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Meteorological Source Variability in Atmospheric Gravity Wave Parameters Derived From a Tropical Infrasound Station
Gravity waves are an important part of the momentum budget of the atmosphere. Despite this, param...
GJ Marlton, AJ Charlton-Perez, RG Harrison, Blanc, LG Evers, A Le-Pichon, PSM Smets | Status: published | Journal: J. Geophys. Res. | Volume: 124 | Year: 2019 | First page: 4352 | Last page: 4364 | doi: https://doi.org/10.1029/2018JD029372
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Atmospheric visibility inferred from continuous-wave Doppler wind lidar
Atmospheric visibility, or meteorological optical range (MOR), is governed by light extinction by...
Manuel Queißer, Michael Harris, and Steven Knoop | Journal: Atmos. Meas. Tech. | Volume: 15 | Year: 2022 | First page: 5527 | Last page: 5544 | doi: https://doi.org/10.5194/amt-15-5527-2022
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Mixing in shallow cumulus clouds studied by Lagrangian particle tracking
Mixing between shallow cumulus clouds and their environment is studied using large eddy-simulatio...
T Heus, G van Dijk, HJJ Jonker, HEA van den Akker | Status: published | Journal: J. Atmos. Sci. | Volume: 65 | Year: 2008 | First page: 2581 | Last page: 2597 | doi: 10.1175/2008JAS2572.1
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Observational validation of the compensating mass flux through the shell around cumulus clouds
The existence of a subsiding shell around cumulus clouds has been observed before in several airc...
T Heus, HJJ Jonker, HEA van den Akker, DH Lenschow | Status: published | Journal: Quart. J. Royal Meteor. Soc. | Volume: 135 | Year: 2009 | First page: 101 | Last page: 112 | doi: 10.1002/qj.358
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Use of tethersonde and aircraft profiles to study the impact of mesoscale and microscale meteorology on air quality
Highly-resolved vertical profiles of ozone and reactive nitrogen in the lower troposphere were ob...
GM Mazzuca, KE Pickering, RD Clark, CP Loughner, A Fried, DC Stein Zweers, A Weinheimer, RR Dickerson | Status: published | Journal: Atmos. Environm. | Volume: 149 | Year: 2017 | First page: 55 | Last page: 69 | doi: http://dx.doi.org/10.1016/j.atmosenv.2016.10.025
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