In scatterometry, the wind vector retrieval problem is ambiguous, i.e., the inversion procedure d...
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The 10 m‐wind over flat terrain in models is often lower than observations indicate. Here we show...
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The parameterised description of subgrid-scale processes in the clear and cloudy boundary layer h...
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Meteorological fields calculated by numerical weather prediction (NWP) models drive offline chemi...
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The Atmospheric LAser Doppler INstrument (ALADIN) on board Aeolus was the first high-spectral-res...
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