71 citations as recorded by crossref.

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2. The Turbulent Structure and Diurnal Growth of the Saharan Atmospheric Boundary Layer L. Garcia-Carreras et al. 10.1175/JAS-D-13-0384.1
3. Evaluating Primary Marine Aerosol Production and Atmospheric Roll Structures in Hawaii’s Natural Oceanic Wind Tunnel* V. Kapustin et al. 10.1175/JTECH-D-11-00079.1
4. Assessing the Influence of Aerosol on Radiation and Its Roles in Planetary Boundary Layer Development Z. Cheng et al. 10.1007/s13351-021-0109-z
5. An Automated Detection Methodology for Dry Well-Mixed Layers S. Nicholls & K. Mohr 10.1175/JTECH-D-18-0149.1
6. Advances in understanding mineral dust and boundary layer processes over the Sahara from Fennec aircraft observations C. Ryder et al. 10.5194/acp-15-8479-2015
7. Structure and dynamics of the Saharan atmospheric boundary layer during the West African monsoon onset: observations and analyses from the research flights of 14 and 17 July 2006 C. Messager et al. 10.1002/qj.469
8. Saharan and Asian dust: similarities and differences determined by CALIPSO, AERONET, and a coupled climate-aerosol microphysical model L. Su & O. Toon 10.5194/acp-11-3263-2011
9. Meteorological and geological controls on dust devil activity: Initial results from a field study at Smith Creek Valley, Nevada, USA L. Fenton et al. 10.1016/j.aeolia.2022.100831
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11. Vertical structure of summer clear‐sky atmospheric boundary layer over the hinterland and southern margin of Taklamakan Desert M. Wang et al. 10.1002/met.1568
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18. Vertical profile of saltating particle concentration over semidesert area G. Gorchakov et al. 10.1088/1755-1315/606/1/012015
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20. Contributions of dusty weather and dust devil to dust emission amounts at the northern margin of the Taklimakan Desert M. Ma et al. 10.1007/s11069-020-04043-3
21. Atmospheric boundary layer and ozone-aerosol interactions under Saharan intrusions observed during AMISOC summer campaign J. Adame et al. 10.1016/j.atmosenv.2014.12.036
22. Turbulent Mechanisms for the Deep Convective Boundary Layer in the Taklimakan Desert L. Zhang et al. 10.1029/2022GL099447
23. A diagnostic analysis on the effect of the residual layer in convective boundary layer development near Mongolia using 20th century reanalysis data B. Han et al. 10.1007/s00376-014-4164-6
24. Quantifying particle size and turbulent scale dependence of dust flux in the Sahara using aircraft measurements P. Rosenberg et al. 10.1002/2013JD021255
25. Bacterial diversity in snow from mid-latitude mountain areas: Alps, Eastern Anatolia, Karakoram and Himalaya R. Azzoni et al. 10.1017/aog.2018.18
26. Large eddy simulation of boundary-layer turbulence over the heterogeneous surface in the source region of the Yellow River Y. Zhang et al. 10.5194/acp-21-15949-2021
27. Physical and optical properties of mineral dust aerosol measured by aircraft during the GERBILS campaign B. Johnson & S. Osborne 10.1002/qj.777
28. Quantifying global dust devil occurrence from meteorological analyses B. Jemmett‐Smith et al. 10.1002/2015GL063078
29. CALIOP-Based Evaluation of Dust Emissions and Long-Range Transport of the Dust from the Aral−Caspian Arid Region by 3D-Source Potential Impact (3D-SPI) Method K. Shukurov et al. 10.3390/rs15112819
30. A rare case of haboob in Tehran: Observational and numerical study S. Karami et al. 10.1016/j.atmosres.2016.10.010
31. Quasiperiodic Emission of Dust Aerosol in a Desertified Area G. Gorchakov et al. 10.3103/S106837392308006X
32. Assessment of the Met Office dust forecast model using observations from the GERBILS campaign B. Johnson et al. 10.1002/qj.736
33. Effect of water vapor on the determination of aerosol direct radiative effect based on the AERONET fluxes J. Huttunen et al. 10.5194/acp-14-6103-2014
34. Mid-level clouds over the Sahara in a convection-permitting regional model D. Mantsis et al. 10.1007/s00382-020-05188-4
35. Contributions of gust under stationery weather conditions to the dust aerosol budget in northwestern China J. Li et al. 10.1016/j.atmosres.2023.106914
36. What is the Mechanism for the Modification of Convective Cloud Distributions by Land Surface–Induced Flows? L. Garcia-Carreras et al. 10.1175/2010JAS3604.1
37. Cloud macro-physical properties in Saharan-dust-laden and dust-free North Atlantic trade wind regimes: a lidar case study M. Gutleben et al. 10.5194/acp-19-10659-2019
38. Physico‐chemical and optical properties of Sahelian and Saharan mineral dust: in situ measurements during the GERBILS campaign A. Klaver et al. 10.1002/qj.889
39. The Saharan convective boundary layer structure over large scale surface heterogeneity: A large eddy simulation study G. Papangelis et al. 10.1016/j.atmosres.2020.105250
