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First 405 results for ” R.; Baptista”

1. Monitoring Beach Topography and Nearshore Bathymetry Using Spaceborne Remote Sensing: A Review

   With high anthropogenic pressure and the effects of climate change (e.g., sea level rise) on coas...

   Salameh, E.; Frappart, F.; Almar, R.; Baptista, P.; Heygster, G.; Lubac, B.; Raucoules, D.; Almeida, L.P.; Bergsma, E.W.J.; Capo, S.; De Michele, M.; Idier, D.; Li, Z.; Marieu, V.; Poupardin, A.; Silva, P.A.; Turki, I.; Laignel, B. | Journal: Remote Sensing | Volume: 11 | Year: 2019 | First page: 1-32 | doi: https://doi.org/10.3390/rs11192212

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2. Moving Beyond Monin-Obukhov Similarity Theory in Modelling Wind Speed Proles in the Stable Lower Atmospheric Boundary Layer

   Monin-Obukhov similarity theory (MOST) is commonly used to model the wind speed profile at altitu...

   M Optis, A Monahan, FC Bosveld | Status: published | Journal: Bound.-Layer Meteorol. | Volume: 153 | Year: 2014 | First page: 497 | Last page: 514 | doi: 10.1007/s10546-014-9953-z

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3. Limitations and breakdown of Monin-Obukhov similarity theory for wind profile extrapolation under stable stratification

   The intent of this study is to investigate the limitations of the Monin–Obukhov similarity theory...

   M Optis, A Monahan, FC Bosveld | Status: published | Journal: Wind Energy | Year: 2015 | doi: 10.1002/we.1883View

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4. Zeewind langs de Hollandse kust : synoptische verwachtingsmethoden

   Zeewind langs de Hollandse kust : synoptische verwachtingsmethoden

   Zeewind langs de Hollandse kust : synoptische verwachtingsmethoden | Year: 1981 | Pages: 76

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5. Wind Sea and Swell Waves in the Nordic Seas

   The output of a high-resolution wave model of the Nordic Seas is analyzed and a climatology devel...

   A Semedo, R Vettor, O Breivik, A Sterl, M Reistad, C Guedes Soares | Conference: 13th International Workshop on Wave Hindcasting and Forecasting and 4th Coastal Hazards Symposium | Organisation: GOOS | Place: Banff, Canada | Year: 2013 | doi: 10.1007/s10236-014-0788-4 | First page: 0 | Last page: 0

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