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Impact of dominant waves on sea drag
The impact of air-flow separation from breaking dominant waves is analyzed.
This impact results f...
VK Makin, VK Kudryavtsev | Status: published | Journal: Bound.-Layer Meteorol. | Volume: 103 | Year: 2002 | First page: 83 | Last page: 99
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Composite hodographs and inertial oscillations in the nocturnal boundary layer.
In this work the dynamic behaviour of the wind in the nocturnal boundary layer is studied, with a...
P Baas, BJH van de Wiel, L van den Brink, AAM Holtslag | Status: accepted | Journal: Quart. J. Royal Meteor. Soc. | Year: 2011 | doi: DOI:10.1002/qj.941
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Coupling of a wave model and a storm surge model through the atmospheric boundary layer
The effect of a wave-dependent drag coefficient on the generation of storm surge in the North...
C Mastenbroek, G Burgers, PAEM Janssen | Status: published | Journal: J. Phys. Oceanogr. | Volume: 23 | Year: 1993 | First page: 1856 | Last page: 1866
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Effects of correcting salinity with altimeter measurements in an equatorial Pacific ocean model
In this paper, we study the consequences of making salinity corrections in a tropical Pacific oce...
FC Vossepoel, G Burgers, PJ van Leeuwen | Status: published | Journal: J. Geophys. Res. | Volume: 107 | Year: 2002 | First page: 8001 | Last page: 8014 | doi: 10.1029/2001JC000816
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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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