...
Dust emission generated by wind erosion is a basic process before the transport and deposition of du...
Dust emission generated by wind erosion is the largest source of tropospheric aerosols. The Gobi Des...
The threshold friction velocities of potential dust sources in the US Southwest were measured in the...
The Taklamakan Desert and the Gobi Desert in East Asia constitute the second-largest sources of dust...
International audienceTo determine the location of the potential dust source regions and to evaluate...
A meteorological and dust monitoring tower with 20 m height set up at a Nomgon site in Umnugobi Aima...
In this study, the effects of soil moisture on sand saltation and dust emission over the Horqin Sand...
A severe dust storm (SDS) event occurred during March-20 to March-22, 2010 in China. A regional dyna...
Based on data from the dust storm monitoring station over Hunshandake Desert Area, Inner Mongolia, t...
Dust deposition is a crucial link of dust cycle that is less constrained in model studies. This stud...
Dust emission from the Gobi desert is one of the major sources of global atmospheric aerosols. Howev...
Based on observations and numerical simulations, the topographic impacts on dust transport in East A...
Northern China experienced two intense dust storms in March 2021, leading to reduced visibility and ...
Dust events have been observed in Japan with high frequency since 2000. On the other hand, the frequ...
This study investigated the effect of snow and vegetation covers on dust emission by the correlation...
Dust emission generated by wind erosion is a basic process before the transport and deposition of du...