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Stationary abyssal circulation forced by enhanced upwelling over a mid-ocean ridge
Stommel and co-workers calculated the stationary, geostrophic circulation in the abyssal ocean ...
CA Katsman | Status: published | Journal: J. Phys. Oceanogr. | Volume: 36 | Year: 2006 | First page: 1660 | Last page: 1671
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Observing Boundary-Layer Winds from Hot-Air Balloon Flights
High-resolution upper-air wind observations are sparse, and additional observations are a welcome...
EIF de Bruijn, S de Haan, FC Bosveld, B Wichers Schreur, AAM Holtslag | Status: published | Journal: Weather and Forecasting | Volume: 31 | Year: 2016 | First page: 1451 | Last page: 1463 | doi: 10.1175/WAF-D-16-0028.1
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Future Space-Based Doppler Wind Lidar Winds
The unique European Space Agency (ESA) Earth Explorer Aeolus Doppler Wind Lidar (DWL) is a succes...
Ad Stoffelen, Gert-Jan Marseille, Tommaso Parinello, Oliver Reitebuch, Michael Rennie, Anne Grete Straume
| Journal: 2021 IEEE International Geoscience and Remote Sensing Symposium IGARSS | Year: 2021 | doi: https://doi.org/10.1109/IGARSS47720.2021.9554250
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Integraal Waterbeheer - kritische zone & onzekerheden Integraal hoofdrapport
In het kader van het Nationaal Modellen- en Datacentrum (NMDC) is in 2011 het NMDC innovatieproje...
PNM Schipper, R van Ek, G Oude Essink, MF van Geer, E Simmelink, P Janssen, J van der Sluijs, J Bessembinder, M Faneca Sanchez, E van Baaren, A Groot, JG Kroes, I Supit, A Bakker, JP Mol | Year: 2012
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Het hoe, wat en waarom van infrageluid metingen
Infrageluid is onhoorbaar geluid omdat het bestaat uit frequenties lager dan 20 Hz. Dit type gelu...
LG Evers | Journal: Meteorologica | Volume: 18 | Year: 2009 | First page: 24 | Last page: 26
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