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The GeoStationary Scanning Imaging absorption Spectrometer (GeoSCIA) as part of the Geo Stationary Tropospheric Pollution Explorer (GeoTROPE) Mission: Objectives and Requirements
One of the major challenges facing atmospheric sciences is to assess, understand and quantify the...
H Bovensmann, KU Eichmann, S Noel, JM Flaud, J Orphal, ..........................., APH Goede | Status: published | Journal: Adv.Space Res. | Volume: 34 | Year: 2004 | First page: 694 | Last page: 699 | doi: doi:10.1016/j.asr.2003.08.068
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The influence of wall permeability on turbulent channel flow
Direct Numerical Simulations (DNS) have been performed of turbulent flow in a plane channel with ...
WP Breugem, BJ Boersma, RE Uittenbogaard | Status: published | Journal: J. Fluid Mech. | Volume: 562 | Year: 2006 | First page: 35 | Last page: 72 | doi: 10.1017/S0022112006000887
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Evaluating the diurnal cycle of South Atlantic stratocumulus clouds as observed by MSG SEVIRI
Marine stratocumulus (Sc) clouds play an essential role in the earth radiation budget. Here, we c...
C Seethala, JF Meirink, A Horvath, R Bennartz, R Roebeling | Status: published | Journal: Atm. Chem. Phys. | Volume: 18 | Year: 2018 | First page: 13283 | Last page: 13304 | doi: 10.5194/acp-18-13283-2018
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Evaluating the diurnal cycle of South Atlantic stratocumulus clouds as observed by MSG SEVIRI
Marine stratocumulus (Sc) clouds play an essential role in the earth radiation budget. Here, we c...
Seethala, C., Meirink, J. F., Horv´ath, A., Bennartz, R., and Roebeling, R | Journal: Atmospheric Chemistry and Physics | Volume: 18 | Year: 2018 | doi: https://doi.org/10.5194/acp-18-13283-2018
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Attribution of the record high Central England temperature of 2014 to anthropogenic influences
In 2014, Central England experienced its warmest year in a record extending back to 1659. Using b...
AD King, GJ van Oldenborgh, DJ Karoly, SC Lewis, H Cullen | Status: published | Journal: Environmental Research Letters | Volume: 10 | Year: 2015 | First page: 054002 | doi: 10.1088/1748-9326/10/5/054002
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