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Lower thermosphere–ionosphere (LTI) quantities: Current status of measuring techniques and models
The lower-thermosphere–ionosphere (LTI) system consists of the upper atmosphere and the lower par...
M Palmroth, M Grandin, T Sarris, E Doornbos, S Tourgaidis, A Aikio, S Buchert, M Clilverd | Status: submitted | Journal: Annales Geophysicae | Year: 2020 | doi: 10.5194/angeo-2020-42
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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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Argo - The challenge of continuing 10 years of progress
In only 10 years, the Argo Program has grown from an idea into a functioning global observing sys...
D Roemmich, and the Argo Steering Team, among others:, A Sterl | Journal: Oceanography | Volume: 22 | Year: 2009 | First page: 46 | Last page: 55
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DIGISTAD: Disclosure of the hourly meteorological observations of the Amsterdam City Water Office 1784-1963
This report describes the digitization, the quality control, metadata and analysis of the hourly ...
Hendrik Wallbrink, Theo Brandsma | Year: 2008 | Pages: 26
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Attribution of extreme climate events
Extreme weather or climate-related events occur in a particular place, by definition, infrequentl...
PA Stott, N Christidis, FEL Otto, Y Sun, JP Vanderlinden, GJ van Oldenborgh, R Vautard, H von Storch, P Walton, P Yiou, F Zwiers | Status: published | Journal: WIRES Climate Change | Volume: 7 | Year: 2015 | First page: 23 | Last page: 41 | doi: 10.1002/wcc.380
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