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First 1429 results for ” R. Justin Small”

1. Baseline Surface Radiation Network (BSRN): structure and data description (1992-2017)

   Small changes in the radiation budget at the earth's surface can lead to large climatological res...

   A Driemel and 38 others, WH Knap | Status: published | Journal: Earth System Science Data | Volume: 10 | Year: 2018 | First page: 1491 | Last page: 1501 | doi: https://doi.org/10.5194/essd-10-1491-2018

   Publication

2. Improving slowness estimate stability and visualization using limited sensor pair correlation on seismic arrays

   Seismic arrays enhance signal detection and parameter estimation by exploiting the time-delays be...

   S Gibbons, S Naesholm, EN Ruigrok, T Kvaerna | Status: published | Journal: Geophys. J. Int. | Volume: 213 | Year: 2018 | First page: 447 | Last page: 460 | doi: 10.1093/gji/ggx550

   Publication

3. Rainfall depth-duration-frequency curves and their uncertainties

   Rainfall depth-duration-frequency (DDF) curves describe rainfall depth as a function of duration ...

   Overeem, Buishand, Holleman | Status: published | Journal: J. Hydrol. | Volume: 348 | Year: 2008 | First page: 124 | Last page: 134 | doi: 10.1016/j.jhydrol.2007.09.044

   Publication

4. 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

   Publication

5. Key parameters for the life cycle of nocturnal radiation fog: a comprehensive large-eddy simulation study

   High-resolution large-eddy simulations (LESs) are used to investigate the effect of turbulence as...

   Maronga, Bosveld | Status: published | Journal: Quart. J. Royal Meteor. Soc. | Volume: 143 | Year: 2017 | First page: 2463 | Last page: 2480 | doi: 10.1002/qj.3100

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