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First 1172 results for ” N Fournier”

1. Cloud impacts on photochemistry: building a climatology of photolysis rates from the Atmospheric Tomography mission

   Measurements from actinic flux spectroradiometers on board the NASA DC-8 during the Atmospheric T...

   SR Hall, K Ullman, MJ Prather, CM Flynn, LT Murray, J Flemming, V Huijnen, NL Abraham, AT Archibald | Status: published | Journal: Atm. Chem. Phys. | Year: 2018 | First page: 16809 | Last page: 16828 | doi: https://doi.org/10.5194/acp-18-16809-2018

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2. Relocation of clustered earthquakes in the Groningen gas field

   Previous locations of earthquakes induced by depletion of the Groningen gas field were not accura...

   L Jagt, EN Ruigrok, H Paulssen | Status: published | Journal: Netherlands Journal of Geosciences | Volume: 96 | Year: 2017 | First page: s163 | Last page: s173 | doi: 10.1017/njg.2017.12

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3. Single-column model simulations of subtropical marine boundary-layer cloud transitions under weakening inversions

   Results are presented of the GASS/EUCLIPSE single-column model inter-comparison study on the subt...

   RAJ Neggers, W de Rooy, C de Bruijn | Status: published | Journal: J. of Advances in Modeling Earth Systems | Volume: 9 | Year: 2017 | First page: 2385 | Last page: 2412 | doi: https://doi.org/10.1002/2017MS001064

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4. Understanding and Reducing False Alarms in Observational Fog Prediction

   The reduction in visibility that accompanies fog events presents a hazard to human safety and nav...

   Izett, Wiel, Baas, Bosveld | Status: published | Journal: Bound.-Layer Meteorol. | Year: 2018 | doi: 10.1007/s10546-018-0374-2

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5. A first comparison of TROPOMI aerosol layer height (ALH) to CALIOP data

   The TROPOspheric Monitoring Instrument (TROPOMI) level-2 aerosol layer height (ALH) product has n...

   S Nanda, M de Graaf, JP Veefkind, MC Sneep, M ter Linden, J Sun, PF Levelt | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 13 | Year: 2019 | First page: 3043 | Last page: 3059 | doi: 10.5194/amt-13-3043-2020

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