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First 1348 results for ” Rune Floberghagen”

1. Shallow lacustrine carbonate microfacies document orbitally paced lake-level history in the Miocene Teruel Basin (North-East Spain)

   Results are presented of a detailed carbonate petrographic study of an UpperMiocene lacustrine mi...

   HA Abels, HA Aziz, JP Calvo, E Tuenter | Status: published | Journal: Acta Geophysica | Volume: 56 | Year: 2009 | First page: 399 | Last page: 419 | doi: 10.1111/j.1365-3091.2008.00976.x

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2. A regional ocean circulation model for the mid-Cretaceous North Atlantic Basin: implications for black shale formation

   High concentrations of organic matter accumulated in marine sediments during Oceanic Anoxic Event...

   RPM Topper, J Trabucho Alexandre, E Tuenter, PT Meijer | Status: published | Journal: Climate of the Past | Volume: 7 | Year: 2011 | First page: 277 | Last page: 297 | doi: 10.5194/cp-7-277-2011

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3. Storm surge and extreme river discharge: a compound event analysis using ensemble impact modelling

   Many winter deep low-pressure systems passing over Western Europe have the potential to induce si...

   S Khanal, N Ridder, H de Vries, W Terink, B vd Hurk | Status: published | Journal: Frontiers in Marine Science | Volume: 7 | Year: 2019 | First page: 1 | Last page: 10 | doi: 10.3389/feart.2019.00224

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4. From near-neutral to strongly stratified: adequately modelling the clear-sky nocturnal boundary layer at Cabauw

   In this study, the performance of an atmospheric single-column model (SCM) is studied systematica...

   Baas, Wiel, Linden, Bosveld | Status: published | Journal: Bound.-Layer Meteorol. | Year: 2017 | doi: 10.1007/s10546-017-0304-8

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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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