40. Research Progress on Estimation of the Atmospheric Boundary Layer Height H. Zhang et al. 10.1007/s13351-020-9910-3
41. Meteorology and dust in the central Sahara: Observations from Fennec supersite‐1 during the June 2011 Intensive Observation Period J. Marsham et al. 10.1002/jgrd.50211
42. The different influence of the residual layer on the development of the summer convective boundary layer in two deserts in northwest China Z. Lin et al. 10.1007/s00704-016-2014-4
43. Organized Roll Circulation and Transport of Mineral Aerosols in the Atmospheric Boundary Layer N. Vazaeva et al. 10.1134/S0001433819020142
44. Parameterization of dust flux emitted by convective turbulent dust emission (CTDE) over the Horqin Sandy Land area T. Ju et al. 10.1016/j.atmosenv.2018.05.043
45. The Fennec Automatic Weather Station (AWS) Network: Monitoring the Saharan Climate System M. Hobby et al. 10.1175/JTECH-D-12-00037.1
46. Observations of Increased Cloud Cover over Irrigated Agriculture in an Arid Environment L. Garcia-Carreras et al. 10.1175/JHM-D-16-0208.1
47. Impacts of Water Vapor on Saharan Air Layer Radiative Heating M. Gutleben et al. 10.1029/2019GL085344
48. Unexpected vertical structure of the Saharan Air Layer and giant dust particles during AER-D F. Marenco et al. 10.5194/acp-18-17655-2018
49. Features of the Deep Atmospheric Boundary Layer Over the Taklimakan Desert in the Summertime and its Influence on Regional Circulation M. Wang et al. 10.1029/2019JD030714
50. THE WAY TO DETERMINE THE APPROXIMATELY HAIL'S DIMENSIONS N. Ilie et al. 10.15551/pesd2020141002
51. Origin, Maintenance and Variability of the Asian Tropopause Aerosol Layer (ATAL): The Roles of Monsoon Dynamics W. Lau et al. 10.1038/s41598-018-22267-z
52. Semi‐Coupling of a Field‐Scale Resolving Land‐Surface Model and WRF‐LES to Investigate the Influence of Land‐Surface Heterogeneity on Cloud Development J. Simon et al. 10.1029/2021MS002602
53. Large Eddy Simulation on Dust Suspension in a Convective Mixed Layer J. Ito et al. 10.2151/sola.2010-034
54. A Parameterization of Convective Dust Storms for Models with Mass-Flux Convection Schemes F. Pantillon et al. 10.1175/JAS-D-14-0341.1
55. Large-eddy simulation of dust-uplift by a haboob density current Q. Huang et al. 10.1016/j.atmosenv.2018.01.048
56. Temporal and spatial characteristics of dust devils and their contribution to the aerosol budget in East Asia—An analysis using a new parameterization scheme for dust devils Y. Tang et al. 10.1016/j.atmosenv.2018.03.050
57. Clouds over the summertime Sahara: an evaluation of Met Office retrievals from Meteosat Second Generation using airborne remote sensing J. Kealy et al. 10.5194/acp-17-5789-2017
58. Dust resuspension under weak wind conditions: direct observations and model O. Chkhetiani et al. 10.5194/acp-12-5147-2012
59. Integrative investigation of dust emissions by dust storms and dust devils in North Africa L. Pan et al. 10.1016/j.scitotenv.2020.144128
60. Simulating boundary‐layer rolls with a numerical weather prediction model W. Thurston et al. 10.1002/qj.2646
61. Dust plume formation in the free troposphere and aerosol size distribution during the Saharan Mineral Dust Experiment in North Africa B. Khan et al. 10.3402/tellusb.v67.27170
62. THE HAIL FALLS AT THE MOLDAVIA LEVEL AND THE IMPORTANCE OF THE HAIL SUPPRESSION UNIT "MOLDOVA 1" IAȘI A. Axinte 10.15551/pesd2019132009
63. Properties of a simulated convective boundary layer over inhomogeneous vegetation C. Wang et al. 10.1002/qj.724
64. Study on the Parameters of Ice Clouds Based on 1.5 µm Micropulse Polarization Lidar Y. Li et al. 10.3390/rs14205162
65. The Atlantic inflow to the Saharan heat low: observations and modelling C. Grams et al. 10.1002/qj.429
66. Relation between the Atmospheric Boundary Layer and Impact Factors under Severe Surface Thermal Conditions Y. Ao et al. 10.1155/2017/8352461
67. Uplift of Saharan dust south of the intertropical discontinuity J. Marsham et al. 10.1029/2008JD009844
68. Measurement report: The promotion of the low-level jet and thermal effects on the development of the deep convective boundary layer at the southern edge of the Taklimakan Desert L. Su et al. 10.5194/acp-24-10947-2024
69. Relationship of atmospheric boundary layer depth with thermodynamic processes at the land surface in arid regions of China Q. Zhang et al. 10.1007/s11430-011-4207-0
70. The Response of the Aerosol Distribution to Monsoon Intensity Over the Summer Monsoon Transition Zone B. Bai et al. 10.3389/feart.2019.00356
71. The Ability of the Small Ice Detector (SID-2) to Characterize Cloud Particle and Aerosol Morphologies Obtained during Flights of the FAAM BAe-146 Research Aircraft R. Cotton et al. 10.1175/2009JTECHA1282.1