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Tracking down the ENSO delayed oscillator with an adjoint OGCM
The adjoint of an ocean general circulation model is used as a tool for investigating the causes ...
GJ van Oldenborgh, G Burgers, S Venzke, C Eckert, R Giering | Status: published | Journal: Mon. Wea. Rev. | Volume: 127 | Year: 1999 | First page: 1477 | Last page: 1496
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Brief review of wind and drag transformations in WBI2017
To determine the hydraulic boundary conditions for the design of coastal defence structures, hydr...
A. Sterl | Year: 2018 | Pages: 12
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Experiments with interactive methods for solving the discrete Poisson equation
After the development of the well-known iterative methods for solving systems of linear equations...
S.J. Bijlsma and R.J. Hoogendoorn | Year: 1979 | Pages: 45
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Determination of the mixing layer height from ceilometer backscatter profiles
The mixing layer height (MLH) is a key parameter in studies of many atmospheric boundary layer pr...
MJ de Haij, H Klein Baltink, WMF Wauben | Journal: KNMI Kenniscentrum | Year: 2010
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Spatial and Temporal Propagation of Scatterometer Winds
Ocean models are generally forced by synthetic (global) NWP model wind fields. It has however bee...
D Harutyunyan, A Stoffelen | Year: 2011
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