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Climate change increases the probability of heavy rains in Northern England/Southern Scotland like those of storm Desmond - a real-time event attribution revisited
On 4–6 December 2015, storm Desmond caused very heavy rainfall in Northern England and Southern S...
FEL Otto, K van der Wiel, GJ van Oldenborgh, S Philip, S Kew, P Uhe, H Cullen | Status: published | Journal: Environmental Research Letters | Volume: 13 | Year: 2018 | First page: 024006 | doi: 10.1088/1748-9326/aa9663
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The MSG-SEVIRI-based cloud property data record CLAAS-2
Clouds play a central role in the Earth's atmosphere, and satellite observations are crucial for ...
Benas N., Finkensieper S., Stengel M., Van Zadelhoff G.-J., Hanschmann T., Hollmann R., Meirink J. F. | Status: published | Journal: Earth System Science Data | Volume: 9 | Year: 2017 | First page: 415 | Last page: 434 | doi: 10.5194/essd-9-415-2017
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Simultaneous and synergistic profiling of cloud and drizzle properties using ground-based observations
Despite the importance of radar reflectivity (Z) measurements in the retrieval of liquid water cl...
SP Rusli, DP Donovan, HWJ Russchenberg | Status: submitted | Journal: Atmospheric Measurement Techniques | Year: 2017 | doi: doi:10.5194/amt-2016-402
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Inter-comparison of different NOX emission inventories and associated variation in simulated surface ozone in Indian region
n this work, we compare for the first time different anthropogenic NOX emission inventories and e...
C Jena, SD Ghude, G Beig, DM Chate, R Kumar, G< Pfister, DM Lal, DE Surendran, S Fadnavis, RJ van der A | Status: published | Journal: Atmos. Environm. | Year: 2015 | First page: 61 | Last page: 73 | doi: 10.1016/j.atmosenv.2015.06.057
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Impacts of afternoon and evening sea-breeze fronts on local
We investigated sharp disruptions of local turbulence and scalar transport due to the arrival of ...
Arrillaga, Vila-Guerau de Arellano, Bosveld, Klein Baltink, Yague, Sastre, Roman-Cascon | Status: published | Journal: Quart. J. Royal Meteor. Soc. | Year: 2018 | doi: 10.1002/qj.3252
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