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First 1907 results for ” Stephan Lenk”

1. Is the intensification of precipitation extremes with global warming better detected at hourly than daily resolutions?

   Although it has been documented that daily precipitation extremes are increasing worldwide, faste...

   Barbero, Fowler, G Lenderink, G Blenkinsop | Status: published | Journal: Geophys. Res. Lett. | Volume: 44 | Year: 2017 | First page: 974 | Last page: 983 | doi: 10.1002/2016GL071917

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2. Path lenght distributions for solar photons under cloudy skies: Comparison of measured first and second moments with predictions from classical and anomalous diffusion theories
   T Scholl, K Pfeilsticker, AB Davis, H Klein Baltink, S Crewell, U Lohnert, C Simmer, J Meywerk, M Quante | Status: published | Journal: J. Geophys. Res. | Volume: 111 | Year: 2006 | First page: 1 | Last page: 16 | doi: doi:10.1029/2004JD005707

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3. Is the THC bi-stable at present? (invited expert box 7.3), p173-174. In: Richardson, K., W. Steffen and D. Liverman, eds
   G van der Schrier, SL Weber | Journal: Climate Change, global risks challenges | Year: 2011 | First page: 801

   Publication

4. A data-driven impact-based analysis stemming from first responders reports to predict wind damage to urban trees

   Transitioning from weather forecasts and warnings to impact-based forecast and warning services r...

   Irene Garcia-Marti, Jouke H. S. de Baar, Jan Willem Noteboom, Rob Sluijter, Gerard van der Schrier | Journal: Frontiers in Climate | Volume: 6 | Year: 2024 | doi: https://doi.org/10.3389/fclim.2024.1505268

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5. Action-based flood forecasting for triggering humanitarian action

   Too often, credible scientific early warning information of increased disaster risk does not resu...

   E Coughlan de Perez, BJJM van den Hurk, MK van Aalst, I Amuron, D Bamanya, T Hauser, B Jongman, A Lopez, S Mason, J Mendler de Suarez, F Pappenberger, A Rueth, E Stephens, P Suarez, J Wagemaker | Status: published | Journal: Hydrology and Earth System Sciences | Year: 2016 | doi: 10.5194/hess-2016-163

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